巴丹吉林沙漠与腾格里沙漠沉积物特征的对比研究
|
摘要
巴丹吉林沙漠和腾格里沙漠位于中国西北干旱荒漠区,两者以雅布赖山为界,行政区划属内蒙古阿拉善盟。两沙漠的地貌景观各具特色,为研究风沙地貌的理想区域,长期以来引起了国内外学者的关注。有关巴丹吉林沙漠的研究主要集中在地貌形态、沙山成因、沙漠地下水及湖泊水来源、沙漠形成年代等方面。关于腾格里沙漠的研究主要集中在该沙漠的东南部,内容涉及沙漠的形成演化史、风沙沉积物、风沙物理及沉积构造等方面。但关于两个沙漠沉积物的系统性研究很少,更没有关于两沙漠沉积物的对比研究。风沙沉积物特征的研究,对确定风沙沉积环境、探索其物源及风沙地貌的形成过程均有着重要的意义。本论文在借助大量详实的野外观测及采样的基础上,对比研究了巴丹吉林-腾格里沙漠地表、典型沉积层位、典型沙丘及断面上沉积物的粒度特征、矿物组成和地球化学元素等内容,为探讨两个沙漠沙物质来源及形成机理提供了重要的依据。本论文获得的主要结论为：
1.巴丹吉林-腾格里沙漠沉积物的粒度分析结果
(1)沉积物的颗粒级配分析表明两沙漠地表沉积物的颗粒组成均以中沙和细沙为主,且巴丹吉林沙漠地表沉积物稍粗于腾格里沙漠。两沙漠不同类型沙丘及不同地貌部位的沙粒级配存在一定的差异：巴丹吉林沙漠的流动沙丘和灌丛沙丘沙粒均以细沙和中沙为主,平沙地和丘间地以粗沙和中沙为主；而腾格里沙漠所有类型沙丘、沙梁和丘间地的沙粒则均以细沙和中沙为主。两沙漠不同沉积层位即垂直剖面上的沙粒粒度组成极为接近,均以细沙和中沙为主。两沙漠沙粒频率分布曲线型态均主要表现为单峰型,但峰值粒径范围存在一定差异,即巴丹吉林沙漠的颗粒频率分布曲线上的峰值粒径范围较广,而腾格里沙漠则相对集中。
(2)粒度参数的分析结果显示：巴丹吉林沙漠地表和垂直剖面上沉积物的平均粒径均粗于腾格里沙漠,而典型沙丘表层颗粒则细于腾格里沙漠；两沙漠沉积物为分选好至分选较好,且巴丹吉林沙漠地表和垂直剖面上的颗粒分选较腾格里沙漠的稍差,而典型沙丘表层沉积物的分选程度则稍好于腾格里沙漠；两沙漠沙粒均为近对称中等峰态分布。
(3)两沙漠沉积物粒度的区域分布规律均较差,但腾格里沙漠沉积物粒度的区域分布规律稍好于巴丹吉林沙漠。
2.巴丹吉林-腾格里沙漠沉积物的矿物分析结果
(1)巴丹吉林-腾格里沙漠主要轻矿物均以石英和长石为主,但巴丹吉林沙漠地表沉积物中轻矿物的比重稍低于腾格里沙漠,且轻矿物成分成熟度也稍低于腾格里沙漠。
(2)巴丹吉林沙漠轻矿物成分成熟度表现为无规律性和反规律性,而腾格里沙漠轻矿物分布则存在一定的区域规律性,即沿主导风向,轻矿物成分成熟度自西北向东南逐渐变好。
(3)巴丹吉林-腾格里沙漠主要重矿物的种类一致,但巴丹吉林沙漠重矿物的含量比重稍高于腾格里沙漠,且巴丹吉林沙漠沉积物的风化程度稍弱于腾格里沙漠,两沙漠的沙丘迎风坡沉积物的风化程度均好于沙丘背风坡。
(4)巴丹吉林沙漠磷灰石的风化程度较腾格里沙漠弱,两沙漠物源区性质非常接近,其源岩均为拥有富含石榴子石的基性酸性岩类,两沙漠沉积物的重矿物成熟度均不高。
3.巴丹吉林-腾格里沙漠沉积物的元素地球化学分析结果
(1)巴丹吉林-腾格里沙漠所含主要常量元素的种类相同,均以SiO2和A1203平均含量较高,除CaO巴丹吉林沙漠相比腾格里沙漠富集外,其他常量元素含量均与腾格里沙漠相接近。与上陆壳(UCC)平均化学成分相比,除Si02外两沙漠其余常量元素均相对亏损。两沙漠不同区域断面上常量元素的曲线分布特征较为一致,但腾格里沙漠沙常量元素的空间分布规律相比巴丹吉林沙漠显著。
(2)巴丹吉林-腾格里沙漠均以Ba元素含量最为丰富,Sr、Co、Cr、Zr和Rb等微量元素平均含量均相对较多,其他微量元素平均含量均较少,除Cu的含量在两沙漠稍有差异外,其余微量元素的平均含量差别不大。与上陆壳(UCC)平均化学成分相比,两沙漠Co和Cr元素相对富集,Ba和Ni元素与UCC含量相当,其他微量元素则表现为迁移淋失。两沙漠不同区域断面微量元素的曲线分布特征较为相似,且区域规律性均不显著。
(3)巴丹吉林-腾格里沙漠沙物质的化学组成虽有差异但差异很小,两沙漠的沉积物均具有很好的均质性,均处在大陆风化的初级阶段,其中腾格里沙漠所经受的化学风化程度稍强于巴丹吉林沙漠。
4.堆积区规律性好于侵蚀区通过对巴丹吉林沙漠和腾格里沙漠沉积物特征的区域对比研究,得出腾格里沙漠沉积物的区域规律性稍好于巴丹吉林沙漠,可见,距离沙源越远,规律性越好。可以推断,在我国西北干旱区,越靠近东南方向,沉积物的区域规律性会变得越好,这就是堆积区规律性好于侵蚀区。
本文通过对巴丹吉林-腾格里沙漠沉积物的粒度特征、矿物和地球化学元素的对比研究,得出两沙漠沉积物特征的异同,对探讨其物源及物质形成过程反演以及风成环境的恢复和重建提供了可靠依据。
Badain Jaran Desert and Tengger Desert are located in the arid area of northwest China. They are bounded by the Yabulai mountain and belong to Alashan League, Inner Mongolia. As their unique geomorphology, it is recognized as the ideal region to study the aeolian geomorphology, hence draw a great attention of the scholars at home and abroad. The studies of Badain Jaran Desert mainly focused on geomorphology, genesis, source of the groundwater and geochronology, et al. The studies of Tengger Desert were mainly done in the southeast area of the desert, focused on genesis and evolution of the desert, aeolian deposits, aeolian physics, sedimentary structure, et al. However, the systematic studies on the material composition are still very little, not to say the contrastive study of the aeolian deposits in the both deserts. The studies on the characteristics of aeolian deposits make great sense in the determining of aeolian sedimentary environment, exploring the source of the aeolian deposits and the evolution of the aeolian geomorphology. In order to do the research, the author collected the samples in the typical surface, different sedimentary layers, typical dune and cross-section of the Badain Jaran Desert and Tengger Desert. And made a comparative study of the representative samples from the characteristic of grain size, mineral composition, and geochemical element and so on, and analysed the similarities and differences of the deposits in the two deserts. These provide an important basis to investigate the source and formation of the sand in the two deserts. The main conclusions are following:
1.The grain size analysis results of the deposits in the Badain Jaran-Tengger Deserts
(1) The grain size composition analysis shows that the sediments of the two deserts are mainly comprised of medium and fine sand, and the surface sediments of Badain Jaran Desert are slightly coarser than that of Tengger Desert. The grain size composition of different type of dunes and different landform positions of the two deserts are different:mobile dunes and shrub canopy dunes of Badain Jaran Desert are mainly composed of fine and medium sand, but flat sandy land and inter-dunes are mainly composed of coarse and medium sand; while all the dunes,ridges,and inter-dunes of Tengger Desert are primarily composed of fine and medium sand.It is similar to the grain size composition in different sedimentary layers namely the vertical section of the two deserts, which are primarily composed by fine and medium sand.The frequency curve is mainly unimodal for dune sands of both deserts, but there are some differences of the peaks'range of grain size, that is the peaks'range of Badain Jaran Desert is broad, while the Tengger Desert is relatively concentrate.
(2) grain size parameters shows that the Badain Jaran Desert's mean grain size of the surface deposits and the longitudinal profile of typical dunes is coarser than that of Tengger Desert, while the surface grain size of typical dunes is finer than that of Tengger Desert. The sorting parameters show that the sediments from the two deserts are better sorted to well sorted with a distribution of near symmetric skewness and mesokurtic.The sediments from the surface and longitudinal profile of Badain Jaran Desert is slightly worse sorted than that of Tengger Desert, while it is slightly better sorted of the sediments from the surface of typical dunes than that of Tengger Desert.
(3) From a regional perspective, The grain size parameters of the sediments from the both deserts have no distinct regional change, but the Tengger Desert is slightly better than the Badain Jaran Desert.
2.The mineral assemblages of sands in the Badain Jaran-Tengger Desert
(1) The main light minerals in Badain Jaran Desert and Tengger Desert are mainly comprised of quartz and feldspar, but the content proportion of the light minerals of surface sediments in Badain Jaran Desert is slightly lower than that of Tengger Desert, and the Light mineral composition maturity in Tengger Desert is also slightly lower than that of Badain Jaran Desert.
(2) From a regional perspective, the light mineral composition maturity shows no regularity and anti-regularity in Badain Jaran Desert. But in Tengger Desert, the light mineral composition maturity shows distinct regional change. That is in the NW-SE cross sections which are parallel to the dominant wind direction, the light mineral composition maturity becoming better.
(3) The types of heavy minerals in both Badan Jaran Desert and Tengger Desert are consistent, but the heavy mineral proportion of sediments in Badan Jaran Desert is slightly higher than that in Tengger Desert. And the weathering degree of the sediments in Badan Jaran Desert is slightly weaker than that in Tengger Desert. The weathering degree of the sediments in windward slope is better than that in leeward slope in both Badain Jaran Desert and Tengger Desert.
(4) The weathering degree of apatite in Badan Jaran Desert is weaker than that in Tengger Desert. The source area of the both deserts is very close. The source of sand is basisc acid rocks, which is rich of garnet. The mineral maturity in the both deserts is not high
3. The geochemical element analysis results
(1) Badain Jaran-Tengger Desert contains the same types of the main major elements, both have a high average content of SiO2 and Al2O3, except the CaO enriches in the Badan Jaran Desert compares to the Tengger Desert, the other major elements contents are similar to the Tengger Desert. Compare to the average chemical composition of the upper continental crust (UCC), except the SiO2, the other major elements of both deserts are suffered a relatively loss. The content distribution curves of major elements of different regional cross sections in the both deserts is more consistent, but the spatial distribution regularity of major elements is more remarkable in Tengger Desert than that of Badan Jaran Desert.
(2) Both Badain Jaran Desert and Tengger Desert are most abundant in Ba, the average content of trace elements, such as Sr、Go、Cr、Zr、Rb and so on are relatively higher, the content of the other trace elements are relatively less. Except the content of Cu are slightly different in both deserts, the average content of the other trace elements have little difference. Compare to the average chemical composition of the upper continental crust(UCC), both deserts are relatively enrich of Co and Cr. The content of Ba and Ni are equivalent to UCC, the other trace elements show migration and lesching out. The content distribution curves of different regional cross sections in the both deserts are similar, and the regional regularity is not remarkable.
(3) There are some difference in the chemical composition of the aeolian deposits in the both deserts, but the difference is tiny. The aeolian deposits of the both deserts are of good homogeneity, which is at the initial stage of continental weathering. The chemical weathering degree in Tengger Desert is slightly stronger than that in the Badain Jaran Desert.
4. Through the contrast studies of desert sedimentary characteristic on regional scale between Badain Jaran Desert and Tenger Desert, this paper draw a conclusion that the regional variation law of desert sedimentary in Tengger Desert is slightly superior to that of desert sedimentary in Badain Jaran Desert. It is inferred that the regional precipitation regularity of desert sedimentary become better and better toward the southeast in arid region in northwest China, that is to say, the precipitation regularity in deposit area is superior to that in erosion area.
Based on the comparative study of the grain size, mineral and geochemical elements of sediments from Badain Jaran Desert and Tengger Desert, this paper obtained the similarities and differences of aeolian sediments'characteristics in the both deserts. This study can provide reliable basis on the discussion of sand source, the inversion of material forming processes, as well as the restoration and reconstruction of aeolian environment of the two deserts.
1.巴丹吉林-腾格里沙漠沉积物的粒度分析结果
(1)沉积物的颗粒级配分析表明两沙漠地表沉积物的颗粒组成均以中沙和细沙为主,且巴丹吉林沙漠地表沉积物稍粗于腾格里沙漠。两沙漠不同类型沙丘及不同地貌部位的沙粒级配存在一定的差异：巴丹吉林沙漠的流动沙丘和灌丛沙丘沙粒均以细沙和中沙为主,平沙地和丘间地以粗沙和中沙为主；而腾格里沙漠所有类型沙丘、沙梁和丘间地的沙粒则均以细沙和中沙为主。两沙漠不同沉积层位即垂直剖面上的沙粒粒度组成极为接近,均以细沙和中沙为主。两沙漠沙粒频率分布曲线型态均主要表现为单峰型,但峰值粒径范围存在一定差异,即巴丹吉林沙漠的颗粒频率分布曲线上的峰值粒径范围较广,而腾格里沙漠则相对集中。
(2)粒度参数的分析结果显示：巴丹吉林沙漠地表和垂直剖面上沉积物的平均粒径均粗于腾格里沙漠,而典型沙丘表层颗粒则细于腾格里沙漠；两沙漠沉积物为分选好至分选较好,且巴丹吉林沙漠地表和垂直剖面上的颗粒分选较腾格里沙漠的稍差,而典型沙丘表层沉积物的分选程度则稍好于腾格里沙漠；两沙漠沙粒均为近对称中等峰态分布。
(3)两沙漠沉积物粒度的区域分布规律均较差,但腾格里沙漠沉积物粒度的区域分布规律稍好于巴丹吉林沙漠。
2.巴丹吉林-腾格里沙漠沉积物的矿物分析结果
(1)巴丹吉林-腾格里沙漠主要轻矿物均以石英和长石为主,但巴丹吉林沙漠地表沉积物中轻矿物的比重稍低于腾格里沙漠,且轻矿物成分成熟度也稍低于腾格里沙漠。
(2)巴丹吉林沙漠轻矿物成分成熟度表现为无规律性和反规律性,而腾格里沙漠轻矿物分布则存在一定的区域规律性,即沿主导风向,轻矿物成分成熟度自西北向东南逐渐变好。
(3)巴丹吉林-腾格里沙漠主要重矿物的种类一致,但巴丹吉林沙漠重矿物的含量比重稍高于腾格里沙漠,且巴丹吉林沙漠沉积物的风化程度稍弱于腾格里沙漠,两沙漠的沙丘迎风坡沉积物的风化程度均好于沙丘背风坡。
(4)巴丹吉林沙漠磷灰石的风化程度较腾格里沙漠弱,两沙漠物源区性质非常接近,其源岩均为拥有富含石榴子石的基性酸性岩类,两沙漠沉积物的重矿物成熟度均不高。
3.巴丹吉林-腾格里沙漠沉积物的元素地球化学分析结果
(1)巴丹吉林-腾格里沙漠所含主要常量元素的种类相同,均以SiO2和A1203平均含量较高,除CaO巴丹吉林沙漠相比腾格里沙漠富集外,其他常量元素含量均与腾格里沙漠相接近。与上陆壳(UCC)平均化学成分相比,除Si02外两沙漠其余常量元素均相对亏损。两沙漠不同区域断面上常量元素的曲线分布特征较为一致,但腾格里沙漠沙常量元素的空间分布规律相比巴丹吉林沙漠显著。
(2)巴丹吉林-腾格里沙漠均以Ba元素含量最为丰富,Sr、Co、Cr、Zr和Rb等微量元素平均含量均相对较多,其他微量元素平均含量均较少,除Cu的含量在两沙漠稍有差异外,其余微量元素的平均含量差别不大。与上陆壳(UCC)平均化学成分相比,两沙漠Co和Cr元素相对富集,Ba和Ni元素与UCC含量相当,其他微量元素则表现为迁移淋失。两沙漠不同区域断面微量元素的曲线分布特征较为相似,且区域规律性均不显著。
(3)巴丹吉林-腾格里沙漠沙物质的化学组成虽有差异但差异很小,两沙漠的沉积物均具有很好的均质性,均处在大陆风化的初级阶段,其中腾格里沙漠所经受的化学风化程度稍强于巴丹吉林沙漠。
4.堆积区规律性好于侵蚀区通过对巴丹吉林沙漠和腾格里沙漠沉积物特征的区域对比研究,得出腾格里沙漠沉积物的区域规律性稍好于巴丹吉林沙漠,可见,距离沙源越远,规律性越好。可以推断,在我国西北干旱区,越靠近东南方向,沉积物的区域规律性会变得越好,这就是堆积区规律性好于侵蚀区。
本文通过对巴丹吉林-腾格里沙漠沉积物的粒度特征、矿物和地球化学元素的对比研究,得出两沙漠沉积物特征的异同,对探讨其物源及物质形成过程反演以及风成环境的恢复和重建提供了可靠依据。
Badain Jaran Desert and Tengger Desert are located in the arid area of northwest China. They are bounded by the Yabulai mountain and belong to Alashan League, Inner Mongolia. As their unique geomorphology, it is recognized as the ideal region to study the aeolian geomorphology, hence draw a great attention of the scholars at home and abroad. The studies of Badain Jaran Desert mainly focused on geomorphology, genesis, source of the groundwater and geochronology, et al. The studies of Tengger Desert were mainly done in the southeast area of the desert, focused on genesis and evolution of the desert, aeolian deposits, aeolian physics, sedimentary structure, et al. However, the systematic studies on the material composition are still very little, not to say the contrastive study of the aeolian deposits in the both deserts. The studies on the characteristics of aeolian deposits make great sense in the determining of aeolian sedimentary environment, exploring the source of the aeolian deposits and the evolution of the aeolian geomorphology. In order to do the research, the author collected the samples in the typical surface, different sedimentary layers, typical dune and cross-section of the Badain Jaran Desert and Tengger Desert. And made a comparative study of the representative samples from the characteristic of grain size, mineral composition, and geochemical element and so on, and analysed the similarities and differences of the deposits in the two deserts. These provide an important basis to investigate the source and formation of the sand in the two deserts. The main conclusions are following:
1.The grain size analysis results of the deposits in the Badain Jaran-Tengger Deserts
(1) The grain size composition analysis shows that the sediments of the two deserts are mainly comprised of medium and fine sand, and the surface sediments of Badain Jaran Desert are slightly coarser than that of Tengger Desert. The grain size composition of different type of dunes and different landform positions of the two deserts are different:mobile dunes and shrub canopy dunes of Badain Jaran Desert are mainly composed of fine and medium sand, but flat sandy land and inter-dunes are mainly composed of coarse and medium sand; while all the dunes,ridges,and inter-dunes of Tengger Desert are primarily composed of fine and medium sand.It is similar to the grain size composition in different sedimentary layers namely the vertical section of the two deserts, which are primarily composed by fine and medium sand.The frequency curve is mainly unimodal for dune sands of both deserts, but there are some differences of the peaks'range of grain size, that is the peaks'range of Badain Jaran Desert is broad, while the Tengger Desert is relatively concentrate.
(2) grain size parameters shows that the Badain Jaran Desert's mean grain size of the surface deposits and the longitudinal profile of typical dunes is coarser than that of Tengger Desert, while the surface grain size of typical dunes is finer than that of Tengger Desert. The sorting parameters show that the sediments from the two deserts are better sorted to well sorted with a distribution of near symmetric skewness and mesokurtic.The sediments from the surface and longitudinal profile of Badain Jaran Desert is slightly worse sorted than that of Tengger Desert, while it is slightly better sorted of the sediments from the surface of typical dunes than that of Tengger Desert.
(3) From a regional perspective, The grain size parameters of the sediments from the both deserts have no distinct regional change, but the Tengger Desert is slightly better than the Badain Jaran Desert.
2.The mineral assemblages of sands in the Badain Jaran-Tengger Desert
(1) The main light minerals in Badain Jaran Desert and Tengger Desert are mainly comprised of quartz and feldspar, but the content proportion of the light minerals of surface sediments in Badain Jaran Desert is slightly lower than that of Tengger Desert, and the Light mineral composition maturity in Tengger Desert is also slightly lower than that of Badain Jaran Desert.
(2) From a regional perspective, the light mineral composition maturity shows no regularity and anti-regularity in Badain Jaran Desert. But in Tengger Desert, the light mineral composition maturity shows distinct regional change. That is in the NW-SE cross sections which are parallel to the dominant wind direction, the light mineral composition maturity becoming better.
(3) The types of heavy minerals in both Badan Jaran Desert and Tengger Desert are consistent, but the heavy mineral proportion of sediments in Badan Jaran Desert is slightly higher than that in Tengger Desert. And the weathering degree of the sediments in Badan Jaran Desert is slightly weaker than that in Tengger Desert. The weathering degree of the sediments in windward slope is better than that in leeward slope in both Badain Jaran Desert and Tengger Desert.
(4) The weathering degree of apatite in Badan Jaran Desert is weaker than that in Tengger Desert. The source area of the both deserts is very close. The source of sand is basisc acid rocks, which is rich of garnet. The mineral maturity in the both deserts is not high
3. The geochemical element analysis results
(1) Badain Jaran-Tengger Desert contains the same types of the main major elements, both have a high average content of SiO2 and Al2O3, except the CaO enriches in the Badan Jaran Desert compares to the Tengger Desert, the other major elements contents are similar to the Tengger Desert. Compare to the average chemical composition of the upper continental crust (UCC), except the SiO2, the other major elements of both deserts are suffered a relatively loss. The content distribution curves of major elements of different regional cross sections in the both deserts is more consistent, but the spatial distribution regularity of major elements is more remarkable in Tengger Desert than that of Badan Jaran Desert.
(2) Both Badain Jaran Desert and Tengger Desert are most abundant in Ba, the average content of trace elements, such as Sr、Go、Cr、Zr、Rb and so on are relatively higher, the content of the other trace elements are relatively less. Except the content of Cu are slightly different in both deserts, the average content of the other trace elements have little difference. Compare to the average chemical composition of the upper continental crust(UCC), both deserts are relatively enrich of Co and Cr. The content of Ba and Ni are equivalent to UCC, the other trace elements show migration and lesching out. The content distribution curves of different regional cross sections in the both deserts are similar, and the regional regularity is not remarkable.
(3) There are some difference in the chemical composition of the aeolian deposits in the both deserts, but the difference is tiny. The aeolian deposits of the both deserts are of good homogeneity, which is at the initial stage of continental weathering. The chemical weathering degree in Tengger Desert is slightly stronger than that in the Badain Jaran Desert.
4. Through the contrast studies of desert sedimentary characteristic on regional scale between Badain Jaran Desert and Tenger Desert, this paper draw a conclusion that the regional variation law of desert sedimentary in Tengger Desert is slightly superior to that of desert sedimentary in Badain Jaran Desert. It is inferred that the regional precipitation regularity of desert sedimentary become better and better toward the southeast in arid region in northwest China, that is to say, the precipitation regularity in deposit area is superior to that in erosion area.
Based on the comparative study of the grain size, mineral and geochemical elements of sediments from Badain Jaran Desert and Tengger Desert, this paper obtained the similarities and differences of aeolian sediments'characteristics in the both deserts. This study can provide reliable basis on the discussion of sand source, the inversion of material forming processes, as well as the restoration and reconstruction of aeolian environment of the two deserts.
引文
[1]董玉祥.“荒漠化”与“沙漠化”[J].科技术语研究,2000,2(4)：18-21.
[2]王涛,吴薇,赵哈林等.沙漠化过程中生物量损失的初步评估—以内蒙古科尔沁地区为例[J].中国沙漠,2005,25(4)：453-456.
[3]董治宝.中国风沙物理研究五十年(1)[J].中国沙漠,2005,25(3)：293-305.
[4]吴正.风沙地貌学[M].北京：科学出版社,1987：98-153.
[5]Livingstone I, Warren A. Aeolian Geomorphology[M].Landon:Addison Wesley Longman Limited,1996,64-101.
[6]杨景春,李有利.地貌学原理[M].北京：北京大学出版社,2007.
[7]Stein M A. Explorations in Central Asia,1906-8[J]. Geographical Journal,1909,58:241-271.
[8]Thomas B. A journey into Rub'al Khali the Southern Arabian Desert[J]. Geographical Journal, 1931,80:1-37.
[9]Beadnell H J L. The sand dunes of the Libyan Desert[J]. Geographical Journal,1910,35: 379-395.
[10]Hogbom I. Ancient inland dunes of northern and middle Europe[J]. Geographical Annal,1923, 5:113-243.
[11]Udden J A. Mechanical composition of some clastic sediments[J]. Geological Society of America, Bulletin,1914,25:655-744.
[12]Cornish V. Limits of form and magnitude of desert dunes[J]. Nature,1928,121:620-622.
[13]费道罗维奇B A.等著.陈治平等译.沙漠地貌的起源及其研究方法(译文集)[M].北京：科学出版社,1962.
[14]Bagnold R A. The Physics of Blown Sand and Desert Dunes[M]. London:Methuen,1941: 25-28,38-41.
[15]兹纳门斯基A N著.杨郁华译,朱震达校.沙地风蚀过程的实验研究和沙堆防止问题[M].北京：科学出版社,1960.
[16]Mckee E D. Structures of dunes at White Sands National Monument, New Mexico[J]. Sedimentology,1966,7:3-69.
[17]Mckee E D编著.赵兴梁译.世界沙海的研究[M].银川：宁夏人民出版社,1993.
[18]Greeley R. Iversen J D. Wind as a Geological Process[M]. Cambridge:Cambridge University Press,1985.
[19]Folk R.L. Longitudinal dunes of the Northwestern edge of the Simpson Desert, Northern Territory, Australia.1. Geomorphology and grain size relationships[J]. Sedimentology,1971,16: 5-54.
[20]Glennie K. W. Desert Sedimentary Environments[M]. Amsterdam:Elsevier,1970.
[21]White B R. Laboratory simulation of aeolian sand transport and physical modeling of flow around dunes[J]. Annals of Arid Zone,1996,35(3):187-214.
[22]Lancaster N. The role of field experiments in studies of dune dynamics and morphology [J]. Annals of Arid Zone,1996,35:171-186.
[23]Livingtone I, Warren A. Aeolian Geomorphology:An Introduction[M]. London:Longman,1996.
[24]Lancaster N. Geomorphology of Desert Dunes [M]. London:Routledge,1995.
[25]Cook R U, Warren A, Goudie A S. Desert Geomorphology [M]. London:UCL Press,1993.
[26]Lancaster N. Control of eolian dune size and spacing [J]. Geology,1988,16:972-975.
[27]Lancaster N. The Namib Sand Sea:Dune Forms, Processes, and Sediments [M]. Balkema: Rotterdam,1989.
[28]Lancaster N. Relations between dune generations in the Gran Desierto of Mexico [J]. Sedimentology,1992,39:631-644.
[29]Lancaster N. Origin of the Gran Desierto Sand Sea:Sonora, Mexico:evidence from dune morphology and sediments In Desert Aeolian Processes, Tchakerian VP (ed.) [M]. New York: Chapman and Hall,1995:11-36.
[30]Liu CQ, Masuda A, Okada A, et al. A geochemical study of loess and desert sand in northern China:implications for continental crust weathering and composition [J]. Chemical Geology, 1993,106:350-374.
[31]Honda M, Shimizu H. Geochemical, mineralogical and sedimentological studies on the Taklimakan Desert sands [J]. Sedimentology,1998,45:1125-1143.
[32]Livingstone I, Bullard JE, Wiggs GFS, et al. Grain-size variation on dunes in the Southwest Kalahari, Southern Africa[J]. Journal of Sedimentary Research,1999,69:546-552.
[33]Kasper-Zubillaga JJ, Dickinson WW. Discriminating depositional environments of sands from modern source terranes using modal analysis [J]. Sedimentary Geology,2001,143:149-167.
[34]Honda M, Yabuki S, Shimizu H. Geochemical and isotopic studies of aeolian sediments in China [J]. Sedimentology,2004,51:211-230.
[35]Muhs DR. Mineralogical maturity in dune fields of North America, Africa and Australia [J]. Geomorphology,2004,59:247-269.
[36]Wang X., Dong Z., Zhang J., et al. Grain size characteristics of dune sands in the central Taklimakan Sand Sea [J]. Sedimentary Geology,2003,161:1-14.
[37]Sweet M. L., Nielson J., Havholm K., et al. Algodones dune field of southern California:case history of a migrating modern dune field [J]. Sedimentology,1988,35:939-952.
[38]Ahlbrandt T. Textural parameters of eolian deposits. In:McKee E. D. (ed.), A study of global sand seas [J]. USGS Professional Paper,1979,1052:21-51.
[39]Lancaster, N. Grain size characteristics of Namib Desert linear dunes [J]. Sedimentology,1981, 28:115-122.
[40]Watson, A. Grain-size variations on a longitudinal dune and a barchan dune [J]. Sedimentary Geology,1986,46,49-66.
[41]Livingstone, I. Grain-size variation on a 'complex' linear dune in the Namib Desert. In:Frostick, L., Reid, I. (Eds.), Desert Sediments, Ancient and Modern. Geological Society Special Publication [C]. Blackwell:Oxford,1987,35:281-291.
[42]Livingstone, I. Temporal trends in grain-size measures on a linear sand dune [J]. Sedimentology, 1989,36:1017-1022.
[43]Rubin, D.M., Hunter, R.E. Why deposits of longitudinal dunes are rarely recognized in the geological record [J]. Sedimentology,1985,32:147-157.
[44]Bristow, C.S., Bailey, S.D., Lancaster, N. The sedimentary structure of linear sand dunes [J]. Nature,2000.406:56-59.
[45]Bagnold, R.A. The size-grading of sand by wind. Proceeding of the Royal Society of London [C]. London:The Royal Society,1937,250-264.
[46]Bagnold, R.A., Barndorff-Nielsen, O.E. The pattern of natural size distributions [J]. Sedimentology,1980,27:199-207.
[47]Tsoar, H. Two-dimensional analysis of dune profiles and the effect of grain size on sand dune morphology. In:El-Baz, F., Hassan, M.H.A. (Eds.), Physics of Desertification[C]. Martinus Nijhof:The Hague,1986,94-108.
[48]Pye, K., Tsoar, H. Aeolian Sand and Sand Dunes [M]. London:Unwin Hyman,1990.
[49]Thomas, D.S.G. Analysis of linear dune sediment-form relationships in the Kalahari Dune Desert [J]. Earth Surface Processes and Landforms,1988,13:545-553.
[50]Wasson, R.J. Dune sediment types, sand color, sediment provenance and hydrology in the Strzelecki-Simpson dunefield, Australia. In:Brookfield, M.E., Ahlbrandt, T.S. (Eds.), Eolian Sediments and Processes[C]. Elsevier:Amsterdam,1983,165-195.
[51]Waitt, M.B.C. Desert dunes of the Kermit Sandhills, Winkler County, Texas [D]. Texas:The University of Texas, USA,1969.
[52]Sneh, A., Weissbrod, T. Size-frequency distribution on longitudinal dune ripple flank sands compared to that of slip face sands of various dune types[J]. Sedimentology,1983,30:717-726.
[53]Goudie, A., Warren, A., Jones, D., et al. The character and possible origins of the aeolian sediments of the Wahiba sand sea, Oman [J]. Geography,1987,153 (2),231-256.
[54]Hastenrath, S.L. The barchans of the Arequipa region, southern Peru[J]. Geomorphology,1967, 11:300-331.
[55]朱震达,吴正,刘恕,等.中国沙漠概论[M].北京：科学出版社,1980：40-45.
[56]朱震达、陈治平、吴正,等.塔克拉玛干沙漠风沙地貌研究[M].北京：科学出版社,1981：44-47,107-108.
[57]李志忠,关有志,孙忠.塔里木沙漠石油公路沿线新月形沙丘的地貌特征[J].新疆大学学报(自然科学版),1998,(1)：80-90.
[58]李志忠.新月形沙丘研究进展综述[J].干旱区地理,1994,17(4)：81-87.
[59]闫满存,王光谦,李保生,等.巴丹吉林沙漠高大沙山的形成发育研究[J].地理学报,2001,56(1)：83-91.
[60]屈建军,常学礼,董光荣,等.巴丹吉林沙漠高大沙山典型区风沙地貌的分形特性[J].中国沙漠,2003,23(4)：361-365.
[61]杨萍,邹学勇,哈斯,等.巴丹吉林沙漠北部风沙地貌形态类型的分区研究[J].中国沙漠,1999,19(3)：210-213.
[62]张伟民,王涛.巴丹吉林沙漠高大沙山形成演化初步探讨[J].中国沙漠,2005,25(2)：281-286.
[63]张伟民,李孝泽,屈建军,等.金字塔沙丘地表气流场及其动力学过程研究[J].中国沙漠,1998,18(3)：215-220.
[64]下训明,董治宝,屈建军.塔克拉玛干沙漠简单横向沙丘形态学示量特征[J].兰州大学学报(自然科学版),2002,38(6)：110-116.
[65]李恒鹏,陈广庭,薛东前.塔克拉玛干沙漠腹地复合沙垄的流场和和上覆沙丘组合及动态特征[J].干旱区地理,2001,24(1)：80-85.
[66]李恒鹏,陈广庭.塔克拉玛干沙漠腹地复合沙垄间地新月形沙丘的逆向演变[J].中国沙 漠,1999,19(2)：134-138.
[67]李生宇,雷加强,徐新文,等.草方格固沙带对垄间新月形沙丘形态和移动的影响[J].干旱区地理理,2006,29(5)：632-638.
[68]凌裕泉,吴正,刘绍中,等.新月形沙丘形态的模拟实验研究[J].地理学报,1998,18(1)：88-93.
[69]李志忠,武胜利,李万娟,等.最近10年来新疆风沙地貌研究进展[J].干旱区研究,2008,25(2)：295-303.
[70]董治宝,屈建军,卢琦,等.关于库姆塔格沙漠“羽毛状”风沙地貌的讨论[J].中国沙漠,2008,28(6)：1005-1091.
[71]屈建军,郑本兴,俞祁浩,等.罗布泊东阿奇克谷地雅丹地貌与库姆塔格沙漠形成的关系[J].中国沙漠,2004,24(3)：294-302.
[72]屈建军,左国朝,张克存,等.库姆塔格沙漠形成演化与区域新构造运动关系研究[J].干旱区地理,2005,28(4)：424-428.
[73]刘虎俊,赵明,王继和,等.库姆塔格沙漠南部的风积地貌特征[J].干旱区资源与环境,2005,19(7)：130-134.
[74]刘虎俊,王继和,廖空太,等.库姆塔格沙漠“羽毛状沙丘”形态的示量特征[J].干旱区地理理,2006,29(3)：314-320.
[75]哈斯,董光荣,王贵勇.腾格里沙漠东南缘格状沙丘的形态动力学研究[J].中国科学(D),1999,29(5)：466-471.
[76]贺大良.风沙地貌形成机制的几个问题[J].中国沙漠,1985,5(1)：33-37.
[77]赵景峰,李崇顺,周兴佳,等.新月形沙丘丘表流场与沙丘蚀积特征[J].中国沙漠,1993,13(3)：18-27.
[78]李志忠,陈广庭.金字塔沙丘风洞流场结构的实验研究[J].中国沙漠,1995,15(3)：227-232.
[79]凌裕泉,刘绍中,吴正,等.金字塔沙丘形成的动力条件分析[J].中国沙漠,1997,17(2)：112-118.
[80]张春来,董光荣,董治宝,等.用风洞实验方法计算土壤风蚀量的时距问题[J].中国沙漠,1996,16(2)：200-203.
[81]刘连友.区域风沙蚀积量和蚀积强度初步研究：以晋陕蒙接壤区为例[J].地理学报,1999,54(1)：60-68.
[82]中国科学院兰州沙漠研究所额济纳旗考察队.乌兰布和沙漠西南铁路沿线沙害防治[J].中国沙漠,1983,3(2)：30-35.
[83]李银芳,周兴佳,潘伯荣,等.兰新铁路哈密地区的沙害[J].中国沙漠,1986,6(4)：56-62.
[84]董治宝,陈广庭,韩致文,等.塔里木沙漠石油公路风沙危害[J].环境科学,1997,18(1)：4-9.
[85]刘铁良,陈昌秀.不易沙埋的铁路路基断面形式问题[J].中国沙漠,1984,4(1)：31-37.
[86]刘贤万,崔志刚.特大风区防翻车挡风墙工程设计的风洞实验研究[J].中国沙漠,1994,14(3)：38-46.
[87]刘贤万,凌裕泉,贺大良,等.下导风工程的风洞实验研究：(1)平面上的实验[J].中国沙漠,1982,2(4)：14-21.
[88]刘贤万,凌裕泉,贺大良,等.下导风工程的风洞实验研究：(2)地形条件下的实验.中国沙漠,1982,3(3)：25-34.
[89]刘贤万.草方格沙障的风洞实验.流沙治理研究(二)[M].银川：宁夏人民出版社，1991：326-334.
[90]徐峻龄,裴章勤,王仁化.半隐蔽式麦草方格沙障防护带宽度的探讨[J].中国沙漠,1982,2(3)：16-23.
[91]卫林.论林带的有效防护距离[J].科学通报,1985,19：1567-1569.
[92]Zhang Weimin, Qu Jianjun, Dong Zhibao, et al. The airflow field and dynamic processes of pyramid dunes [J]. Journal of arid Environments,2000,45:357-368.
[93]Wang Tao, Zhang Weimin, Dong Zhibao, et al. The dynamic characteristics and migration of a pyramid dune [J]. Sedimentology,2005,52:429-440.
[94]Liu Xianwan, Lisen, Shen Jianyou. Wind tunnel simulation experiment of mountain dunes [J]. Journal of Arid Environments,1999,42:49-59.
[95]李振山,倪晋仁.风成沙纹发育过程中形态变化的风洞实验研究[J].应用基础与工程科学学报,2003,11(3)：247-254.
[96]马玉明,姚洪林.光电子集沙仪对毛乌素沙地沙丘蚀积过程的观测[J].中国沙漠,2001,21(增刊)：68-71.
[97]武生智,马崇武,苗天德.沙粒级配和沙丘分布的分形研究[J].中国沙漠,1999,19(3)：247-250.
[98]王建成,武生智,马崇武.沙丘背风坡的净力学稳定性分析[J].中国沙漠,2001,21(增刊):84-86.
[99]王训明,董治宝,屈建军.塔克拉玛干沙漠简单线形沙丘形态-动力学过程研究[J].中国沙漠,2003,23(3)：257-262.
[100]哈斯,庄燕美,王蕾,等.毛乌素沙地南缘横向沙丘粒度分布及其对风向变化的响应[J].地理科学进展,2006,25(6)：42-51.
[101]哈斯.腾格里沙漠东南缘格状沙丘粒度特征与成因探讨[J].地理研究,1998,17(2)：178-184.
[102]哈斯,王贵勇.沙坡头地区新月形沙丘粒度特征[J].中国沙漠,2001,21(3)：271-275.
[103]哈斯,王贵勇.腾格里沙漠东南缘横向沙丘粒度变化及其与坡面形态的关系[J].中国沙漠,1996,16(2)：216-221.
[104]钱亦兵,张希明,李晓明.塔克拉玛干沙漠南缘绿洲沙物质粒度特征[J].中国沙漠,1995,]5(2)：131-135.
[105]钱亦兵,周兴佳,吴兆宁.准噶尔盆地沙物质粒度特征研究[J].干旱区研究,2000,17(2)：34-41.
[106]钱亦兵,周兴佳,李崇舜,等.准噶尔盆地沙漠沙矿物组成的多源性[J].中国沙漠,2001,21(2)：182-187.
[107]钱亦兵,吴兆宁,杨海峰,等.古尔班通古特沙漠南部风沙土粒度分布的空间异质性[J].干旱区地理,2009,32(5)：655-661.
[108]陈渭南.塔克拉玛干沙漠84°E沿线沙物质的粒度特征[J].地理学报,1993,48(1)：33-46.
[109]陈渭南,雷加强.塔克拉玛干沙漠新月形沙丘不同部位的粒度特征[J].干旱区资源与环境,1992,6(2)：101-110.
[110]李振山,陈广庭,冯起,等.塔克拉玛干沙漠腹地纵向沙垄表面沙物质粒度特征[J].干旱区资源与环境,1998,12(1)：21-28.
[111]赵元杰,周兴佳.塔里木沙漠公路沿线沙物质特征及环境意义[J].干旱区研究,1999,16(3)：53-58.
[112]赵元杰,夏训诚,王富葆,等.罗布泊地区红柳沙包纹层沙粒度特征与环境指示意义[J].干旱区地理,2007,30(6)：791-796.
[113]温小浩,李宝生,李森,等.2.5kaBP以来额济纳绿洲沙丘的粒度特征及其反映的沉积过程[J].地质学报,79(5)：710-718.
[114]吉启慧.克里雅河流域沉积物的粒度特征[J].干旱取研究,1992,9(3)：48-56.
[115]吉启慧.粒度分析在塔克拉玛干沙漠中的应用[J].中国沙漠,1996,16(2)：173-179.
[116]韩广,张桂芳,杨文斌.呼伦贝尔沙地沙丘沙来源的定量分析[J].地理学报,2004,59(2)：189-186.
[117]王训明,董治宝,屈建军,等.塔克拉玛干沙漠简单线形沙丘形态动力学过程研究[J].中国沙漠,2003,23(3)：257-262.
[118]王训明,陈广庭.塔里木沙漠石油公路半隐蔽式沙障区与流沙区沙物质粒度变化[J].中国沙漠,1996,16：(2)：180-184.
[119]黄杏珍,潘中海.应用粒度资料探讨毛乌素沙漠西南部的风沙特征[J].地理学报,1981,36(1)：70-78.
[120]季方,叶玮,魏文寿.古尔班通古特沙漠固定与半固定沙丘成因初探[J].干旱区地理理,2000,23(1)：32-36.
[121]张瑞军,何清,孔丹,等.塔克拉玛干沙漠北缘沙尘暴源区地表沉积物粒度特征[J].干旱区研究,2008,25(6)：887-883.
[122]魏怀东,徐先英,王继和,等.库姆塔格沙漠沙丘的粒度特征[J].水土保持学报,2007,21(3)：6-9.
[123]魏怀东,王继和,徐先英,等.库姆塔格沙漠各沙丘类型沙粒粒度分析[J].甘肃科技,2007,23(5)：85-88.
[124]何清,杨兴华,霍文,等.库姆塔格沙漠粒度分布特征及环境意义[J].中国沙漠,2009,29(1)：18-22.
[125]唐进年,王继和,苏志珠,等.库姆塔格沙漠羽毛状沙丘表面沙粒度分布特征[J].干旱区地理,2008,31(6)：918-925.
[126]张宇红,李保生,靳鹤龄,等.萨拉乌苏河流域150 ka BP以来的粒度旋回[J].地理学报,2001,56(3)：332-344.
[127]魏文寿.沙漠表层粒度与水热变化的环境效应分析—以古尔班通古特沙漠为例[J].沉积学报,1998,16(1)：152-157.
[128]冯起,陈广庭,朱震达.塔克拉玛干沙漠北部全新世环境演变(Ⅰ)[J].环境科学学报,1996,16(2)：238-244.
[129]李志忠.塔里木石油公路沿线风成沙特征及其区域分异[J].新疆师范大学学报(自然科学版),1996,15(4)：52-62.
[130]李志忠,关有志,孙忠贾,等.塔克拉玛干沙漠腹地纵向沙垄的粒度分布特征[J].干旱区研究,1996,13(2)：37-43.
[131]张虎才.撒哈拉沙漠东北部苏丹境内东西断面粒度分布特征及其成因与环境[J].中国沙漠,1996,16(3)：242-246.
[132]贾铁飞,何雨,裴东.鸟兰布和沙漠北部沉积物特征及环境意义[J].干旱区地理,1998,21(2)：36-42.
[133]Weltje G J, von Eynatten H. Quantitative provenance analysis of sediments:review and outlook[J]. Sedimentary Geology,2004,171(1-4):1-11.
[134]Garzanti E, Vezzoli G, Ando S et al. Quantifying sand provenance and erosion (Marsyandi River, Nepal Himalaya) [J].Earth and Planetary Science Letters,2007,258(3-4):500-515.
[135]Nesbitt H, Young G. Petrogenesis of sediments in the absence of chemical weathering:Effects of abrasion and sorting on bulk composition and mineralogy[J]. Sedimentology,1996,43(2): 341-358.
[136]Nesbitt H, Markovics G. Weathering of granodioritic crust, long-term storage of elements in weathering profiles, and petrogenesis of siliciclastic sediments[J]. Geochimica et Cosmochimica Acta,1997,61(8):1653-1670.
[137]Muhs D. Mineralogical maturity in dunefields of North America, Africa and Australia[J]. Geomorphology,2004,59(1-4):247-269.]
[138]Nesbitt H W, Young G M. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites [J]. Nature,1982,299(21):715-717.
[139]Ding Z L, Sun J M, Yang S L et al. Geochemistry of the Pliocene red clay formation in the Chinese Loess Plateau and implications for its origin, source provenance and paleoclimate change[J]. Geochimica et Cosmochimica Acta,2001,65(6):901-913.
[140]Chen J, An Z. S., Liu L. W., et al. Variations in chemical compositions of the eolian dust in Chinese Loess Plateau over the past 2.5Ma and chemical weathering in the Asian inland[J]. Science in China:Series D,2001,31(2):136-145.
[141]Ujvari G., Varga A., Balogh-Brunstad Z. Origin weathering, and geochemical composition of loess in southwestern Hungary [J]. Quaternary Research,2008,69(3):421-437.
[142]宋锦熙.北京地区沙物质的重矿物成分、结构特征与风沙的沙物质来源[J].中国沙漠,1987,17(1)：24-33.
[143]钱亦兵.新疆伊犁塔克尔穆库尔沙漠沙的特征与沙源的关系[J].中国沙漠,]985,5(2)：36-43.
[144]钱亦兵,石井武政,水野清秀.塔克拉玛干沙漠和田河流域沙漠沙物质来源初探[J].干旱区研究,1991,(4)：48-51.
[145]钱亦兵,吴兆宁,石井武政,等.塔克拉玛干沙漠沙物质成分特征及其来源[J].中国沙漠,1993,13(4)：32-38.
[146]钱亦兵,吴兆宁,金井丰,等.塔克拉玛干沙漠沙物质成分研究[J].干旱区研究,1994,11(4)：46-52.
[147]谢静,丁仲礼.中国东北部沙地重矿物组成及沙源分析[J].中国科学D辑：地球科学,2007,37(8)：1065-1072.
[148]Yang, X. P., Zhang, F., Fu, X. D., et al. Oxygen isotopic compositions of quartz in the sand seas and sandy lands of northern China and their implications for understanding the provenances of aeolian sands [J]. Geomorphology,2008,102:278-285
[149]刘宝珺.沉积岩石学[M].北京：地质出版社,1980：126.
[150]邵磊.陆源碎屑岩地球化学在盆地分析中的应用[J].地学前缘,2000,7(3)：297-304.
[151]张小曳,张光宇,朱光华,等.中国源区粉尘的元素示踪[J].中国科学(D辑),1996,26(5)：423-430.
[152]孙业乐,庄国顺,袁蕙,等.2002年北京特大沙尘暴的理化特性及其组分来源分析[J].科学通报,2004,49(4)：340-346.
[153]孙继敏.中国黄十的物质来源及其粉尘的产生机制与搬运过程[J].第四纪研究,2004,24(2)：175-183.
[154]谢远云,何葵,周嘉,等.哈尔滨沙尘暴的化学特征及其物质源探讨[J].地理研究,2006,25(2)：255-261.
[155]陈骏,季峻峰,仇纲,等.陕西洛川黄十化学风化程度的地球化学研究[J].中国科学(D辑)，1997，27(6)：531-536
[156]陈骏,安芷生,刘连文,等.最近2.5 Ma以来黄土高原风尘化学组成的变化与亚洲内陆的化学风化[J].中国科学(D辑),2001,31(2)：136-144
[157]Ohta T, Arai H. Statistical empirical index of chemical weathering in igneous rocks:A new tool for evaluating the degree of weathering [J]. Chemical Geology,2007,240(3-4):280-297.
[158]Chen J, Ji J F, Chou G et al. Geochemistry of the chemical weathering intensity of the loess profile in Luochuan,Shaanxi Province[J]. Science in China:Series D,1997,27(6):531-536.
[159]徐志伟,鹿化煜,赵存法,等.库姆塔格沙漠地表物质组成、来源和风化过程[J].地理学报,2010,65(1)：53-64.
[160]Mckee E D. A Study of Global Sand Seas [M]. Washington:U. S. Government Printing Office, 1979:12-67.
[161]王涛.巴丹吉林沙漠形成演变的若干问题[J].中国沙漠,1990,10(1)：29-40.
[162]董光荣,高全洲,邹学勇,等.晚更新世以来巴丹吉林沙漠南缘气候变化[J].科学通报,1995,40：1214-1218.
[163]Jakel D. The Badain Jaran Desert:its o rigin and development [J]. Geow issenschaf en, 1996(78):272-274.
[164]Petroy M P. Theordos, alanshan and peishan, the deserts of Central Asia [J]. Research Service, 1966(1):241-260.
[165]Dong Zhibao, Wang Tao,Wang Xunming. Geomorphology of the megadunes in the Badain Jaran Desert [J]. Geomorphology,2003,60:1-13.
[166]陆锦华,Jakel D巴丹吉林沙漠及其毗邻地区地貌图(1：50万)[M].兰州：兰州大学出版社,1998.
[167]杨小平.近3万年来巴丹吉林沙漠的景观发育与雨量变化[J].科学通报,2000,45(4)：428-434.
[168]朱震达.中国沙漠、沙漠化、荒漠化及其治理的对策[M].北京：中国环境出版社,1999：137-142.
[169]楼桐茂.甘肃民勤至巴丹吉林庙间沙漠成因及其改造利用.治沙研究(第三号)[C].1962：90-95.
[170]孙培善,孙德钦.内蒙古高原西部水文地质初步研究.治沙研究(第六号)[C].北京：科学出版社,1964：245-317.
[171]谭见安.内蒙古阿拉善荒漠的类型.地理集刊(第八号)[C].北京：科学出版社,1964：1-31.
[172]Lancaster N. Palaeoclimatic evidence from sand seas [J]. Paleoclimatology,1990,76: 279-290.
[173]Hofmann J. Lakes in the SE part of Badain Jaran Shamo, their limnology and geochemistry[J]. Geowissenschaften,1996,14(7-8):275-278.
[174]Geyh M A,Gu Weizu,Jakel D. Groundwater recharge study in the Gobi Desert, China [J].Geowissenschaflen,1996,7(8):279-280.
[175]Yang X. P., Williams M. A. J. The ion chemistry of lakes and Late Holocene desiccation in the Badain Jaran Desert, lnner Mongolia, China [J]. Catena,2003,51(1):45-60.
[176]Yang Xiaoping. Geomorphologische Untersuchungen in Trockenreamen NW-China unter besonderer Berocksichtigung von Badanjilin and Takelamagan [J]. Gettinger Oeographische Abhandlungen,1991,96:1-124.
[177]Yang X. P., Liu T. S.,Xiao H.L., Evolution of megadunes and lakes in the Badain Jaran Desert, Inner Mongolia, China during the last 31000 years[J].Quatermary International,2003,104: 99-112.
[178]陈建生,赵霞,汪集旸,等.巴丹吉林沙漠湖泊钙华与根状结核的发现对研究湖泊水补给的意义[J].中国岩溶，2004,23(4)：277-282.
[179]Chen J. S., Li L., Wang J. Y., et al. Groundwater maintains dune landscape [J]. Nature, 2004,432,459-460.
[180]杨小平,刘东生.距今30ka前后我国西北沙漠地区古环境[J].第四纪研究,2003,23(1)：25-30.
[181]张虎才,马玉贞,彭金兰,等.距今42-18ka腾格里沙漠古湖泊及古环境[J].科学通报,2002,47(24)：1847-1857.
[182]高全洲,董光荣,李保生,等.晚更新世以来巴丹吉林南缘地区沙漠演化[J].中国沙漠,1995,15(4)：345-352.
[183]Yang X. Late Quaternary evolution and paleoclimates, Western Alashan Plateau, Inner Mongolia, China [J]. Z. Geomorph. N. F.,2001,45:1-16.
[184]德日进.中国之大陆沉积[J].中国地质学会志(丁文江先生纪念册),1937,16：195-220.
[185]周廷儒.新生代古地理.《中国自然地理》编辑委员会.中国自然地理古地理(上册)[C].北京：科学出版社,1984：1-233.
[186]李吉均,方小敏.新生代晚期青藏高原强烈隆起及其对周边环境的影响[J].第四纪研究,2001,21(5)：381-391.
[187]张川波,何元良.辽宁北票附近中侏罗世晚期的沙漠沉积[J].沉积学报,1983,1(4)：48-58.
[188]郭正堂,彭淑贞,郝青振,等.晚第三纪中国西北干旱化的发展及其对北极冰盖形成演化和青藏高原隆升的关系[J].中国第四纪研究,1999,(6)：556-567.
[189]杨东,方小敏,董光荣,等.1.8Ma BP以来陇西断岘黄土剖面沉积特征及其反映的腾格里沙漠演化[J].中国沙漠,2006,26(1)：6-13.
[190]闫满存,董光荣,陶贞,等.滕格里沙漠东南缘晚第三纪古风成沙及其环境[J].中国沙漠,1992,12(3)：10-15.
[191]闫满存,董光荣,李保生,等.腾格里沙漠东南缘沙漠演化的初步研究[J].中国沙漠,1998,18(2)：111-117.
[192]强明瑞,李森,金明,等.60ka来腾格里沙漠东南缘风成沉积与沙漠演化[J].中国沙漠,2000,20(3)：256-259.
[193]董光荣,李森,等.中国沙漠形成演化的初步研究[J].中国沙漠,1991,11(4)：23-32.
[194]哈斯.腾格里沙漠东南缘沙丘形态示量特征及其影响因素[J].中国沙漠,1995,15(2)：136-142.
[195]张克存,屈建军,姐瑞平,等.腾格里沙漠东南缘风沙活动动力条件分析—以沙坡头地区为例[J].干旱区地理,2008,31(5)：643-649.
[196]哈斯.腾格里沙漠东南缘沙丘表面风沙流结构变异的初步研究[J].科学通报,2004,49(11)：1099-1104.
[197]哈斯,王贵勇,董光荣.腾格里沙漠东南缘沙丘迎风坡风速变化的初步研究[J].干旱区地理,1999,22(1)：41-46.
[198]张克存,俎瑞平,屈建军,等.腾格里沙漠东南缘输沙势与最大可能输沙量之比较[J].中国沙漠,2008,28(4)：605-610.
[199]哈斯.腾格里沙漠东南缘格状沙丘沉积构造的解析[J].地学前沿,2004,11(1)：277-278.
[20]吴泰然,何国琦.阿拉善地块北缘的蛇绿混杂岩带及其大地构造意义[J].现代地 质,1992.6(3)：286-295.
[201]王廷印,王士政,王金荣.阿拉善地区古生代岩石圈形成与演化[M].兰州：兰州大学出版社,1994.
[202]王廷印,张铭杰,王金荣,等.恩格尔乌苏冲断带特征及大地构造意义[J].地质科学,1998,33(4)：385-394.
[203]张虎才,马玉贞,李吉均.腾格里沙漠南缘全新世古气候变化初步研究[J].科学通报,1998,43(2)：1252-1256.
[204]裴浩,敖艳红,李云鹏等.内蒙古阿拉善地区气候区划研究[J].干旱区资源与环境,2000,14(3)：76-76.
[205]刘振敏,崔天秀,丰创等.腾格里沙漠地区钾芒硝的首次发现及地质意义[J].矿物岩石地球化学通报,1998,17(1)：62-65.
[206]郭绍礼.腾格里沙漠东部的湖盆与风沙地貌特征.中国科学院治沙队.治沙研究(第四号)[C].北京：科学出版社,1962：76-80.
[207]成都地质学院陕北队.沉积岩(物)粒度分析及其应用[M].北京：地质出版社,1978.
[208]Cornillault J. Particle size analyzer [J]. Applied Optics,1972,11:265-268.
[209]Weiss E. L., Frock H. N. Rapid analysis of particle-size distributions by laser light scattering[J]. Powder Technology,1976,14:287-293.
[210]Weiner B. B. Particle and spray sizing using laser diffraction [J]. Society Photo-Optical Instrumentation Engineers,1979,170:53-56.
[211]Mc Cave I.. N., Bryant R. S., Cook H. F., et al. Evaluation of a laser-diffraction-size analyzer for use with natural sediments [J]. Journal of Sedimentary Petrology,1986,56:561-564.
[212]Loizeau J L, Arbouille D, Santiago S,et al. Evaluation of a wide range laser diffraction grain size analyzer for use with sediments [J]. Sedimentology,1994,41:353～361.
[213]Konert M., Vandenderghe J. Comparison of laser grain size analysis with pipette and sieve analysis:a solution for the underestimation of the clay fraction [J]. Sedimentology,1997,44: 523-535.
[214]Singer J. K., Anderson J. B., Ledbetter M. T., et al. An assessment of analytical techniques for the size analysis of fineg-rained sediments [J]. Journal of Sedimentary Petrology,1988,58: 534-543.
[215]Prins M. A., Postma G.,Weltje G. Controls on the terrigenous sediment supply to the Arabian Sea during the late Quaternary:The Markran continental slope[J]. Marine Geology,2000,169: 351-371.
[216]Prins,A., Vandenberghe,J., Weltje,G. J. Palaeoclimate signals in loess size distributions[J]. Workshop HWK Delmenhorst From Particle Size to Sediment Dynamics,2004,123-125.
[217]鹿化煜,安芷生.前处理方法对黄土沉积物粒度测量影响的实验研究?[J].科学通报,1997,42(23)：2535-2538.
[218]程鹏,高抒,李徐生.激光粒度仪测试结果及其与沉降法、筛析法的比较[J].沉积学报,2001,19(3)：449-455.
[219]鹿化煜,苗晓东,孙有斌.前处理步骤与方法对风成红黏土粒度测量的影响[J].海洋地质与第四纪地质,2002,22(3)：129-135.
[220]庞奖励,黄春长,贾耀峰.不同方法测定黄土和和古土壤样品粒度的比较[J].陕西师范大学学报(自然科学版),2003,31(4)：87-92.
[221]王君波,朱立平.不同前处理对湖泊沉积物粒度测量结果的影响.湖泊科学,2005,17(1)：17-23.
[222]孙有斌,高抒,鹿化煜.前处理方法对北黄海沉积物粒度的影响.海洋与湖沼,2001,32(6)：665-671.
[223]徐树建,杜忠花.激光粒度仪测量风成堆积物粒度的实验研究[J].水土保持研究,2007,14(2)：209-212.
[224]雷国良,张虎才,张文翔,等Mastersize2000型激光粒度仪分析数据可靠性检验及意义—以洛川剖面S4层古土壤为例[J].沉积学报,2006,24(4)：531-539.
[225]王德杰,范代读,李从先.不同预处理对沉积物粒度分析结果的影响[J].同济大学学报,2003,31(3)：314-318.
[226]杨玉颖,张学文,赵红,等.粒度分析样品分散条件的研究[J].建筑材料学报,2002,5(2)：198-201.
[227]F.J. Pettijohn, P.E.Potter, R.Siever. Sand and Sandstone.(second edication) Springer-Verlag [M]. New York:Berlin Heidelberg, London Paris Tokyo,1987:69-95.
[228]成都地质学院.沉积岩石学[M].北京：地质出版社,1980：307-313.
[229]任明达,王乃梁.现代沉积环境概论[M].北京：科学出版社,1981：8-25.
[230]华东石油学院岩矿教研室.沉积岩石学(上册)[M].北京：石油工业出版社,1982：79-96.
[231]华东石油学院勘探系、基础地质、石油地质教研室.沉积岩[M].北京：石油化学工业出版社,1977：66-93.
[232]刘东生.黄土与环境[M].北京：科学出版社,1985.
[233]Folk R. L., Ward W. C. Brazos river bar:a study in the significance of grain size relationship [J]. Journal of Sedimentary Petrology,1957,27:3-26.
[234]陈广庭,冯起等.塔里木盆地沙漠石油公路沿线风沙环境的形成与演变[M].北京：中国环境科学出版社,1997：158.
[235]Wang X. M., Dong Z. B., Zhang J. W., et al. Grain size characteristics of dune sands in the central Taklimakan Sand Sea [J]. Sedimentary Geology,2003,161:1-14.
[236]Vincent P.J. particle size variation over a transiverse dune in the Nafud as sirr, central saudi,Arabia [J].Arid Environments,1983,7:329-36.
[237]Folk R. L. Longitudinal dunes of the northwestern edge of the Simpson Desert, Northern Territory, Australia.1. Geomorphology and grain size relationships [J]. Sedimentology,1971,16: 5-54.
[238]Lancaster N. Grain size characteristics of linear dunes in the Southwestern Kalahali [J]. Sediment Petrol,1986,55:395-495.
[239]杨小平.巴丹吉林沙漠及其毗邻地区的景观类型及其形成机制初探[J].中国沙漠,2000,20(2)：166-170.
[240]Mischke S. New evidence for origin of Badain Jaran Desert of Inner Mongolia from granulometry and thermoluminescence dating [J]古地理学报,2005,7(1)：79-97.
[241]Howard, A. D., et al. Sand transport model of barchan dune equilibrium[J]. Sedimentology, 1978,25:307-28.
[242]Lai R. J., Wu J. Windd erosion and deposition along a coastal sand dune sea grant program[J]. University of Delevare,1978, (10-78):2699.
[243]Waston A. Grain-size Variation on a longitudimal dune and a barchan dune.Sediment [J].Geology,1986,46:49-66.
[244]钱广强,董治宝,罗万银,等.横向沙丘背风侧气流重附风洞模拟[J].中国沙漠,2008(1)：16-20.
[245]普罗霍罗娃,r.A.1950,水和风的搬运作用对卡拉库姆沙的矿物及沙粒形态的影响.陈治平等译.沙漠地貌的起源及其研究方法[C].北京：科学出版社,1962：114-155.
[246]Pettijohn F. J., Potter P. E., SieverR. Sand and Sandstone [M]. Beijing:Science Press,1977: 35-40.
[247]Joanne C., Lihou, Maria A., et al. Provenance of the Sardona Flysch, eastern Swiss Alps:examplee of high-resolution heavy mineral analysis applied to an ultrastable assemblage[J]. Sedimentary Geology,1996,105:141-157.
[248]Harald G. Dill. A review of heavy minerals in clastic sediments with case studies from the alluvial-fan through the nearshore-marine environments [J]. Earth-Science Reviews,1998,45: 103-132.
[249]邹松梅.江苏常州地区第四纪重矿物地层及其意义[J].江苏地质,2001,25(1)：6-10.
[250]杨群慧,林振宏,张富元.南海中东部表层沉积物矿物组合分区及其地质意义[J].海洋与湖沼,2002,33(6)：591-599.
[251]范德江,孙效功,杨作升.沉积物物源定量识别的非线性规划模型[J].沉积学报,2003,20(1)：30-34.
[252]Ruud T.E. Schuttenhelm, Cees Laban. Heavy minerals, provenance and large scale dynamics of seabed sands in the Southern North Sea:Baak's (1936) heavy mineral study revisited [J]. Quaternary International,2005,133:179-193.
[253]Morton A. C., Halls worth C. R. Identifying provenance specific features of detrital heavy mineral assemblages in sandstones[J]. Sedimentary Geology,1994,90(3):241-256.
[254]Morton A. C. Influences of provenance and diagenesis on detrital garnet suites in the Forties Sandstone, Paleocene Central North Sea [J]. Sediment. Petrology,1987,57:1027-1032.
[255]Morton, A. C., Hallsworth, C. R., et al. Processes controlling the composition of heavy mineral assemblages in sandstones [J]. Sedimentary Geology,1999,124(1-4):3-29.
[256]Morton A. C., Hurst, A., et al. Correlation of sandstones using heavy minerals:an example from the Statfjord Formation of the Snorre Field,northern North Sea. In:Dunay R E,Hailwood E A, eds. Nonbiostratigraphical Methods of Dating and Correlation[C]. London:Geological Society Special Publication,1995:89:3-22.
[257]和钟桦,刘招君,郭巍.柴达木盆地北缘大媒沟剖面重矿物分析及其地质意义[J].世界地质,2001,275-281.
[258]陆洁民,郭召杰,赵泽辉,等.新生代酒西盆地沉积特征及其与祁连山隆升关系的研究[J].高校地质学报,2004,10(1)：50-61.
[259]刘英俊,王鹤年,曹励明,等.元素地球化学[M].北京：科学出版社,1984.
[260]Bagnold,R A. The physics of blown sand and desert dunes [M]. London:Methuen,1954:1-8.
[261]吴正,刘恕.风沙地貌与治沙工程学[M].北京：科学出版社,2003：236-286.
[262]Yang X. B., Zhu B. Q., White P. D. Provenance of aeolian sediment in the Taklamakan Desert of western China, inferred from REE and major-elemental data[J]. Quaternary International, 2007,175(1):71-85.
[263]Taylor S. R., McLennan S. M. The Continental Crust:Its Composition and Evolution [M]. London:Blackwell,1985:277.
[264]Puchelt, H., Barium. In:Wedepohl,K H (Editor), Handbook of Geochemistry [M]. Berlin: Springer,1972:56B1-5602
[265]Whitfield, M., Turner, D. R. Water-rock partition coefficients and the composition of seawater and river water [J]. Nature,1979,300:433-435.
[266]Nesbitt H. W., Markovics G.., Price R. C. Chemical processes affecting alkalis and alkaline earths during continental weathering[J].Geochimicaet Cosmochimica Acts,1980,44:1659-1666.
[267]Dasch E. J. Strontium isotopes in weathering profiles, deep sea sediments and sedimentary rocks[J]. Geochim Cosmochim Acta,1969,33:1521-1552.
[268]Chen J., An Z. S., Head J. Variation of Rb/Sr ratios in the loess-paleosol sequences of central China during last 130 000 years and their implications for monsoon paleoclimatology[J]. Quaternary Research,1999,51:215-219.
[269]Chen J., Wang Y.J., Chen Y., et al. Geochemical characterization of Rb and Sr in the Chinese loess stratigraphy and its implications for paleomonsoon climate[J].Acta Geologica Sinica,2000, 4 (2):279-288.
[270]Wedepohl K H.Handbook of Geochemistry [M].Berlin:Springer,1969:248.
[271]Nesbitt, H. W., Young, G. M. Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations[J]. Geochimica et Cosmochimica Acta, 1984,48,1523-1534.
[272]Yong, G. M., Nesbitt, H. W. Paleoclimatology and provenance of the glaciogenic Gowganda Formation (Paleoproterozoic), Ontario, Canada:A chemostratigraphic approach[J]. GSA Bulletin, 1999,111:264-274.
[273]冯连君,储雪蕾,张启锐,等.化学蚀变指数(CIA)及其在新元古代碎屑岩中的应用[J].地学前缘,2003,10(4)：539-544.
[274]王自强,尹崇玉,高林志,等.黔南—桂北地区南华系化学地层特征[J].地球学报,2009,30(4)：465-474.
[275]McLennan, S. M., Hemming, S., McDaniel, D. K., et al. Geochemical approaches to sedimentation, provenance and tectonics. Johnsson, M.J., Basu, A. Processes Controlling the Composition of Clastic Sediment:Geological Society of America Special Paper[C],1993:284, 21-40.
[276]Nesbitt, H. W., Fedo, C. M., Young, G, M. Quartz and Feldspar Stability, Steady and Non-steady-State Weathering, and Petrogenesis of Siliciclastic Sands and Muds[J]. The journal of geology,1989,105:173-191.
[277]COX R. The influence of sediment recycling and basement composition on evolution of mudrock chemistry in the southwestern United States [J]. Geochimica et Cosmochimica Acta, 1995,59:2919-2940.
[278]Cullers R. L., Podkovyrov V. M. Geochemistry of the Mesoproterozoic Lakhanda shales in southeatern Yakutia, Russia:Implications for mineralogical and provenance control,and recycling[J]. Precambrian Research,2000,104:77-93.
[279]Cullers R. L. The source and origin of terrigenous sedimentary rocks in the Mesoproterozoic Ui group, southeastern Russia [J]. Precambrian Research,2002,117:157-183.
[280]Young G. M., Nesbitt H. W. Paleoclimatology and provenance of the glaciogenic Gowganda Formation (Paleoproterozoic), Ontario, Canada:A chemostratigraphic approach[J]. GSA Bulletin, 1999,111:264-274.
[281]李徐生,韩志勇,杨守业等.镇江下蜀土剖面的化学风化强度与元素迁移特征[J].地理学报,2007,62(11)：1174-1184.
[282]Fedo, C. M., Nesbitt, H. W., Young, G. M. Unraveling the effects of potassium metasomatism in sedimentary rocks and paleosols, with implications for paleoweathering conditions and provenance[J]. Geology,1995,.23,921-924.
[283]Matsuhisa, Y., Mizota, C., Faure, K., et al. Homogenization processes of fine particles in the arid regions of western China, inferred from oxygen isotope composition of quartz[J]. The Todai International Symposium on Cosmochronlogy and Isotope Geoscience Abstracts,1996,29-32.
[2]王涛,吴薇,赵哈林等.沙漠化过程中生物量损失的初步评估—以内蒙古科尔沁地区为例[J].中国沙漠,2005,25(4)：453-456.
[3]董治宝.中国风沙物理研究五十年(1)[J].中国沙漠,2005,25(3)：293-305.
[4]吴正.风沙地貌学[M].北京：科学出版社,1987：98-153.
[5]Livingstone I, Warren A. Aeolian Geomorphology[M].Landon:Addison Wesley Longman Limited,1996,64-101.
[6]杨景春,李有利.地貌学原理[M].北京：北京大学出版社,2007.
[7]Stein M A. Explorations in Central Asia,1906-8[J]. Geographical Journal,1909,58:241-271.
[8]Thomas B. A journey into Rub'al Khali the Southern Arabian Desert[J]. Geographical Journal, 1931,80:1-37.
[9]Beadnell H J L. The sand dunes of the Libyan Desert[J]. Geographical Journal,1910,35: 379-395.
[10]Hogbom I. Ancient inland dunes of northern and middle Europe[J]. Geographical Annal,1923, 5:113-243.
[11]Udden J A. Mechanical composition of some clastic sediments[J]. Geological Society of America, Bulletin,1914,25:655-744.
[12]Cornish V. Limits of form and magnitude of desert dunes[J]. Nature,1928,121:620-622.
[13]费道罗维奇B A.等著.陈治平等译.沙漠地貌的起源及其研究方法(译文集)[M].北京：科学出版社,1962.
[14]Bagnold R A. The Physics of Blown Sand and Desert Dunes[M]. London:Methuen,1941: 25-28,38-41.
[15]兹纳门斯基A N著.杨郁华译,朱震达校.沙地风蚀过程的实验研究和沙堆防止问题[M].北京：科学出版社,1960.
[16]Mckee E D. Structures of dunes at White Sands National Monument, New Mexico[J]. Sedimentology,1966,7:3-69.
[17]Mckee E D编著.赵兴梁译.世界沙海的研究[M].银川：宁夏人民出版社,1993.
[18]Greeley R. Iversen J D. Wind as a Geological Process[M]. Cambridge:Cambridge University Press,1985.
[19]Folk R.L. Longitudinal dunes of the Northwestern edge of the Simpson Desert, Northern Territory, Australia.1. Geomorphology and grain size relationships[J]. Sedimentology,1971,16: 5-54.
[20]Glennie K. W. Desert Sedimentary Environments[M]. Amsterdam:Elsevier,1970.
[21]White B R. Laboratory simulation of aeolian sand transport and physical modeling of flow around dunes[J]. Annals of Arid Zone,1996,35(3):187-214.
[22]Lancaster N. The role of field experiments in studies of dune dynamics and morphology [J]. Annals of Arid Zone,1996,35:171-186.
[23]Livingtone I, Warren A. Aeolian Geomorphology:An Introduction[M]. London:Longman,1996.
[24]Lancaster N. Geomorphology of Desert Dunes [M]. London:Routledge,1995.
[25]Cook R U, Warren A, Goudie A S. Desert Geomorphology [M]. London:UCL Press,1993.
[26]Lancaster N. Control of eolian dune size and spacing [J]. Geology,1988,16:972-975.
[27]Lancaster N. The Namib Sand Sea:Dune Forms, Processes, and Sediments [M]. Balkema: Rotterdam,1989.
[28]Lancaster N. Relations between dune generations in the Gran Desierto of Mexico [J]. Sedimentology,1992,39:631-644.
[29]Lancaster N. Origin of the Gran Desierto Sand Sea:Sonora, Mexico:evidence from dune morphology and sediments In Desert Aeolian Processes, Tchakerian VP (ed.) [M]. New York: Chapman and Hall,1995:11-36.
[30]Liu CQ, Masuda A, Okada A, et al. A geochemical study of loess and desert sand in northern China:implications for continental crust weathering and composition [J]. Chemical Geology, 1993,106:350-374.
[31]Honda M, Shimizu H. Geochemical, mineralogical and sedimentological studies on the Taklimakan Desert sands [J]. Sedimentology,1998,45:1125-1143.
[32]Livingstone I, Bullard JE, Wiggs GFS, et al. Grain-size variation on dunes in the Southwest Kalahari, Southern Africa[J]. Journal of Sedimentary Research,1999,69:546-552.
[33]Kasper-Zubillaga JJ, Dickinson WW. Discriminating depositional environments of sands from modern source terranes using modal analysis [J]. Sedimentary Geology,2001,143:149-167.
[34]Honda M, Yabuki S, Shimizu H. Geochemical and isotopic studies of aeolian sediments in China [J]. Sedimentology,2004,51:211-230.
[35]Muhs DR. Mineralogical maturity in dune fields of North America, Africa and Australia [J]. Geomorphology,2004,59:247-269.
[36]Wang X., Dong Z., Zhang J., et al. Grain size characteristics of dune sands in the central Taklimakan Sand Sea [J]. Sedimentary Geology,2003,161:1-14.
[37]Sweet M. L., Nielson J., Havholm K., et al. Algodones dune field of southern California:case history of a migrating modern dune field [J]. Sedimentology,1988,35:939-952.
[38]Ahlbrandt T. Textural parameters of eolian deposits. In:McKee E. D. (ed.), A study of global sand seas [J]. USGS Professional Paper,1979,1052:21-51.
[39]Lancaster, N. Grain size characteristics of Namib Desert linear dunes [J]. Sedimentology,1981, 28:115-122.
[40]Watson, A. Grain-size variations on a longitudinal dune and a barchan dune [J]. Sedimentary Geology,1986,46,49-66.
[41]Livingstone, I. Grain-size variation on a 'complex' linear dune in the Namib Desert. In:Frostick, L., Reid, I. (Eds.), Desert Sediments, Ancient and Modern. Geological Society Special Publication [C]. Blackwell:Oxford,1987,35:281-291.
[42]Livingstone, I. Temporal trends in grain-size measures on a linear sand dune [J]. Sedimentology, 1989,36:1017-1022.
[43]Rubin, D.M., Hunter, R.E. Why deposits of longitudinal dunes are rarely recognized in the geological record [J]. Sedimentology,1985,32:147-157.
[44]Bristow, C.S., Bailey, S.D., Lancaster, N. The sedimentary structure of linear sand dunes [J]. Nature,2000.406:56-59.
[45]Bagnold, R.A. The size-grading of sand by wind. Proceeding of the Royal Society of London [C]. London:The Royal Society,1937,250-264.
[46]Bagnold, R.A., Barndorff-Nielsen, O.E. The pattern of natural size distributions [J]. Sedimentology,1980,27:199-207.
[47]Tsoar, H. Two-dimensional analysis of dune profiles and the effect of grain size on sand dune morphology. In:El-Baz, F., Hassan, M.H.A. (Eds.), Physics of Desertification[C]. Martinus Nijhof:The Hague,1986,94-108.
[48]Pye, K., Tsoar, H. Aeolian Sand and Sand Dunes [M]. London:Unwin Hyman,1990.
[49]Thomas, D.S.G. Analysis of linear dune sediment-form relationships in the Kalahari Dune Desert [J]. Earth Surface Processes and Landforms,1988,13:545-553.
[50]Wasson, R.J. Dune sediment types, sand color, sediment provenance and hydrology in the Strzelecki-Simpson dunefield, Australia. In:Brookfield, M.E., Ahlbrandt, T.S. (Eds.), Eolian Sediments and Processes[C]. Elsevier:Amsterdam,1983,165-195.
[51]Waitt, M.B.C. Desert dunes of the Kermit Sandhills, Winkler County, Texas [D]. Texas:The University of Texas, USA,1969.
[52]Sneh, A., Weissbrod, T. Size-frequency distribution on longitudinal dune ripple flank sands compared to that of slip face sands of various dune types[J]. Sedimentology,1983,30:717-726.
[53]Goudie, A., Warren, A., Jones, D., et al. The character and possible origins of the aeolian sediments of the Wahiba sand sea, Oman [J]. Geography,1987,153 (2),231-256.
[54]Hastenrath, S.L. The barchans of the Arequipa region, southern Peru[J]. Geomorphology,1967, 11:300-331.
[55]朱震达,吴正,刘恕,等.中国沙漠概论[M].北京：科学出版社,1980：40-45.
[56]朱震达、陈治平、吴正,等.塔克拉玛干沙漠风沙地貌研究[M].北京：科学出版社,1981：44-47,107-108.
[57]李志忠,关有志,孙忠.塔里木沙漠石油公路沿线新月形沙丘的地貌特征[J].新疆大学学报(自然科学版),1998,(1)：80-90.
[58]李志忠.新月形沙丘研究进展综述[J].干旱区地理,1994,17(4)：81-87.
[59]闫满存,王光谦,李保生,等.巴丹吉林沙漠高大沙山的形成发育研究[J].地理学报,2001,56(1)：83-91.
[60]屈建军,常学礼,董光荣,等.巴丹吉林沙漠高大沙山典型区风沙地貌的分形特性[J].中国沙漠,2003,23(4)：361-365.
[61]杨萍,邹学勇,哈斯,等.巴丹吉林沙漠北部风沙地貌形态类型的分区研究[J].中国沙漠,1999,19(3)：210-213.
[62]张伟民,王涛.巴丹吉林沙漠高大沙山形成演化初步探讨[J].中国沙漠,2005,25(2)：281-286.
[63]张伟民,李孝泽,屈建军,等.金字塔沙丘地表气流场及其动力学过程研究[J].中国沙漠,1998,18(3)：215-220.
[64]下训明,董治宝,屈建军.塔克拉玛干沙漠简单横向沙丘形态学示量特征[J].兰州大学学报(自然科学版),2002,38(6)：110-116.
[65]李恒鹏,陈广庭,薛东前.塔克拉玛干沙漠腹地复合沙垄的流场和和上覆沙丘组合及动态特征[J].干旱区地理,2001,24(1)：80-85.
[66]李恒鹏,陈广庭.塔克拉玛干沙漠腹地复合沙垄间地新月形沙丘的逆向演变[J].中国沙 漠,1999,19(2)：134-138.
[67]李生宇,雷加强,徐新文,等.草方格固沙带对垄间新月形沙丘形态和移动的影响[J].干旱区地理理,2006,29(5)：632-638.
[68]凌裕泉,吴正,刘绍中,等.新月形沙丘形态的模拟实验研究[J].地理学报,1998,18(1)：88-93.
[69]李志忠,武胜利,李万娟,等.最近10年来新疆风沙地貌研究进展[J].干旱区研究,2008,25(2)：295-303.
[70]董治宝,屈建军,卢琦,等.关于库姆塔格沙漠“羽毛状”风沙地貌的讨论[J].中国沙漠,2008,28(6)：1005-1091.
[71]屈建军,郑本兴,俞祁浩,等.罗布泊东阿奇克谷地雅丹地貌与库姆塔格沙漠形成的关系[J].中国沙漠,2004,24(3)：294-302.
[72]屈建军,左国朝,张克存,等.库姆塔格沙漠形成演化与区域新构造运动关系研究[J].干旱区地理,2005,28(4)：424-428.
[73]刘虎俊,赵明,王继和,等.库姆塔格沙漠南部的风积地貌特征[J].干旱区资源与环境,2005,19(7)：130-134.
[74]刘虎俊,王继和,廖空太,等.库姆塔格沙漠“羽毛状沙丘”形态的示量特征[J].干旱区地理理,2006,29(3)：314-320.
[75]哈斯,董光荣,王贵勇.腾格里沙漠东南缘格状沙丘的形态动力学研究[J].中国科学(D),1999,29(5)：466-471.
[76]贺大良.风沙地貌形成机制的几个问题[J].中国沙漠,1985,5(1)：33-37.
[77]赵景峰,李崇顺,周兴佳,等.新月形沙丘丘表流场与沙丘蚀积特征[J].中国沙漠,1993,13(3)：18-27.
[78]李志忠,陈广庭.金字塔沙丘风洞流场结构的实验研究[J].中国沙漠,1995,15(3)：227-232.
[79]凌裕泉,刘绍中,吴正,等.金字塔沙丘形成的动力条件分析[J].中国沙漠,1997,17(2)：112-118.
[80]张春来,董光荣,董治宝,等.用风洞实验方法计算土壤风蚀量的时距问题[J].中国沙漠,1996,16(2)：200-203.
[81]刘连友.区域风沙蚀积量和蚀积强度初步研究：以晋陕蒙接壤区为例[J].地理学报,1999,54(1)：60-68.
[82]中国科学院兰州沙漠研究所额济纳旗考察队.乌兰布和沙漠西南铁路沿线沙害防治[J].中国沙漠,1983,3(2)：30-35.
[83]李银芳,周兴佳,潘伯荣,等.兰新铁路哈密地区的沙害[J].中国沙漠,1986,6(4)：56-62.
[84]董治宝,陈广庭,韩致文,等.塔里木沙漠石油公路风沙危害[J].环境科学,1997,18(1)：4-9.
[85]刘铁良,陈昌秀.不易沙埋的铁路路基断面形式问题[J].中国沙漠,1984,4(1)：31-37.
[86]刘贤万,崔志刚.特大风区防翻车挡风墙工程设计的风洞实验研究[J].中国沙漠,1994,14(3)：38-46.
[87]刘贤万,凌裕泉,贺大良,等.下导风工程的风洞实验研究：(1)平面上的实验[J].中国沙漠,1982,2(4)：14-21.
[88]刘贤万,凌裕泉,贺大良,等.下导风工程的风洞实验研究：(2)地形条件下的实验.中国沙漠,1982,3(3)：25-34.
[89]刘贤万.草方格沙障的风洞实验.流沙治理研究(二)[M].银川：宁夏人民出版社，1991：326-334.
[90]徐峻龄,裴章勤,王仁化.半隐蔽式麦草方格沙障防护带宽度的探讨[J].中国沙漠,1982,2(3)：16-23.
[91]卫林.论林带的有效防护距离[J].科学通报,1985,19：1567-1569.
[92]Zhang Weimin, Qu Jianjun, Dong Zhibao, et al. The airflow field and dynamic processes of pyramid dunes [J]. Journal of arid Environments,2000,45:357-368.
[93]Wang Tao, Zhang Weimin, Dong Zhibao, et al. The dynamic characteristics and migration of a pyramid dune [J]. Sedimentology,2005,52:429-440.
[94]Liu Xianwan, Lisen, Shen Jianyou. Wind tunnel simulation experiment of mountain dunes [J]. Journal of Arid Environments,1999,42:49-59.
[95]李振山,倪晋仁.风成沙纹发育过程中形态变化的风洞实验研究[J].应用基础与工程科学学报,2003,11(3)：247-254.
[96]马玉明,姚洪林.光电子集沙仪对毛乌素沙地沙丘蚀积过程的观测[J].中国沙漠,2001,21(增刊)：68-71.
[97]武生智,马崇武,苗天德.沙粒级配和沙丘分布的分形研究[J].中国沙漠,1999,19(3)：247-250.
[98]王建成,武生智,马崇武.沙丘背风坡的净力学稳定性分析[J].中国沙漠,2001,21(增刊):84-86.
[99]王训明,董治宝,屈建军.塔克拉玛干沙漠简单线形沙丘形态-动力学过程研究[J].中国沙漠,2003,23(3)：257-262.
[100]哈斯,庄燕美,王蕾,等.毛乌素沙地南缘横向沙丘粒度分布及其对风向变化的响应[J].地理科学进展,2006,25(6)：42-51.
[101]哈斯.腾格里沙漠东南缘格状沙丘粒度特征与成因探讨[J].地理研究,1998,17(2)：178-184.
[102]哈斯,王贵勇.沙坡头地区新月形沙丘粒度特征[J].中国沙漠,2001,21(3)：271-275.
[103]哈斯,王贵勇.腾格里沙漠东南缘横向沙丘粒度变化及其与坡面形态的关系[J].中国沙漠,1996,16(2)：216-221.
[104]钱亦兵,张希明,李晓明.塔克拉玛干沙漠南缘绿洲沙物质粒度特征[J].中国沙漠,1995,]5(2)：131-135.
[105]钱亦兵,周兴佳,吴兆宁.准噶尔盆地沙物质粒度特征研究[J].干旱区研究,2000,17(2)：34-41.
[106]钱亦兵,周兴佳,李崇舜,等.准噶尔盆地沙漠沙矿物组成的多源性[J].中国沙漠,2001,21(2)：182-187.
[107]钱亦兵,吴兆宁,杨海峰,等.古尔班通古特沙漠南部风沙土粒度分布的空间异质性[J].干旱区地理,2009,32(5)：655-661.
[108]陈渭南.塔克拉玛干沙漠84°E沿线沙物质的粒度特征[J].地理学报,1993,48(1)：33-46.
[109]陈渭南,雷加强.塔克拉玛干沙漠新月形沙丘不同部位的粒度特征[J].干旱区资源与环境,1992,6(2)：101-110.
[110]李振山,陈广庭,冯起,等.塔克拉玛干沙漠腹地纵向沙垄表面沙物质粒度特征[J].干旱区资源与环境,1998,12(1)：21-28.
[111]赵元杰,周兴佳.塔里木沙漠公路沿线沙物质特征及环境意义[J].干旱区研究,1999,16(3)：53-58.
[112]赵元杰,夏训诚,王富葆,等.罗布泊地区红柳沙包纹层沙粒度特征与环境指示意义[J].干旱区地理,2007,30(6)：791-796.
[113]温小浩,李宝生,李森,等.2.5kaBP以来额济纳绿洲沙丘的粒度特征及其反映的沉积过程[J].地质学报,79(5)：710-718.
[114]吉启慧.克里雅河流域沉积物的粒度特征[J].干旱取研究,1992,9(3)：48-56.
[115]吉启慧.粒度分析在塔克拉玛干沙漠中的应用[J].中国沙漠,1996,16(2)：173-179.
[116]韩广,张桂芳,杨文斌.呼伦贝尔沙地沙丘沙来源的定量分析[J].地理学报,2004,59(2)：189-186.
[117]王训明,董治宝,屈建军,等.塔克拉玛干沙漠简单线形沙丘形态动力学过程研究[J].中国沙漠,2003,23(3)：257-262.
[118]王训明,陈广庭.塔里木沙漠石油公路半隐蔽式沙障区与流沙区沙物质粒度变化[J].中国沙漠,1996,16：(2)：180-184.
[119]黄杏珍,潘中海.应用粒度资料探讨毛乌素沙漠西南部的风沙特征[J].地理学报,1981,36(1)：70-78.
[120]季方,叶玮,魏文寿.古尔班通古特沙漠固定与半固定沙丘成因初探[J].干旱区地理理,2000,23(1)：32-36.
[121]张瑞军,何清,孔丹,等.塔克拉玛干沙漠北缘沙尘暴源区地表沉积物粒度特征[J].干旱区研究,2008,25(6)：887-883.
[122]魏怀东,徐先英,王继和,等.库姆塔格沙漠沙丘的粒度特征[J].水土保持学报,2007,21(3)：6-9.
[123]魏怀东,王继和,徐先英,等.库姆塔格沙漠各沙丘类型沙粒粒度分析[J].甘肃科技,2007,23(5)：85-88.
[124]何清,杨兴华,霍文,等.库姆塔格沙漠粒度分布特征及环境意义[J].中国沙漠,2009,29(1)：18-22.
[125]唐进年,王继和,苏志珠,等.库姆塔格沙漠羽毛状沙丘表面沙粒度分布特征[J].干旱区地理,2008,31(6)：918-925.
[126]张宇红,李保生,靳鹤龄,等.萨拉乌苏河流域150 ka BP以来的粒度旋回[J].地理学报,2001,56(3)：332-344.
[127]魏文寿.沙漠表层粒度与水热变化的环境效应分析—以古尔班通古特沙漠为例[J].沉积学报,1998,16(1)：152-157.
[128]冯起,陈广庭,朱震达.塔克拉玛干沙漠北部全新世环境演变(Ⅰ)[J].环境科学学报,1996,16(2)：238-244.
[129]李志忠.塔里木石油公路沿线风成沙特征及其区域分异[J].新疆师范大学学报(自然科学版),1996,15(4)：52-62.
[130]李志忠,关有志,孙忠贾,等.塔克拉玛干沙漠腹地纵向沙垄的粒度分布特征[J].干旱区研究,1996,13(2)：37-43.
[131]张虎才.撒哈拉沙漠东北部苏丹境内东西断面粒度分布特征及其成因与环境[J].中国沙漠,1996,16(3)：242-246.
[132]贾铁飞,何雨,裴东.鸟兰布和沙漠北部沉积物特征及环境意义[J].干旱区地理,1998,21(2)：36-42.
[133]Weltje G J, von Eynatten H. Quantitative provenance analysis of sediments:review and outlook[J]. Sedimentary Geology,2004,171(1-4):1-11.
[134]Garzanti E, Vezzoli G, Ando S et al. Quantifying sand provenance and erosion (Marsyandi River, Nepal Himalaya) [J].Earth and Planetary Science Letters,2007,258(3-4):500-515.
[135]Nesbitt H, Young G. Petrogenesis of sediments in the absence of chemical weathering:Effects of abrasion and sorting on bulk composition and mineralogy[J]. Sedimentology,1996,43(2): 341-358.
[136]Nesbitt H, Markovics G. Weathering of granodioritic crust, long-term storage of elements in weathering profiles, and petrogenesis of siliciclastic sediments[J]. Geochimica et Cosmochimica Acta,1997,61(8):1653-1670.
[137]Muhs D. Mineralogical maturity in dunefields of North America, Africa and Australia[J]. Geomorphology,2004,59(1-4):247-269.]
[138]Nesbitt H W, Young G M. Early Proterozoic climates and plate motions inferred from major element chemistry of lutites [J]. Nature,1982,299(21):715-717.
[139]Ding Z L, Sun J M, Yang S L et al. Geochemistry of the Pliocene red clay formation in the Chinese Loess Plateau and implications for its origin, source provenance and paleoclimate change[J]. Geochimica et Cosmochimica Acta,2001,65(6):901-913.
[140]Chen J, An Z. S., Liu L. W., et al. Variations in chemical compositions of the eolian dust in Chinese Loess Plateau over the past 2.5Ma and chemical weathering in the Asian inland[J]. Science in China:Series D,2001,31(2):136-145.
[141]Ujvari G., Varga A., Balogh-Brunstad Z. Origin weathering, and geochemical composition of loess in southwestern Hungary [J]. Quaternary Research,2008,69(3):421-437.
[142]宋锦熙.北京地区沙物质的重矿物成分、结构特征与风沙的沙物质来源[J].中国沙漠,1987,17(1)：24-33.
[143]钱亦兵.新疆伊犁塔克尔穆库尔沙漠沙的特征与沙源的关系[J].中国沙漠,]985,5(2)：36-43.
[144]钱亦兵,石井武政,水野清秀.塔克拉玛干沙漠和田河流域沙漠沙物质来源初探[J].干旱区研究,1991,(4)：48-51.
[145]钱亦兵,吴兆宁,石井武政,等.塔克拉玛干沙漠沙物质成分特征及其来源[J].中国沙漠,1993,13(4)：32-38.
[146]钱亦兵,吴兆宁,金井丰,等.塔克拉玛干沙漠沙物质成分研究[J].干旱区研究,1994,11(4)：46-52.
[147]谢静,丁仲礼.中国东北部沙地重矿物组成及沙源分析[J].中国科学D辑：地球科学,2007,37(8)：1065-1072.
[148]Yang, X. P., Zhang, F., Fu, X. D., et al. Oxygen isotopic compositions of quartz in the sand seas and sandy lands of northern China and their implications for understanding the provenances of aeolian sands [J]. Geomorphology,2008,102:278-285
[149]刘宝珺.沉积岩石学[M].北京：地质出版社,1980：126.
[150]邵磊.陆源碎屑岩地球化学在盆地分析中的应用[J].地学前缘,2000,7(3)：297-304.
[151]张小曳,张光宇,朱光华,等.中国源区粉尘的元素示踪[J].中国科学(D辑),1996,26(5)：423-430.
[152]孙业乐,庄国顺,袁蕙,等.2002年北京特大沙尘暴的理化特性及其组分来源分析[J].科学通报,2004,49(4)：340-346.
[153]孙继敏.中国黄十的物质来源及其粉尘的产生机制与搬运过程[J].第四纪研究,2004,24(2)：175-183.
[154]谢远云,何葵,周嘉,等.哈尔滨沙尘暴的化学特征及其物质源探讨[J].地理研究,2006,25(2)：255-261.
[155]陈骏,季峻峰,仇纲,等.陕西洛川黄十化学风化程度的地球化学研究[J].中国科学(D辑)，1997，27(6)：531-536
[156]陈骏,安芷生,刘连文,等.最近2.5 Ma以来黄土高原风尘化学组成的变化与亚洲内陆的化学风化[J].中国科学(D辑),2001,31(2)：136-144
[157]Ohta T, Arai H. Statistical empirical index of chemical weathering in igneous rocks:A new tool for evaluating the degree of weathering [J]. Chemical Geology,2007,240(3-4):280-297.
[158]Chen J, Ji J F, Chou G et al. Geochemistry of the chemical weathering intensity of the loess profile in Luochuan,Shaanxi Province[J]. Science in China:Series D,1997,27(6):531-536.
[159]徐志伟,鹿化煜,赵存法,等.库姆塔格沙漠地表物质组成、来源和风化过程[J].地理学报,2010,65(1)：53-64.
[160]Mckee E D. A Study of Global Sand Seas [M]. Washington:U. S. Government Printing Office, 1979:12-67.
[161]王涛.巴丹吉林沙漠形成演变的若干问题[J].中国沙漠,1990,10(1)：29-40.
[162]董光荣,高全洲,邹学勇,等.晚更新世以来巴丹吉林沙漠南缘气候变化[J].科学通报,1995,40：1214-1218.
[163]Jakel D. The Badain Jaran Desert:its o rigin and development [J]. Geow issenschaf en, 1996(78):272-274.
[164]Petroy M P. Theordos, alanshan and peishan, the deserts of Central Asia [J]. Research Service, 1966(1):241-260.
[165]Dong Zhibao, Wang Tao,Wang Xunming. Geomorphology of the megadunes in the Badain Jaran Desert [J]. Geomorphology,2003,60:1-13.
[166]陆锦华,Jakel D巴丹吉林沙漠及其毗邻地区地貌图(1：50万)[M].兰州：兰州大学出版社,1998.
[167]杨小平.近3万年来巴丹吉林沙漠的景观发育与雨量变化[J].科学通报,2000,45(4)：428-434.
[168]朱震达.中国沙漠、沙漠化、荒漠化及其治理的对策[M].北京：中国环境出版社,1999：137-142.
[169]楼桐茂.甘肃民勤至巴丹吉林庙间沙漠成因及其改造利用.治沙研究(第三号)[C].1962：90-95.
[170]孙培善,孙德钦.内蒙古高原西部水文地质初步研究.治沙研究(第六号)[C].北京：科学出版社,1964：245-317.
[171]谭见安.内蒙古阿拉善荒漠的类型.地理集刊(第八号)[C].北京：科学出版社,1964：1-31.
[172]Lancaster N. Palaeoclimatic evidence from sand seas [J]. Paleoclimatology,1990,76: 279-290.
[173]Hofmann J. Lakes in the SE part of Badain Jaran Shamo, their limnology and geochemistry[J]. Geowissenschaften,1996,14(7-8):275-278.
[174]Geyh M A,Gu Weizu,Jakel D. Groundwater recharge study in the Gobi Desert, China [J].Geowissenschaflen,1996,7(8):279-280.
[175]Yang X. P., Williams M. A. J. The ion chemistry of lakes and Late Holocene desiccation in the Badain Jaran Desert, lnner Mongolia, China [J]. Catena,2003,51(1):45-60.
[176]Yang Xiaoping. Geomorphologische Untersuchungen in Trockenreamen NW-China unter besonderer Berocksichtigung von Badanjilin and Takelamagan [J]. Gettinger Oeographische Abhandlungen,1991,96:1-124.
[177]Yang X. P., Liu T. S.,Xiao H.L., Evolution of megadunes and lakes in the Badain Jaran Desert, Inner Mongolia, China during the last 31000 years[J].Quatermary International,2003,104: 99-112.
[178]陈建生,赵霞,汪集旸,等.巴丹吉林沙漠湖泊钙华与根状结核的发现对研究湖泊水补给的意义[J].中国岩溶，2004,23(4)：277-282.
[179]Chen J. S., Li L., Wang J. Y., et al. Groundwater maintains dune landscape [J]. Nature, 2004,432,459-460.
[180]杨小平,刘东生.距今30ka前后我国西北沙漠地区古环境[J].第四纪研究,2003,23(1)：25-30.
[181]张虎才,马玉贞,彭金兰,等.距今42-18ka腾格里沙漠古湖泊及古环境[J].科学通报,2002,47(24)：1847-1857.
[182]高全洲,董光荣,李保生,等.晚更新世以来巴丹吉林南缘地区沙漠演化[J].中国沙漠,1995,15(4)：345-352.
[183]Yang X. Late Quaternary evolution and paleoclimates, Western Alashan Plateau, Inner Mongolia, China [J]. Z. Geomorph. N. F.,2001,45:1-16.
[184]德日进.中国之大陆沉积[J].中国地质学会志(丁文江先生纪念册),1937,16：195-220.
[185]周廷儒.新生代古地理.《中国自然地理》编辑委员会.中国自然地理古地理(上册)[C].北京：科学出版社,1984：1-233.
[186]李吉均,方小敏.新生代晚期青藏高原强烈隆起及其对周边环境的影响[J].第四纪研究,2001,21(5)：381-391.
[187]张川波,何元良.辽宁北票附近中侏罗世晚期的沙漠沉积[J].沉积学报,1983,1(4)：48-58.
[188]郭正堂,彭淑贞,郝青振,等.晚第三纪中国西北干旱化的发展及其对北极冰盖形成演化和青藏高原隆升的关系[J].中国第四纪研究,1999,(6)：556-567.
[189]杨东,方小敏,董光荣,等.1.8Ma BP以来陇西断岘黄土剖面沉积特征及其反映的腾格里沙漠演化[J].中国沙漠,2006,26(1)：6-13.
[190]闫满存,董光荣,陶贞,等.滕格里沙漠东南缘晚第三纪古风成沙及其环境[J].中国沙漠,1992,12(3)：10-15.
[191]闫满存,董光荣,李保生,等.腾格里沙漠东南缘沙漠演化的初步研究[J].中国沙漠,1998,18(2)：111-117.
[192]强明瑞,李森,金明,等.60ka来腾格里沙漠东南缘风成沉积与沙漠演化[J].中国沙漠,2000,20(3)：256-259.
[193]董光荣,李森,等.中国沙漠形成演化的初步研究[J].中国沙漠,1991,11(4)：23-32.
[194]哈斯.腾格里沙漠东南缘沙丘形态示量特征及其影响因素[J].中国沙漠,1995,15(2)：136-142.
[195]张克存,屈建军,姐瑞平,等.腾格里沙漠东南缘风沙活动动力条件分析—以沙坡头地区为例[J].干旱区地理,2008,31(5)：643-649.
[196]哈斯.腾格里沙漠东南缘沙丘表面风沙流结构变异的初步研究[J].科学通报,2004,49(11)：1099-1104.
[197]哈斯,王贵勇,董光荣.腾格里沙漠东南缘沙丘迎风坡风速变化的初步研究[J].干旱区地理,1999,22(1)：41-46.
[198]张克存,俎瑞平,屈建军,等.腾格里沙漠东南缘输沙势与最大可能输沙量之比较[J].中国沙漠,2008,28(4)：605-610.
[199]哈斯.腾格里沙漠东南缘格状沙丘沉积构造的解析[J].地学前沿,2004,11(1)：277-278.
[20]吴泰然,何国琦.阿拉善地块北缘的蛇绿混杂岩带及其大地构造意义[J].现代地 质,1992.6(3)：286-295.
[201]王廷印,王士政,王金荣.阿拉善地区古生代岩石圈形成与演化[M].兰州：兰州大学出版社,1994.
[202]王廷印,张铭杰,王金荣,等.恩格尔乌苏冲断带特征及大地构造意义[J].地质科学,1998,33(4)：385-394.
[203]张虎才,马玉贞,李吉均.腾格里沙漠南缘全新世古气候变化初步研究[J].科学通报,1998,43(2)：1252-1256.
[204]裴浩,敖艳红,李云鹏等.内蒙古阿拉善地区气候区划研究[J].干旱区资源与环境,2000,14(3)：76-76.
[205]刘振敏,崔天秀,丰创等.腾格里沙漠地区钾芒硝的首次发现及地质意义[J].矿物岩石地球化学通报,1998,17(1)：62-65.
[206]郭绍礼.腾格里沙漠东部的湖盆与风沙地貌特征.中国科学院治沙队.治沙研究(第四号)[C].北京：科学出版社,1962：76-80.
[207]成都地质学院陕北队.沉积岩(物)粒度分析及其应用[M].北京：地质出版社,1978.
[208]Cornillault J. Particle size analyzer [J]. Applied Optics,1972,11:265-268.
[209]Weiss E. L., Frock H. N. Rapid analysis of particle-size distributions by laser light scattering[J]. Powder Technology,1976,14:287-293.
[210]Weiner B. B. Particle and spray sizing using laser diffraction [J]. Society Photo-Optical Instrumentation Engineers,1979,170:53-56.
[211]Mc Cave I.. N., Bryant R. S., Cook H. F., et al. Evaluation of a laser-diffraction-size analyzer for use with natural sediments [J]. Journal of Sedimentary Petrology,1986,56:561-564.
[212]Loizeau J L, Arbouille D, Santiago S,et al. Evaluation of a wide range laser diffraction grain size analyzer for use with sediments [J]. Sedimentology,1994,41:353～361.
[213]Konert M., Vandenderghe J. Comparison of laser grain size analysis with pipette and sieve analysis:a solution for the underestimation of the clay fraction [J]. Sedimentology,1997,44: 523-535.
[214]Singer J. K., Anderson J. B., Ledbetter M. T., et al. An assessment of analytical techniques for the size analysis of fineg-rained sediments [J]. Journal of Sedimentary Petrology,1988,58: 534-543.
[215]Prins M. A., Postma G.,Weltje G. Controls on the terrigenous sediment supply to the Arabian Sea during the late Quaternary:The Markran continental slope[J]. Marine Geology,2000,169: 351-371.
[216]Prins,A., Vandenberghe,J., Weltje,G. J. Palaeoclimate signals in loess size distributions[J]. Workshop HWK Delmenhorst From Particle Size to Sediment Dynamics,2004,123-125.
[217]鹿化煜,安芷生.前处理方法对黄土沉积物粒度测量影响的实验研究?[J].科学通报,1997,42(23)：2535-2538.
[218]程鹏,高抒,李徐生.激光粒度仪测试结果及其与沉降法、筛析法的比较[J].沉积学报,2001,19(3)：449-455.
[219]鹿化煜,苗晓东,孙有斌.前处理步骤与方法对风成红黏土粒度测量的影响[J].海洋地质与第四纪地质,2002,22(3)：129-135.
[220]庞奖励,黄春长,贾耀峰.不同方法测定黄土和和古土壤样品粒度的比较[J].陕西师范大学学报(自然科学版),2003,31(4)：87-92.
[221]王君波,朱立平.不同前处理对湖泊沉积物粒度测量结果的影响.湖泊科学,2005,17(1)：17-23.
[222]孙有斌,高抒,鹿化煜.前处理方法对北黄海沉积物粒度的影响.海洋与湖沼,2001,32(6)：665-671.
[223]徐树建,杜忠花.激光粒度仪测量风成堆积物粒度的实验研究[J].水土保持研究,2007,14(2)：209-212.
[224]雷国良,张虎才,张文翔,等Mastersize2000型激光粒度仪分析数据可靠性检验及意义—以洛川剖面S4层古土壤为例[J].沉积学报,2006,24(4)：531-539.
[225]王德杰,范代读,李从先.不同预处理对沉积物粒度分析结果的影响[J].同济大学学报,2003,31(3)：314-318.
[226]杨玉颖,张学文,赵红,等.粒度分析样品分散条件的研究[J].建筑材料学报,2002,5(2)：198-201.
[227]F.J. Pettijohn, P.E.Potter, R.Siever. Sand and Sandstone.(second edication) Springer-Verlag [M]. New York:Berlin Heidelberg, London Paris Tokyo,1987:69-95.
[228]成都地质学院.沉积岩石学[M].北京：地质出版社,1980：307-313.
[229]任明达,王乃梁.现代沉积环境概论[M].北京：科学出版社,1981：8-25.
[230]华东石油学院岩矿教研室.沉积岩石学(上册)[M].北京：石油工业出版社,1982：79-96.
[231]华东石油学院勘探系、基础地质、石油地质教研室.沉积岩[M].北京：石油化学工业出版社,1977：66-93.
[232]刘东生.黄土与环境[M].北京：科学出版社,1985.
[233]Folk R. L., Ward W. C. Brazos river bar:a study in the significance of grain size relationship [J]. Journal of Sedimentary Petrology,1957,27:3-26.
[234]陈广庭,冯起等.塔里木盆地沙漠石油公路沿线风沙环境的形成与演变[M].北京：中国环境科学出版社,1997：158.
[235]Wang X. M., Dong Z. B., Zhang J. W., et al. Grain size characteristics of dune sands in the central Taklimakan Sand Sea [J]. Sedimentary Geology,2003,161:1-14.
[236]Vincent P.J. particle size variation over a transiverse dune in the Nafud as sirr, central saudi,Arabia [J].Arid Environments,1983,7:329-36.
[237]Folk R. L. Longitudinal dunes of the northwestern edge of the Simpson Desert, Northern Territory, Australia.1. Geomorphology and grain size relationships [J]. Sedimentology,1971,16: 5-54.
[238]Lancaster N. Grain size characteristics of linear dunes in the Southwestern Kalahali [J]. Sediment Petrol,1986,55:395-495.
[239]杨小平.巴丹吉林沙漠及其毗邻地区的景观类型及其形成机制初探[J].中国沙漠,2000,20(2)：166-170.
[240]Mischke S. New evidence for origin of Badain Jaran Desert of Inner Mongolia from granulometry and thermoluminescence dating [J]古地理学报,2005,7(1)：79-97.
[241]Howard, A. D., et al. Sand transport model of barchan dune equilibrium[J]. Sedimentology, 1978,25:307-28.
[242]Lai R. J., Wu J. Windd erosion and deposition along a coastal sand dune sea grant program[J]. University of Delevare,1978, (10-78):2699.
[243]Waston A. Grain-size Variation on a longitudimal dune and a barchan dune.Sediment [J].Geology,1986,46:49-66.
[244]钱广强,董治宝,罗万银,等.横向沙丘背风侧气流重附风洞模拟[J].中国沙漠,2008(1)：16-20.
[245]普罗霍罗娃,r.A.1950,水和风的搬运作用对卡拉库姆沙的矿物及沙粒形态的影响.陈治平等译.沙漠地貌的起源及其研究方法[C].北京：科学出版社,1962：114-155.
[246]Pettijohn F. J., Potter P. E., SieverR. Sand and Sandstone [M]. Beijing:Science Press,1977: 35-40.
[247]Joanne C., Lihou, Maria A., et al. Provenance of the Sardona Flysch, eastern Swiss Alps:examplee of high-resolution heavy mineral analysis applied to an ultrastable assemblage[J]. Sedimentary Geology,1996,105:141-157.
[248]Harald G. Dill. A review of heavy minerals in clastic sediments with case studies from the alluvial-fan through the nearshore-marine environments [J]. Earth-Science Reviews,1998,45: 103-132.
[249]邹松梅.江苏常州地区第四纪重矿物地层及其意义[J].江苏地质,2001,25(1)：6-10.
[250]杨群慧,林振宏,张富元.南海中东部表层沉积物矿物组合分区及其地质意义[J].海洋与湖沼,2002,33(6)：591-599.
[251]范德江,孙效功,杨作升.沉积物物源定量识别的非线性规划模型[J].沉积学报,2003,20(1)：30-34.
[252]Ruud T.E. Schuttenhelm, Cees Laban. Heavy minerals, provenance and large scale dynamics of seabed sands in the Southern North Sea:Baak's (1936) heavy mineral study revisited [J]. Quaternary International,2005,133:179-193.
[253]Morton A. C., Halls worth C. R. Identifying provenance specific features of detrital heavy mineral assemblages in sandstones[J]. Sedimentary Geology,1994,90(3):241-256.
[254]Morton A. C. Influences of provenance and diagenesis on detrital garnet suites in the Forties Sandstone, Paleocene Central North Sea [J]. Sediment. Petrology,1987,57:1027-1032.
[255]Morton, A. C., Hallsworth, C. R., et al. Processes controlling the composition of heavy mineral assemblages in sandstones [J]. Sedimentary Geology,1999,124(1-4):3-29.
[256]Morton A. C., Hurst, A., et al. Correlation of sandstones using heavy minerals:an example from the Statfjord Formation of the Snorre Field,northern North Sea. In:Dunay R E,Hailwood E A, eds. Nonbiostratigraphical Methods of Dating and Correlation[C]. London:Geological Society Special Publication,1995:89:3-22.
[257]和钟桦,刘招君,郭巍.柴达木盆地北缘大媒沟剖面重矿物分析及其地质意义[J].世界地质,2001,275-281.
[258]陆洁民,郭召杰,赵泽辉,等.新生代酒西盆地沉积特征及其与祁连山隆升关系的研究[J].高校地质学报,2004,10(1)：50-61.
[259]刘英俊,王鹤年,曹励明,等.元素地球化学[M].北京：科学出版社,1984.
[260]Bagnold,R A. The physics of blown sand and desert dunes [M]. London:Methuen,1954:1-8.
[261]吴正,刘恕.风沙地貌与治沙工程学[M].北京：科学出版社,2003：236-286.
[262]Yang X. B., Zhu B. Q., White P. D. Provenance of aeolian sediment in the Taklamakan Desert of western China, inferred from REE and major-elemental data[J]. Quaternary International, 2007,175(1):71-85.
[263]Taylor S. R., McLennan S. M. The Continental Crust:Its Composition and Evolution [M]. London:Blackwell,1985:277.
[264]Puchelt, H., Barium. In:Wedepohl,K H (Editor), Handbook of Geochemistry [M]. Berlin: Springer,1972:56B1-5602
[265]Whitfield, M., Turner, D. R. Water-rock partition coefficients and the composition of seawater and river water [J]. Nature,1979,300:433-435.
[266]Nesbitt H. W., Markovics G.., Price R. C. Chemical processes affecting alkalis and alkaline earths during continental weathering[J].Geochimicaet Cosmochimica Acts,1980,44:1659-1666.
[267]Dasch E. J. Strontium isotopes in weathering profiles, deep sea sediments and sedimentary rocks[J]. Geochim Cosmochim Acta,1969,33:1521-1552.
[268]Chen J., An Z. S., Head J. Variation of Rb/Sr ratios in the loess-paleosol sequences of central China during last 130 000 years and their implications for monsoon paleoclimatology[J]. Quaternary Research,1999,51:215-219.
[269]Chen J., Wang Y.J., Chen Y., et al. Geochemical characterization of Rb and Sr in the Chinese loess stratigraphy and its implications for paleomonsoon climate[J].Acta Geologica Sinica,2000, 4 (2):279-288.
[270]Wedepohl K H.Handbook of Geochemistry [M].Berlin:Springer,1969:248.
[271]Nesbitt, H. W., Young, G. M. Prediction of some weathering trends of plutonic and volcanic rocks based on thermodynamic and kinetic considerations[J]. Geochimica et Cosmochimica Acta, 1984,48,1523-1534.
[272]Yong, G. M., Nesbitt, H. W. Paleoclimatology and provenance of the glaciogenic Gowganda Formation (Paleoproterozoic), Ontario, Canada:A chemostratigraphic approach[J]. GSA Bulletin, 1999,111:264-274.
[273]冯连君,储雪蕾,张启锐,等.化学蚀变指数(CIA)及其在新元古代碎屑岩中的应用[J].地学前缘,2003,10(4)：539-544.
[274]王自强,尹崇玉,高林志,等.黔南—桂北地区南华系化学地层特征[J].地球学报,2009,30(4)：465-474.
[275]McLennan, S. M., Hemming, S., McDaniel, D. K., et al. Geochemical approaches to sedimentation, provenance and tectonics. Johnsson, M.J., Basu, A. Processes Controlling the Composition of Clastic Sediment:Geological Society of America Special Paper[C],1993:284, 21-40.
[276]Nesbitt, H. W., Fedo, C. M., Young, G, M. Quartz and Feldspar Stability, Steady and Non-steady-State Weathering, and Petrogenesis of Siliciclastic Sands and Muds[J]. The journal of geology,1989,105:173-191.
[277]COX R. The influence of sediment recycling and basement composition on evolution of mudrock chemistry in the southwestern United States [J]. Geochimica et Cosmochimica Acta, 1995,59:2919-2940.
[278]Cullers R. L., Podkovyrov V. M. Geochemistry of the Mesoproterozoic Lakhanda shales in southeatern Yakutia, Russia:Implications for mineralogical and provenance control,and recycling[J]. Precambrian Research,2000,104:77-93.
[279]Cullers R. L. The source and origin of terrigenous sedimentary rocks in the Mesoproterozoic Ui group, southeastern Russia [J]. Precambrian Research,2002,117:157-183.
[280]Young G. M., Nesbitt H. W. Paleoclimatology and provenance of the glaciogenic Gowganda Formation (Paleoproterozoic), Ontario, Canada:A chemostratigraphic approach[J]. GSA Bulletin, 1999,111:264-274.
[281]李徐生,韩志勇,杨守业等.镇江下蜀土剖面的化学风化强度与元素迁移特征[J].地理学报,2007,62(11)：1174-1184.
[282]Fedo, C. M., Nesbitt, H. W., Young, G. M. Unraveling the effects of potassium metasomatism in sedimentary rocks and paleosols, with implications for paleoweathering conditions and provenance[J]. Geology,1995,.23,921-924.
[283]Matsuhisa, Y., Mizota, C., Faure, K., et al. Homogenization processes of fine particles in the arid regions of western China, inferred from oxygen isotope composition of quartz[J]. The Todai International Symposium on Cosmochronlogy and Isotope Geoscience Abstracts,1996,29-32.