新疆西准噶尔唐巴勒蛇绿岩及其构造意义
|
摘要
本文以西准噶尔唐巴勒蛇绿岩为研究对象,从岩石组合、岩石学、岩石地球化学、构造环境、及大地构造意义等方面对该岩带作了比较系统的研究。
(1)唐巴勒蛇绿岩位于哈萨克斯坦—准噶尔板块唐巴勒—卡拉麦里古生代复合沟弧带内的准噶尔盆地西南部,出露宽度约4km～8km,由大小不等的多个超基性岩块组成,表现为组分齐全的蛇绿岩。
(2)空间位置关系上,蛇纹岩作为基质分布于岩带的最下部,辉长岩、辉石岩及玄武岩堆积于蛇纹岩之上,硅质岩覆盖在玄武岩之上。各单元之间由于后期构造破坏,均为断层接触。
(3)蛇绿岩中的辉长岩LA-ICP-MS锆石U—Pb测年结果显示,年龄分散且年轻(240-320Ma),代表热事件或者变质年龄,并不代表辉长岩形成的真实年龄。为此综合前人的年代学研究资料,认为唐巴勒蛇绿岩的年龄为447-531Ma,时代属于寒武纪—奥陶纪。
(4)唐巴勒蛇绿岩中玄武岩具有拉斑玄武岩特征,富集大离子亲石元素,亏损高场强元素和显示弱的或没有Eu异常,普遍具有Nb,Ta相对亏损。地球化学特征表明,其形成于弧后盆地环境。
(5)通过对抗蚀变元素Zr,Nb和Y分析,揭示唐巴勒蛇绿岩的岩浆来源于亏损地幔。
(6)综合前人资料及本次研究,西准噶尔地区寒武纪—奥陶纪曾经发生过一次北西向的洋内俯冲事件。
This dissertation is object on Tangbale ophiolitic in Western Junggar, Xinjiang. Systemic researching the character of ophiolitic of rock combination, petrology, formtive age、petrochemistry, geochemistry, tectonic setting, tectonic significance and so on.
(1)Tangbale ophiolitic distribute the southwest of Junggar basin, kazakhstan-Junggar plate Tangbale-Kalamaili Paleozoic complex trench arc zone, the width is about 4 to 8km, consist of kind of ultrabasicrock, has a complete sequence of ophiolite.
(2)The position of serpentinite is lowest as matrix, gabbro、diabase and basalt accumulate on the serpentinite, and siliceousrock cover with basalt. contact relation between each sequence was fault because of structural demolished.
(3)The gabbro, a sequence of ophiolitic, LA-ICP-MS zircon U-Pb dating shows that ages are disperse and young, stand for tectothermal event or metamorphic age, which can't stand the gabbro's true formation age. so synthesize former formation data, consider that Tangbale ophiolitic was formed about 447Ma-531Ma, belong to Cambrian-Ordovician.
(4)The basalts from the Tangbale ophiolitic display tholeiitic in composition with enrichment in LILEs (e.g., Rb, K and Ba), depletion in HFSEs (e.g., Nb, Ti, Zr and Hf) and weak or no Eu anomalies, depletion Nb, Ta generally, geochemistry character show Tangbale ophiolitic formed in back-arc basin setting。
(5)Insusceptible elements, such as Zr, Nb and Y, are employed to discriminate the nature of magma source of depleted mantle.
(6)This study and previous work constrains north westward subduction model in the West Junggar for the Cambrian-Ordovician.
(1)唐巴勒蛇绿岩位于哈萨克斯坦—准噶尔板块唐巴勒—卡拉麦里古生代复合沟弧带内的准噶尔盆地西南部,出露宽度约4km～8km,由大小不等的多个超基性岩块组成,表现为组分齐全的蛇绿岩。
(2)空间位置关系上,蛇纹岩作为基质分布于岩带的最下部,辉长岩、辉石岩及玄武岩堆积于蛇纹岩之上,硅质岩覆盖在玄武岩之上。各单元之间由于后期构造破坏,均为断层接触。
(3)蛇绿岩中的辉长岩LA-ICP-MS锆石U—Pb测年结果显示,年龄分散且年轻(240-320Ma),代表热事件或者变质年龄,并不代表辉长岩形成的真实年龄。为此综合前人的年代学研究资料,认为唐巴勒蛇绿岩的年龄为447-531Ma,时代属于寒武纪—奥陶纪。
(4)唐巴勒蛇绿岩中玄武岩具有拉斑玄武岩特征,富集大离子亲石元素,亏损高场强元素和显示弱的或没有Eu异常,普遍具有Nb,Ta相对亏损。地球化学特征表明,其形成于弧后盆地环境。
(5)通过对抗蚀变元素Zr,Nb和Y分析,揭示唐巴勒蛇绿岩的岩浆来源于亏损地幔。
(6)综合前人资料及本次研究,西准噶尔地区寒武纪—奥陶纪曾经发生过一次北西向的洋内俯冲事件。
This dissertation is object on Tangbale ophiolitic in Western Junggar, Xinjiang. Systemic researching the character of ophiolitic of rock combination, petrology, formtive age、petrochemistry, geochemistry, tectonic setting, tectonic significance and so on.
(1)Tangbale ophiolitic distribute the southwest of Junggar basin, kazakhstan-Junggar plate Tangbale-Kalamaili Paleozoic complex trench arc zone, the width is about 4 to 8km, consist of kind of ultrabasicrock, has a complete sequence of ophiolite.
(2)The position of serpentinite is lowest as matrix, gabbro、diabase and basalt accumulate on the serpentinite, and siliceousrock cover with basalt. contact relation between each sequence was fault because of structural demolished.
(3)The gabbro, a sequence of ophiolitic, LA-ICP-MS zircon U-Pb dating shows that ages are disperse and young, stand for tectothermal event or metamorphic age, which can't stand the gabbro's true formation age. so synthesize former formation data, consider that Tangbale ophiolitic was formed about 447Ma-531Ma, belong to Cambrian-Ordovician.
(4)The basalts from the Tangbale ophiolitic display tholeiitic in composition with enrichment in LILEs (e.g., Rb, K and Ba), depletion in HFSEs (e.g., Nb, Ti, Zr and Hf) and weak or no Eu anomalies, depletion Nb, Ta generally, geochemistry character show Tangbale ophiolitic formed in back-arc basin setting。
(5)Insusceptible elements, such as Zr, Nb and Y, are employed to discriminate the nature of magma source of depleted mantle.
(6)This study and previous work constrains north westward subduction model in the West Junggar for the Cambrian-Ordovician.
引文
[1]Buckman, S., Aitchison, J.C.2004. Tectonic evolution of Paleozoic terranes in West Junggar, Xinjiang, NW China. In:Malpas, J., Fletcher, C.J.N., Aitchison, J.C. (Eds.), Aspects of the Tectonic Evolution of China [J]. Geological Society of London, Special Publication.226,101-129.
[2]Church W R, Riccio L.1977. Fractionation trend of the bay of islands of Newfoundland:polycyclic cumulate sequences in ophiolites and their classification. Can. Earth Sci.,14:1156-1165
[3]Coleman, R G 1977. Ophiolites:Ancient Oceanic Lithosphere[M]. Berlin:Springer-Verlag,1-140.
[4]Coleman, R.G.1989. Continental Growth of Northest China. Tectonics,8(3):621-635.
[5]Coleman, R. G, Keith, T. E. C.1971. A chemical study of serpentinization-Burro Mountain, California [J]. Journal of Petrology,12:311-328.
[6]Dewey, J.F., Bird, J.1971. Origin and emplacement of the ophiolite suite:Appalachian ophiolites in Newfoundland[J]. Journal of Geophysical Research,76:3179-3206.
[7]Feng, Y., R. G. Coleman, G.Tilton, X.Xiao,1989. Tectonic evolution of the West Junggar region, Xinjiang, China. Tectonics,8:729-752.
[8]Frey F A.1984. Rare earth element abundance in upper mantlrocks. In:HendersonP(ed.). Rare Earth Elemen Geochemistry[M]. Elesevier Science PublisherB.V.,153-203.
[9]Gass, I. G. 1968. Is the Troodos Massif of Cyprus a fragment of Mesozoic oceanic floor? [J]. Nature,220:39-42.
[10]Geng, H.Y., Sun, M., Yuan, C., Zhao, G.C., Xiao, W.J.2011. Geochemical and geochronological study of early Carboniferous volcanic rocks from the West Junggar:petrogenesis and tectonic implications [J]. Journal of Asian Earth Sciences, doi:10.1016/j.jseaes.2011.01.006.
[11]Hollings P., Kerrich,R.,2004. Geochemical systematics of tholeiites from the 2.86 Ga Pickle Crow assemblage, northwestern Ontario Arc basalts with positive and negative Nb-Hf anomalies. Precambrian Research,134:1-20.
[12]Ishiwatari A.1985. Igneous petrogenesis of the Yakuno ophiolite (Japan) in the context of the diversity of ophiolites. Contrib. Mineral. petrol.,89:155-167.
[13]Jian P, Liu DY, Shi YR and Zhang FQ.2005. SHRIMP dating of SSZ ophiolites from northern Xinjiang Province, China:Implications for generation of oceanic crust in the central Asian orogenic belt. In:Sklyarov EV (ed.). Structural and Tectonic Correlation across the Central Asian Orogenic Collage:Northeastern Segment. Guidebook and Abstract Volume of the Siberian Workshop IGCP-480,1-246.
[14]Kidd, R. G. W.1977. A model for the process of formation of the upper oceanic crust [J]. Geophysical Journal of the Royal Astronmical Society,50:149-183.
[15]Kwon, S. T., Tilton, G.R., Coleman, R. G., et al.1989. Isotopic investigation on the tectonic of the west Junggar, Xinjiang, China[J]. Tectonics,8:719-727.
[16]Meschede, M.,1986. A method of discriminating between differeni types of mid-ocean ridge and continental tholeiites with the Nb-Zr-Y diagram. Chem Geol,56:207-218(in English).
[17]Melcher F, Meisel T, Puhl J.2002. PeLrogenesis and geotectonic setting of ultramafic rocks in the Eastern Alps:constrains from geochemistry[J]. LiLhos,65:69-112.
[18]Moores, E. M., Vine, F. J.1971. The Troodos massif, Cyprus and other ophiolites as oceanic crust: evaluation and implicat Philos [J]. Trans.R.Soc., A268:433-466.
[19]Mullen, E. D.,1983. MnO/TiO2/P2O5:a minor element discrimination for basaltic tacks of oceanic environments and its implications for petrogenesis. Earth Planet Sci.Lett.,62:53-62(in English).
[20]Pearce, J. A., Cann, J. R.,1973. Tectonic setting of basaltic volcanic rocks using trace element analysis. Earth Planet. Sci. Lett.19:290-300.
[21]Pearce J.A., Deng WM.1983. The ophiolites of the Geotraverse, Lhasa to Golmud (1985) and Lhasa to Kathmandu (1986).In:Chang C et al. (eds.). The Geological Evolution of the Tibet. London:The Royal Society,215-238.
[22]Pearce, J.A., Peate, D.W.1995. Tectonic implications of the composition of volcanic ARC magmas [J]. Annual Review of Earth and Planetary Sciences.23:251-285.
[23]Pearce, J.A., Norry, M.J.1979 Petrogenetic implications of Ti, Zr, Y and Nb variations in volcanic rocks [J]. Contributions to Mineralogy and Petrology.69,33-47.
[24]Peng, G. Y.1996. Podiform chromite and associate rocks in Western Junggar. China. PhD:1-369.
[25]Robertson A H F.2002. Overview of the genesis and emplacement of Mesozoic ophiolites in the
Eastern Mediterranean Tethyan regin. Lithos,65:1-67
[26]Shervais JW.1982. Ti-V plot and the petrogenesis of modern and ophiolitic lavas. Earth and Planetary of Science Letters 59,101-118.
[27]Wilson M.1989. Igneous Petrogenesis[M].London:Unwin Hyman,21-22.
[28]Zhang, C., M. G. Zhai, M.B.Allen, A. D. Saunder, G. R. Wang, X.Huang,1993. Implications of Palaeozoic Ophiolites from Western Junggar, NW China, for the Tectonics of Central Asia. Journal of Geological Society,150:551-561.
[29]白文吉,P. Robinson,杨经绥,周美付,胡旭峰.1995,西准噶尔不同时代蛇绿岩及其构造演化.岩石学报,11：62-72.
[30]白文吉,杨经绥,施倪承等.2004.西藏罗布莎蛇绿岩地幔岩首次发现超高压矿物方铁矿和自然铁[J].地质论评,50(2)：184-188.
[31]冯益民.1987.西准噶尔古板块构造特征.中国地质科学院西安地质矿产研究所所刊,18：141-160.
[32]辜平阳,李永军,张兵等.2009.西准达尔布特蛇绿岩中辉长岩LA-ICP-MS锆石U-Pb测年.岩石学报,25(6)：1364-72.
[33]管云彬.1990.新疆西准噶尔地区唐巴勒蛇绿岩的岩石学及地球化学研究(摘要).地质地球化学.
[34]郝梓国.1988.新疆西准噶尔地区蛇绿岩与豆荚型铬铁矿床的成因研究.中国地质科学院攻读博士学位研究生毕业论文.
[35]郝梓国,王希斌,鲍佩生等.1989.新疆西准噶尔地区两类蛇绿岩的地质特及其成因研究[J].岩石矿物学杂志,8：299-310.
[36]何国琦,李茂松.2001.中国新疆北部奥陶—志留系岩石组合的古构造、古地理意义.北京大学学报(自然科学版),37(6)：852-858.
[37]霍有光.1984.西准噶尔唐巴勒地区蛇绿岩套岩石化学和稀土元素特征及其地质意义.中国地质科学院西安地质矿产研究所所刊,(7)：82-94.
[38]李才,翟庆国,董永胜等.2008.冈瓦纳大陆北缘早期的洋壳信息—来自青藏高原羌塘中部早古生代蛇绿岩的证据.地质通报,27(10)：1605—1612
[39]李金铭,师占义.1985a.新疆西准噶尔地区地幔岩的特征及其演化.西北地质,(3)：20-28.
[40]李金铭,师占义.1985b.新疆西准噶尔地区超基性岩中地幔团块的结构与组构.中国地质科学院地质矿产研究所所刊,(11)：33-49
[41]李金铭.1994.新疆西准噶尔地区唐巴勒超基性岩体地幔岩残体的超微构造与组构特征[J].西北地质科学,15(1)：1-10.
[42]李曙光.1993.蛇绿岩生成构造环境的Ba-Th-Nb-La判别图[J].岩石学报,9(2)：146-157.
[43]李嵩龄,张志德,杨德朴.1986.新疆西准噶尔地区早古生代超基性岩岩石化学特征.新疆地质.4(2)：45-53.
[44]刘本培,冯庆来,方念乔等.1995.滇西南昌宁—孟连和澜沧江带古特提斯多岛洋构造演化[J].
地球科学,18(5)：529-539.
[45]Jarvis K.E.等著,尹明,李冰译.1997.电感耦合等离子体质谱手册.北京：原子能出版社.
[46]邵济安,唐克东等.1995.中国东北地体与东北亚大陆边缘演化.北京：地质出版社,1—185
[47]史仁灯.2005.蛇绿岩研究进展、存在问题及思考[J].地质论评,51(6)：681-693.
[48]唐克东,邵济安.1996.古亚洲洋区蛇绿岩的某些特征与古洋演化[J].见：张旗主编.蛇绿岩与地球动力学研究.北京：地质出版社,108-111.
[49]王树庆,许继峰,刘希军等.2008.内蒙朝克山蛇绿岩地球化学：洋脊弧后盆地的产物?[J].岩石学报,24(12)：2869-79.
[50]王金荣,谢荣,王怀涛等.2011.新疆西准噶尔阿克乔克花岗岩年代学地球化学及构造意义[J].兰州大学学报(自然科学版),47(1)：127-128.
[51]王希斌,鲍佩声,戎合.1995.中国蛇绿岩中变质橄榄岩的稀土元素地球化学[J].岩石学报,11(增刊)：24-41.
[52]夏林圻,夏祖春,徐学义等.2007.利用地球化学手段判别大陆玄武岩和岛弧玄武岩[J].岩石矿物学杂志,26(1)：77-89,
[53]肖序常,汤耀庆,冯益民.1992.新疆北部及其邻区大地构造[M].北京：地质出版社,1—169.
[54]新疆维吾尔族自治区地质矿产局.1993.新疆维吾尔族自治区区域地质志[M].北京：地质出版社.
[55]新疆维吾尔族自治区地质矿产局,1999.新疆维吾尔族自治区岩石地层[M].北京：中国地质大学出版社.
[56]许继峰,陈繁荣,于学元等.2001.新疆北部阿尔泰地区库尔提蛇绿岩：古弧后盆地系统的产物.岩石矿物学杂志,20(3)：344-352.
[57]徐新,何国琦,李华芹等.2006.克拉玛依蛇绿混杂岩带的基本特征和锆石SHRIMP年龄信息[J].中国地质,33：470-475.
[58]杨瑞瑛.1993.西准噶尔地区中奥陶纪火山岩的地球化学特征.地球化学,(4)：399-408.
[59]杨瑞瑛.2006.中子活化法研究唐巴勒蛇绿岩中超镁铁质岩的地球化学特征[J].现代仪器,6：18-20.
[60]张驰,黄萱.1992.新疆西准噶尔蛇绿岩形成时代和环境讨论[J].地质论评,38：509-524.
[61]张弛,黄萱,翟明国.1995.新疆西准噶尔蛇绿岩地质特征及其形成环境和时代[J].中国科学院地质研究所集刊,8：165-218.
[62]张弛,翟明国.1993.西准噶尔蛇绿岩带及其形成环境[J].见：涂光炽主编.新疆北部固体地球科学进展.北京：科学出版社,53-78.
[63]张立飞.1997.疆西准噶尔唐巴勒蓝片岩40Ar/39Ar年龄及其地质意义[J].科学通报,42：2178-2181.
[64]张旗.1990.蛇绿岩的分类[J].地质科学,25(1)：54-61
[65]张旗.1994.蛇绿岩研究的进展[J].地学前缘,1(2)：98-103
[66]张旗.1995a.蛇绿岩研究中的几个问题[J].岩石学报,11(增刊)：228-240.
[67]张旗,肖序常.1995b.中国蛇绿岩研究概述[J].岩石学报,11 (增刊):1-9.
[68]钟立峰,夏斌,周国庆等.2006.藏南罗布莎蛇绿岩辉绿岩中锆石SHRIMP测年[J].地质评论,52(2)：224-229.
[69]朱宝清,冯益民.1994.新疆西准噶尔板块构造及演化[J].新疆地质,12(02)：91-105.
[70]朱宝清,王来生,王连晓.1987.西准噶尔西南地区古生代蛇绿岩[M].西安地质矿产研究所所刊,17：3-64.
[71]朱永峰,徐新,魏少妮.2007.西准噶尔克拉玛依OIB型枕状玄武岩地球化学及其地质意义研究[J],岩石学报,023(07)：1739-48.
[72]朱永锋,徐新.2006.新疆塔尔巴哈台发现早奥陶世蛇绿岩[J].岩石学报,22(12)：2833-2842.
[2]Church W R, Riccio L.1977. Fractionation trend of the bay of islands of Newfoundland:polycyclic cumulate sequences in ophiolites and their classification. Can. Earth Sci.,14:1156-1165
[3]Coleman, R G 1977. Ophiolites:Ancient Oceanic Lithosphere[M]. Berlin:Springer-Verlag,1-140.
[4]Coleman, R.G.1989. Continental Growth of Northest China. Tectonics,8(3):621-635.
[5]Coleman, R. G, Keith, T. E. C.1971. A chemical study of serpentinization-Burro Mountain, California [J]. Journal of Petrology,12:311-328.
[6]Dewey, J.F., Bird, J.1971. Origin and emplacement of the ophiolite suite:Appalachian ophiolites in Newfoundland[J]. Journal of Geophysical Research,76:3179-3206.
[7]Feng, Y., R. G. Coleman, G.Tilton, X.Xiao,1989. Tectonic evolution of the West Junggar region, Xinjiang, China. Tectonics,8:729-752.
[8]Frey F A.1984. Rare earth element abundance in upper mantlrocks. In:HendersonP(ed.). Rare Earth Elemen Geochemistry[M]. Elesevier Science PublisherB.V.,153-203.
[9]Gass, I. G. 1968. Is the Troodos Massif of Cyprus a fragment of Mesozoic oceanic floor? [J]. Nature,220:39-42.
[10]Geng, H.Y., Sun, M., Yuan, C., Zhao, G.C., Xiao, W.J.2011. Geochemical and geochronological study of early Carboniferous volcanic rocks from the West Junggar:petrogenesis and tectonic implications [J]. Journal of Asian Earth Sciences, doi:10.1016/j.jseaes.2011.01.006.
[11]Hollings P., Kerrich,R.,2004. Geochemical systematics of tholeiites from the 2.86 Ga Pickle Crow assemblage, northwestern Ontario Arc basalts with positive and negative Nb-Hf anomalies. Precambrian Research,134:1-20.
[12]Ishiwatari A.1985. Igneous petrogenesis of the Yakuno ophiolite (Japan) in the context of the diversity of ophiolites. Contrib. Mineral. petrol.,89:155-167.
[13]Jian P, Liu DY, Shi YR and Zhang FQ.2005. SHRIMP dating of SSZ ophiolites from northern Xinjiang Province, China:Implications for generation of oceanic crust in the central Asian orogenic belt. In:Sklyarov EV (ed.). Structural and Tectonic Correlation across the Central Asian Orogenic Collage:Northeastern Segment. Guidebook and Abstract Volume of the Siberian Workshop IGCP-480,1-246.
[14]Kidd, R. G. W.1977. A model for the process of formation of the upper oceanic crust [J]. Geophysical Journal of the Royal Astronmical Society,50:149-183.
[15]Kwon, S. T., Tilton, G.R., Coleman, R. G., et al.1989. Isotopic investigation on the tectonic of the west Junggar, Xinjiang, China[J]. Tectonics,8:719-727.
[16]Meschede, M.,1986. A method of discriminating between differeni types of mid-ocean ridge and continental tholeiites with the Nb-Zr-Y diagram. Chem Geol,56:207-218(in English).
[17]Melcher F, Meisel T, Puhl J.2002. PeLrogenesis and geotectonic setting of ultramafic rocks in the Eastern Alps:constrains from geochemistry[J]. LiLhos,65:69-112.
[18]Moores, E. M., Vine, F. J.1971. The Troodos massif, Cyprus and other ophiolites as oceanic crust: evaluation and implicat Philos [J]. Trans.R.Soc., A268:433-466.
[19]Mullen, E. D.,1983. MnO/TiO2/P2O5:a minor element discrimination for basaltic tacks of oceanic environments and its implications for petrogenesis. Earth Planet Sci.Lett.,62:53-62(in English).
[20]Pearce, J. A., Cann, J. R.,1973. Tectonic setting of basaltic volcanic rocks using trace element analysis. Earth Planet. Sci. Lett.19:290-300.
[21]Pearce J.A., Deng WM.1983. The ophiolites of the Geotraverse, Lhasa to Golmud (1985) and Lhasa to Kathmandu (1986).In:Chang C et al. (eds.). The Geological Evolution of the Tibet. London:The Royal Society,215-238.
[22]Pearce, J.A., Peate, D.W.1995. Tectonic implications of the composition of volcanic ARC magmas [J]. Annual Review of Earth and Planetary Sciences.23:251-285.
[23]Pearce, J.A., Norry, M.J.1979 Petrogenetic implications of Ti, Zr, Y and Nb variations in volcanic rocks [J]. Contributions to Mineralogy and Petrology.69,33-47.
[24]Peng, G. Y.1996. Podiform chromite and associate rocks in Western Junggar. China. PhD:1-369.
[25]Robertson A H F.2002. Overview of the genesis and emplacement of Mesozoic ophiolites in the
Eastern Mediterranean Tethyan regin. Lithos,65:1-67
[26]Shervais JW.1982. Ti-V plot and the petrogenesis of modern and ophiolitic lavas. Earth and Planetary of Science Letters 59,101-118.
[27]Wilson M.1989. Igneous Petrogenesis[M].London:Unwin Hyman,21-22.
[28]Zhang, C., M. G. Zhai, M.B.Allen, A. D. Saunder, G. R. Wang, X.Huang,1993. Implications of Palaeozoic Ophiolites from Western Junggar, NW China, for the Tectonics of Central Asia. Journal of Geological Society,150:551-561.
[29]白文吉,P. Robinson,杨经绥,周美付,胡旭峰.1995,西准噶尔不同时代蛇绿岩及其构造演化.岩石学报,11：62-72.
[30]白文吉,杨经绥,施倪承等.2004.西藏罗布莎蛇绿岩地幔岩首次发现超高压矿物方铁矿和自然铁[J].地质论评,50(2)：184-188.
[31]冯益民.1987.西准噶尔古板块构造特征.中国地质科学院西安地质矿产研究所所刊,18：141-160.
[32]辜平阳,李永军,张兵等.2009.西准达尔布特蛇绿岩中辉长岩LA-ICP-MS锆石U-Pb测年.岩石学报,25(6)：1364-72.
[33]管云彬.1990.新疆西准噶尔地区唐巴勒蛇绿岩的岩石学及地球化学研究(摘要).地质地球化学.
[34]郝梓国.1988.新疆西准噶尔地区蛇绿岩与豆荚型铬铁矿床的成因研究.中国地质科学院攻读博士学位研究生毕业论文.
[35]郝梓国,王希斌,鲍佩生等.1989.新疆西准噶尔地区两类蛇绿岩的地质特及其成因研究[J].岩石矿物学杂志,8：299-310.
[36]何国琦,李茂松.2001.中国新疆北部奥陶—志留系岩石组合的古构造、古地理意义.北京大学学报(自然科学版),37(6)：852-858.
[37]霍有光.1984.西准噶尔唐巴勒地区蛇绿岩套岩石化学和稀土元素特征及其地质意义.中国地质科学院西安地质矿产研究所所刊,(7)：82-94.
[38]李才,翟庆国,董永胜等.2008.冈瓦纳大陆北缘早期的洋壳信息—来自青藏高原羌塘中部早古生代蛇绿岩的证据.地质通报,27(10)：1605—1612
[39]李金铭,师占义.1985a.新疆西准噶尔地区地幔岩的特征及其演化.西北地质,(3)：20-28.
[40]李金铭,师占义.1985b.新疆西准噶尔地区超基性岩中地幔团块的结构与组构.中国地质科学院地质矿产研究所所刊,(11)：33-49
[41]李金铭.1994.新疆西准噶尔地区唐巴勒超基性岩体地幔岩残体的超微构造与组构特征[J].西北地质科学,15(1)：1-10.
[42]李曙光.1993.蛇绿岩生成构造环境的Ba-Th-Nb-La判别图[J].岩石学报,9(2)：146-157.
[43]李嵩龄,张志德,杨德朴.1986.新疆西准噶尔地区早古生代超基性岩岩石化学特征.新疆地质.4(2)：45-53.
[44]刘本培,冯庆来,方念乔等.1995.滇西南昌宁—孟连和澜沧江带古特提斯多岛洋构造演化[J].
地球科学,18(5)：529-539.
[45]Jarvis K.E.等著,尹明,李冰译.1997.电感耦合等离子体质谱手册.北京：原子能出版社.
[46]邵济安,唐克东等.1995.中国东北地体与东北亚大陆边缘演化.北京：地质出版社,1—185
[47]史仁灯.2005.蛇绿岩研究进展、存在问题及思考[J].地质论评,51(6)：681-693.
[48]唐克东,邵济安.1996.古亚洲洋区蛇绿岩的某些特征与古洋演化[J].见：张旗主编.蛇绿岩与地球动力学研究.北京：地质出版社,108-111.
[49]王树庆,许继峰,刘希军等.2008.内蒙朝克山蛇绿岩地球化学：洋脊弧后盆地的产物?[J].岩石学报,24(12)：2869-79.
[50]王金荣,谢荣,王怀涛等.2011.新疆西准噶尔阿克乔克花岗岩年代学地球化学及构造意义[J].兰州大学学报(自然科学版),47(1)：127-128.
[51]王希斌,鲍佩声,戎合.1995.中国蛇绿岩中变质橄榄岩的稀土元素地球化学[J].岩石学报,11(增刊)：24-41.
[52]夏林圻,夏祖春,徐学义等.2007.利用地球化学手段判别大陆玄武岩和岛弧玄武岩[J].岩石矿物学杂志,26(1)：77-89,
[53]肖序常,汤耀庆,冯益民.1992.新疆北部及其邻区大地构造[M].北京：地质出版社,1—169.
[54]新疆维吾尔族自治区地质矿产局.1993.新疆维吾尔族自治区区域地质志[M].北京：地质出版社.
[55]新疆维吾尔族自治区地质矿产局,1999.新疆维吾尔族自治区岩石地层[M].北京：中国地质大学出版社.
[56]许继峰,陈繁荣,于学元等.2001.新疆北部阿尔泰地区库尔提蛇绿岩：古弧后盆地系统的产物.岩石矿物学杂志,20(3)：344-352.
[57]徐新,何国琦,李华芹等.2006.克拉玛依蛇绿混杂岩带的基本特征和锆石SHRIMP年龄信息[J].中国地质,33：470-475.
[58]杨瑞瑛.1993.西准噶尔地区中奥陶纪火山岩的地球化学特征.地球化学,(4)：399-408.
[59]杨瑞瑛.2006.中子活化法研究唐巴勒蛇绿岩中超镁铁质岩的地球化学特征[J].现代仪器,6：18-20.
[60]张驰,黄萱.1992.新疆西准噶尔蛇绿岩形成时代和环境讨论[J].地质论评,38：509-524.
[61]张弛,黄萱,翟明国.1995.新疆西准噶尔蛇绿岩地质特征及其形成环境和时代[J].中国科学院地质研究所集刊,8：165-218.
[62]张弛,翟明国.1993.西准噶尔蛇绿岩带及其形成环境[J].见：涂光炽主编.新疆北部固体地球科学进展.北京：科学出版社,53-78.
[63]张立飞.1997.疆西准噶尔唐巴勒蓝片岩40Ar/39Ar年龄及其地质意义[J].科学通报,42：2178-2181.
[64]张旗.1990.蛇绿岩的分类[J].地质科学,25(1)：54-61
[65]张旗.1994.蛇绿岩研究的进展[J].地学前缘,1(2)：98-103
[66]张旗.1995a.蛇绿岩研究中的几个问题[J].岩石学报,11(增刊)：228-240.
[67]张旗,肖序常.1995b.中国蛇绿岩研究概述[J].岩石学报,11 (增刊):1-9.
[68]钟立峰,夏斌,周国庆等.2006.藏南罗布莎蛇绿岩辉绿岩中锆石SHRIMP测年[J].地质评论,52(2)：224-229.
[69]朱宝清,冯益民.1994.新疆西准噶尔板块构造及演化[J].新疆地质,12(02)：91-105.
[70]朱宝清,王来生,王连晓.1987.西准噶尔西南地区古生代蛇绿岩[M].西安地质矿产研究所所刊,17：3-64.
[71]朱永峰,徐新,魏少妮.2007.西准噶尔克拉玛依OIB型枕状玄武岩地球化学及其地质意义研究[J],岩石学报,023(07)：1739-48.
[72]朱永锋,徐新.2006.新疆塔尔巴哈台发现早奥陶世蛇绿岩[J].岩石学报,22(12)：2833-2842.