汝箕沟地区中生代构造环境分析
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摘要
鄂尔多斯盆地西缘构造带由于所处的重要构造环境以及良好的油气和煤炭资源前景,长期以来就引起能源工作者的广泛关注。区内的汝箕沟地区是我国重要的太西煤的产地,盛产世界上少有的低灰低硫优质无烟煤。
本论文在充分收集前人资料和课题研究的基础上,以构造地质学、层序地层学和沉积学为理论依据,结合现有的基础地质资料与最新测试成果和相关论文,配合地球化学分析的方法,从贺兰山汝箕沟地区中生代的地层特征,岩石特性,沉积分析及构造变形等方面的研究入手,通过典型的地质现象分析,探讨了贺兰山汝箕沟地区中生代构造环境属性。
(1)通过汝箕沟地区中生代晚三叠世-早中侏罗世的地层特征,沉积分析和鄂尔多斯盆地内部进行对比、晚三叠世延长组及早侏罗世沉积物源和古水流向分析,推断出汝箕沟地区在中生代早中期是鄂尔多斯盆地的一部分,物源区主要是来自于北部的正谊关断裂;
(2)通过对汝箕沟玄武岩地质地球化学指标,稀土和微量元素测试资料进行的多种判别分析,确定该玄武岩为板内拉斑玄武岩,形成于板内张性构造环境,其形成时代为晚三叠世-早中侏罗世,反映了该时期汝箕沟地区处于拉张的区域构造环境;
(3)通过小松山断层面之下地层分布规律,顺层断层特征及裂变径迹测试资料,结合其变形特点,认为中生代汝箕沟地区西麓处于一个由东向西平缓抬高的斜坡环境,小松山断层是一重力滑覆断层,它代表了近东西向的拉张,目前汝箕沟地区西麓东高西低的剖面特征是该区后期构造反转的结果;
(4)综合分析论证得出,汝箕沟地区在晚三叠世-早中侏罗世处于近东西向拉张应力背景下的区域构造环境,具有拉张断陷性质。
Because of the western margin of ordos basin tectonic belt locates in the important tectonic setting as well as the bright prospect of its oil, gas and coal resources, it has widely aroused energy worker's interest and attention for a long time. Rujigou area is an important area of Taixi coal producing area of our country. Taixi coal which is low ash and sulfur,while high quality anthracite is very rare in the world.
This thesis is basesd on collecting the predecessor material and the researchs on this topic, taking the tectonic geology, the sequence stratigraphy and the sedimentology as the theory bases, unifing the existing foundation geological data with the newest test achievement and the related papers, and coordinating the geochemistry analysis method. It starts with formation characteristics, the rock characteristics, the deposition analysis and constructure distortion researchs,etc of the Rujigou area Mesozoic Era's. Through the analysis of typical geological phenomenon, the author of this thesis has discussed the nature of Rujigou area mesozoic tectonic setting.
(1)Through comparison between Rujigou area Mesozoic Era late Triassic period-early and middle Jurassic period formation characteristics, sedimentation analysis and that of Ordos Basin and the analysis of the late Triassic period extension and early-middle Jurassic Period deposit provenance it sets forth that during the period. Rujigou area was part of the Ordos basin and the provenance originated Zhengyiguan fault;
(2)Through the analysises of the indicators of the Rujigou basalt geology geochemistry, the rare earth and the trace element test material, it is determined that this basalt for within-plate tholeiite basalt formed in within-plate extension tectonic setting in the late Triassic-middle Jurassic periods. It reflectes that this period the Rujigou area is in the extension tectonic setting;
(3)According to the stratum distribution rules and characteristic of the Xiao Sungshan bedding fault, and the fission diameter mark test materials, and its distortion characteristics, the author of this thesis belives that thought that the Mesozoic Era, the western ridge of Rujigou area used to be on a slope and topography slowly declines from west to east. The Xiao Sungshan bedding fault used to be gravity slip detachment struture and it has represented the extension from the east to west. At present the Rujigou area is higher in the east and lower in the west, which is the result of the reversion of this area in later time;
(4)It can be concludes that, in Mesozoic Era late Triassic period-early and middle Jurassic period, Rujigou area was in east-west region tensional stress environment which was tensional fault subsidence.
本论文在充分收集前人资料和课题研究的基础上,以构造地质学、层序地层学和沉积学为理论依据,结合现有的基础地质资料与最新测试成果和相关论文,配合地球化学分析的方法,从贺兰山汝箕沟地区中生代的地层特征,岩石特性,沉积分析及构造变形等方面的研究入手,通过典型的地质现象分析,探讨了贺兰山汝箕沟地区中生代构造环境属性。
(1)通过汝箕沟地区中生代晚三叠世-早中侏罗世的地层特征,沉积分析和鄂尔多斯盆地内部进行对比、晚三叠世延长组及早侏罗世沉积物源和古水流向分析,推断出汝箕沟地区在中生代早中期是鄂尔多斯盆地的一部分,物源区主要是来自于北部的正谊关断裂;
(2)通过对汝箕沟玄武岩地质地球化学指标,稀土和微量元素测试资料进行的多种判别分析,确定该玄武岩为板内拉斑玄武岩,形成于板内张性构造环境,其形成时代为晚三叠世-早中侏罗世,反映了该时期汝箕沟地区处于拉张的区域构造环境;
(3)通过小松山断层面之下地层分布规律,顺层断层特征及裂变径迹测试资料,结合其变形特点,认为中生代汝箕沟地区西麓处于一个由东向西平缓抬高的斜坡环境,小松山断层是一重力滑覆断层,它代表了近东西向的拉张,目前汝箕沟地区西麓东高西低的剖面特征是该区后期构造反转的结果;
(4)综合分析论证得出,汝箕沟地区在晚三叠世-早中侏罗世处于近东西向拉张应力背景下的区域构造环境,具有拉张断陷性质。
Because of the western margin of ordos basin tectonic belt locates in the important tectonic setting as well as the bright prospect of its oil, gas and coal resources, it has widely aroused energy worker's interest and attention for a long time. Rujigou area is an important area of Taixi coal producing area of our country. Taixi coal which is low ash and sulfur,while high quality anthracite is very rare in the world.
This thesis is basesd on collecting the predecessor material and the researchs on this topic, taking the tectonic geology, the sequence stratigraphy and the sedimentology as the theory bases, unifing the existing foundation geological data with the newest test achievement and the related papers, and coordinating the geochemistry analysis method. It starts with formation characteristics, the rock characteristics, the deposition analysis and constructure distortion researchs,etc of the Rujigou area Mesozoic Era's. Through the analysis of typical geological phenomenon, the author of this thesis has discussed the nature of Rujigou area mesozoic tectonic setting.
(1)Through comparison between Rujigou area Mesozoic Era late Triassic period-early and middle Jurassic period formation characteristics, sedimentation analysis and that of Ordos Basin and the analysis of the late Triassic period extension and early-middle Jurassic Period deposit provenance it sets forth that during the period. Rujigou area was part of the Ordos basin and the provenance originated Zhengyiguan fault;
(2)Through the analysises of the indicators of the Rujigou basalt geology geochemistry, the rare earth and the trace element test material, it is determined that this basalt for within-plate tholeiite basalt formed in within-plate extension tectonic setting in the late Triassic-middle Jurassic periods. It reflectes that this period the Rujigou area is in the extension tectonic setting;
(3)According to the stratum distribution rules and characteristic of the Xiao Sungshan bedding fault, and the fission diameter mark test materials, and its distortion characteristics, the author of this thesis belives that thought that the Mesozoic Era, the western ridge of Rujigou area used to be on a slope and topography slowly declines from west to east. The Xiao Sungshan bedding fault used to be gravity slip detachment struture and it has represented the extension from the east to west. At present the Rujigou area is higher in the east and lower in the west, which is the result of the reversion of this area in later time;
(4)It can be concludes that, in Mesozoic Era late Triassic period-early and middle Jurassic period, Rujigou area was in east-west region tensional stress environment which was tensional fault subsidence.
引文
[1]丁振举.贺兰断褶带北西向构造的遥感解译[J].中国煤田地质总局,1992,4(2)
[2]霍福臣,潘行适,尤国林等.宁夏地质概论[M].北京:科学出版社,1989,224
[3]高山林,李芳,李天斌等.汝箕沟晚中生代玄武岩的确定与煤变质作用关系简论[J].煤田地质与勘探,2003,31(3):8-10
[4]甘克文.鄂尔多斯盆地西缘的构造和古油气远景[C].(见《鄂尔多斯盆地西缘地区石油地质文集》).内蒙古民出版社,1983
[5]黄喜峰,钱壮志,吴文奎等.贺兰山小松山基性-超基性杂岩体岩石地球化学特征[J].地球科学与环境学报,2008,30(4):352-356
[6]柯保嘉,陈昌明,汪寿松.试论贺兰山地区延长群与鄂尔多斯盆地的关系[J].地质科学,1992
[7]康铁笙,王世成.地质热历史研究的裂变径迹法[M].北京:科学出版社,1991
[8]李振宏,张军,郑聪斌.鄂尔多斯盆地西缘断裂特征与油气运聚研究[J].石油物探,2005,44(3)
[9]李天斌.鄂尔多斯盆地西缘逆冲推覆构造特征及演化[D].北京:中国地质大学,2006
[10]李斌.鄂尔多斯盆地西缘前陆盆地构造特征和油气成藏研究[D].广州:中国科学院广州地球化学研究所,2006
[11]刘和甫,陆伟文,王玉新.鄂尔多斯西缘冲断褶皱带形成与形变[A].见:杨俊杰主编,鄂尔多斯盆地西缘逆冲带构造与油气[C].兰州:甘肃科学技术出版社,1990:54-75
[12]刘少峰,杨士恭.鄂尔多斯盆地西缘南北差异及其形成机制[J].地质科学,1997,32(3):397-408
[13]李思田,程守田,杨士恭等.鄂尔多斯盆地东北部层序地层及沉积体系分析[M].北京:地质出版社,1992,11-12
[14]李捷.贺兰山北段地质构造[J].地质知识,1954(2):34-36
[15]路凤香等.岩石学[M].北京:地质出版社,2001
[16]陆克政.含油气盆地分析[M].山东:石油大学出版社,2001
[17]林畅松,杨起,李思田.贺兰拗拉槽盆地充填演化分析[M].北京:地质出版社,1995,1-143
[18]李向平,陈刚.鄂尔多斯盆地中生代构造事件及其沉积响应特点[J].西安石油大学学报(自然科学版),2006,3(21)
[19]刘少锋,柯爱蓉,吴丽云.鄂尔多斯西南缘前陆盆地沉积物物源分析及其构造意义[J].沉积学 报,1997,15(1):156-159
[20]刘池洋,赵红格,王锋等,鄂尔多斯盆地西缘(部)中生代构造属性[J].地质学报,2005,79(6):737-747
[21]刘池洋,赵红格,杨兴科等.前陆盆地及其确定和研究[J].石油与天然气地质,2002,23(4):307-313
[22]刘继庆,苏生瑞.贺兰山北段的伸展构造[J].西北地质,1993,14(62)
[23]宁夏回族自治区地质矿产局.宁夏回族自治区岩石地层[M].武汉:中国地质大学出版社,1996,1-132
[24]宁夏回族自治区地质矿产局.宁夏回族自治区区域地质志[M].北京:地质出版社,1990:145-339
[25]内蒙古石油学会编.鄂尔多斯盆地西缘地区石油地质论文集[C].呼和浩特内蒙古人民出版社,1984,50-68
[26]苏春乾,杨兴科,刘继庆等.从贺兰山区的三叠-侏罗系论国内前陆盆地的研究[J].岩石矿物学杂志,2004,23(4):318-326
[27]孙书勤,汪云亮,张成江.玄武岩类岩石大地构造环境的Th、Nb、Zr判别[J].地质论评,2003,49(1):40-47
[28]孙肇才.简论鄂尔多斯盆地地质构造风格及其油气潜力[J].石油实验地质,2000,22(4):291-296
[29]苏春乾,刘仿韩.贺兰山三叠纪断陷盆地的沉积体系及古地理分析[J].西安地质学院学报,1995,17(1)
[20]苏春乾,刘仿韩.汝箕沟侏罗纪断陷盆地的沉积相分析[J].西安地质学院学报,1995,17(1):28-33
[31]孙书勤,张成江,黄润秋.板块汇聚边缘玄武岩大地构造环境的Th、Nb、Zr判别[J].地球科学进展,2006,6(21)
[32]孙书勤,张成江,赵松江.大陆板内构造环境的微量元素判别[M].大地构造成矿学,2007,1(31),104-109
[33]汤锡元,郭忠铭.陕甘宁盆地西缘逆冲推覆构造及油气勘探[M].陕西西安:西北大学出版社,1992,101-114
[34]王晓鹏,刘彦堂,张忠富.对汝箕沟煤田含煤地层的讨论[J].中国煤田地质,2005,17(5)
[35]魏红红,李文厚,邵磊等.汝箕沟盆地上三叠统延长组沉积环境[J].西北大学学报(自然科学版),2001,31(2):171-174
[36]王锋,刘池洋,赵红格等.贺兰山盆地与鄂尔多斯盆地的关系[J].石油学报,2006,27(4):15-17,22
[37]汤锡元,郭忠铭,王定一.鄂尔多斯盆地西部逆冲推覆构造带特征及其演化与油气勘探[J].石油与天然气地质,1988,9(1):1-10
[38]魏红红,彭惠群,李静群等.鄂尔多斯盆地石炭-二叠系沉积特征与储集条件[J].石油与天然气地质,1998,19(2):136-141
[39]王锋,刘池洋,杨兴科等.贺兰山汝箕沟玄武岩地质地球化学特征及其构造环境意义[J].大庆石油地质与开发,2005,24(4):25-27
[40]汪云亮,张成江,修淑芝.玄武岩形成的大地构造环境的Th/Hf--Ta/Hf图解判别[J].岩石学报,2001,17(3):413-421
[41]武莉娜,王志畅,汪云亮.微量元素La,Nb,Zr在判别大地构造环境方面的应用[J].华东地质学院学报,2003,26(4):343-348
[42]王锋,刘池洋,赵红格等.贺兰山西麓中生代构造反转及意义[J].石油实验地质,2005,28(3):206-209
[43]王锋,赵红格.鄂尔多斯地块西部构造研究中几个值得注意的问题[J].中国地质,2007,34(3)
[44]夏义平,徐礼贵,郑良合.鄂尔多斯盆地西缘逆冲断裂带构造特征及油气勘探方向[J].中国石油勘探,2005.10(5):17-20
[45]杨兴科.鄂尔多斯盆地东西缘热力构造特点及其SHRIMP测年意义.鄂尔多斯盆地及邻区中新生代演化动力学及其资源效应学术研讨会论文.2005
[46]杨俊杰.鄂尔多斯盆地构造演化与油气分布规律[M].北京:石油工业出版社,2002:1-36
[47]赵红格,刘池洋,王锋.鄂尔多斯盆地西缘的构造分区性探讨[J].地学前缘,2005,12(4):542
[48]赵红格,刘池洋,王锋.贺兰山隆升时限及其演化[J].中国科学,2007,1(增刊)37:185-192
[49]张学文,穆桂松,孟方等.宁夏汝箕沟矿区煤层气地质学特征[J].煤田地质与勘探,2005,3(33)
[50]张进,马宗晋,任文军.贺兰山南部构造特征及其与固原-青铜峡断裂的关系[J].吉林大学学报,2004,2(34)
[51]张进,马宗晋,任文军.再论贺兰山南部北西向构造成因[J].地球科学与环境学报,2005,1(27)
[52]王锋,刘池洋,赵红格.鄂尔多斯地块西部南北向拆离滑覆构造[J].地球科学与环境学报, 2004,1(23)
[53]张树明,王方正.玄武岩在研究岩石圈深部过程及构造背景中的应用[J].地球科学进展,2002,17(5):690-695
[54]郑海飞等.元素比值和元素丰度模式法的可靠性实验研究[J].矿物学岩石学地球化学研究新进展.兰州大学出版社.1994
[55]张成江,汪云亮,侯增谦.蛾眉山玄武岩系的Th、Ta、Hf特征及岩浆源区大地构造环境探讨[J].地质论评,1999,45(增刊):858-860
[56]张进,马宗晋,任文军.再论贺兰山地区新生代之前拉张活动的性质[J].石油学报,2004,25(6):8-11
[57]张泓等.鄂尔多斯聚煤盆地的形成及构造环境[J].煤田地质与勘探,1995,23(3):1-9
[58]张慧,晋香兰,张泓,李小彦,吴传荣.鄂尔多斯盆地西缘汝箕沟煤矿区的石英脉及其地质意义[J].地质学报,2006,79(6):757-773
[59]张泓,何宗莲,晋香兰.鄂尔多斯盆地构造演化与成煤作用[M].北京:地质出版社,2005,17-24
[60]张庆龙,解国爱,任文军等.鄂尔多斯盆地西缘南北向断裂的发育及其地质意义[J].石油实验地质,2002,24(2):119-125
[61]赵红格,刘池洋,王锋.鄂尔多斯盆地西缘构造分区及其特征[J].石油与天然气地质,2006,27(2):173-178
[62]长庆油田地质志编写组.中国石油地质志(卷十二)一长庆油田[M].北京:石油工业出版社,1992
[63]长安大学(原西安地质学院).呼鲁斯太、古拉本幅1:5万区域地质调查报告[R].1991
[64]西安地质学院区调队,1:5万区域地质调查报告[R].1991
[65]宁夏地质矿产局区调队,阿左旗幅1:20万区域地质调查报告[R].1983
[66]久野.火山及火山岩[C].刘德权,常子文译.北京:地质出版社,1978
[67]Davis J and Hawkesworth C.The petrogenesis of 30-20 Mabasic and intermediate volcanics from the Mogollon-Datil Volcanic Field,New Mexico,U.S.A.Contrib[J].Miner.Petrol.,1993,115:165-183
[68]Hawkesworth CJ,O'Nions RK,Pankhurst RJet al..A geochemical study of island-are and back-arc tholeiites from Scotia Sea[J].Earth Planet.Sci.Lett.,1977,36:253-262
[69]Ormerod DS,Rogers NW and Hawkesworth CJ.Melting inthe lithospheric mantle.Inverse modelling of alkali olivine basalt from the Big Pine volcanic field,California.Contrib[J].Miner.Petrol, 1991,108:305-317
[70]ShinjoR,Chung S L,KatoY,etal.Geochemical and Sr-Nd i-sotopic characteristics of volcanic rocks from theOkinawa Troughand Ryukyu Arc:Implications for the evolution of a young,intracontinental back arc basin[J].Journal ofGeophysicalResearch,1999,104(B5):10 591-10 608
[2]霍福臣,潘行适,尤国林等.宁夏地质概论[M].北京:科学出版社,1989,224
[3]高山林,李芳,李天斌等.汝箕沟晚中生代玄武岩的确定与煤变质作用关系简论[J].煤田地质与勘探,2003,31(3):8-10
[4]甘克文.鄂尔多斯盆地西缘的构造和古油气远景[C].(见《鄂尔多斯盆地西缘地区石油地质文集》).内蒙古民出版社,1983
[5]黄喜峰,钱壮志,吴文奎等.贺兰山小松山基性-超基性杂岩体岩石地球化学特征[J].地球科学与环境学报,2008,30(4):352-356
[6]柯保嘉,陈昌明,汪寿松.试论贺兰山地区延长群与鄂尔多斯盆地的关系[J].地质科学,1992
[7]康铁笙,王世成.地质热历史研究的裂变径迹法[M].北京:科学出版社,1991
[8]李振宏,张军,郑聪斌.鄂尔多斯盆地西缘断裂特征与油气运聚研究[J].石油物探,2005,44(3)
[9]李天斌.鄂尔多斯盆地西缘逆冲推覆构造特征及演化[D].北京:中国地质大学,2006
[10]李斌.鄂尔多斯盆地西缘前陆盆地构造特征和油气成藏研究[D].广州:中国科学院广州地球化学研究所,2006
[11]刘和甫,陆伟文,王玉新.鄂尔多斯西缘冲断褶皱带形成与形变[A].见:杨俊杰主编,鄂尔多斯盆地西缘逆冲带构造与油气[C].兰州:甘肃科学技术出版社,1990:54-75
[12]刘少峰,杨士恭.鄂尔多斯盆地西缘南北差异及其形成机制[J].地质科学,1997,32(3):397-408
[13]李思田,程守田,杨士恭等.鄂尔多斯盆地东北部层序地层及沉积体系分析[M].北京:地质出版社,1992,11-12
[14]李捷.贺兰山北段地质构造[J].地质知识,1954(2):34-36
[15]路凤香等.岩石学[M].北京:地质出版社,2001
[16]陆克政.含油气盆地分析[M].山东:石油大学出版社,2001
[17]林畅松,杨起,李思田.贺兰拗拉槽盆地充填演化分析[M].北京:地质出版社,1995,1-143
[18]李向平,陈刚.鄂尔多斯盆地中生代构造事件及其沉积响应特点[J].西安石油大学学报(自然科学版),2006,3(21)
[19]刘少锋,柯爱蓉,吴丽云.鄂尔多斯西南缘前陆盆地沉积物物源分析及其构造意义[J].沉积学 报,1997,15(1):156-159
[20]刘池洋,赵红格,王锋等,鄂尔多斯盆地西缘(部)中生代构造属性[J].地质学报,2005,79(6):737-747
[21]刘池洋,赵红格,杨兴科等.前陆盆地及其确定和研究[J].石油与天然气地质,2002,23(4):307-313
[22]刘继庆,苏生瑞.贺兰山北段的伸展构造[J].西北地质,1993,14(62)
[23]宁夏回族自治区地质矿产局.宁夏回族自治区岩石地层[M].武汉:中国地质大学出版社,1996,1-132
[24]宁夏回族自治区地质矿产局.宁夏回族自治区区域地质志[M].北京:地质出版社,1990:145-339
[25]内蒙古石油学会编.鄂尔多斯盆地西缘地区石油地质论文集[C].呼和浩特内蒙古人民出版社,1984,50-68
[26]苏春乾,杨兴科,刘继庆等.从贺兰山区的三叠-侏罗系论国内前陆盆地的研究[J].岩石矿物学杂志,2004,23(4):318-326
[27]孙书勤,汪云亮,张成江.玄武岩类岩石大地构造环境的Th、Nb、Zr判别[J].地质论评,2003,49(1):40-47
[28]孙肇才.简论鄂尔多斯盆地地质构造风格及其油气潜力[J].石油实验地质,2000,22(4):291-296
[29]苏春乾,刘仿韩.贺兰山三叠纪断陷盆地的沉积体系及古地理分析[J].西安地质学院学报,1995,17(1)
[20]苏春乾,刘仿韩.汝箕沟侏罗纪断陷盆地的沉积相分析[J].西安地质学院学报,1995,17(1):28-33
[31]孙书勤,张成江,黄润秋.板块汇聚边缘玄武岩大地构造环境的Th、Nb、Zr判别[J].地球科学进展,2006,6(21)
[32]孙书勤,张成江,赵松江.大陆板内构造环境的微量元素判别[M].大地构造成矿学,2007,1(31),104-109
[33]汤锡元,郭忠铭.陕甘宁盆地西缘逆冲推覆构造及油气勘探[M].陕西西安:西北大学出版社,1992,101-114
[34]王晓鹏,刘彦堂,张忠富.对汝箕沟煤田含煤地层的讨论[J].中国煤田地质,2005,17(5)
[35]魏红红,李文厚,邵磊等.汝箕沟盆地上三叠统延长组沉积环境[J].西北大学学报(自然科学版),2001,31(2):171-174
[36]王锋,刘池洋,赵红格等.贺兰山盆地与鄂尔多斯盆地的关系[J].石油学报,2006,27(4):15-17,22
[37]汤锡元,郭忠铭,王定一.鄂尔多斯盆地西部逆冲推覆构造带特征及其演化与油气勘探[J].石油与天然气地质,1988,9(1):1-10
[38]魏红红,彭惠群,李静群等.鄂尔多斯盆地石炭-二叠系沉积特征与储集条件[J].石油与天然气地质,1998,19(2):136-141
[39]王锋,刘池洋,杨兴科等.贺兰山汝箕沟玄武岩地质地球化学特征及其构造环境意义[J].大庆石油地质与开发,2005,24(4):25-27
[40]汪云亮,张成江,修淑芝.玄武岩形成的大地构造环境的Th/Hf--Ta/Hf图解判别[J].岩石学报,2001,17(3):413-421
[41]武莉娜,王志畅,汪云亮.微量元素La,Nb,Zr在判别大地构造环境方面的应用[J].华东地质学院学报,2003,26(4):343-348
[42]王锋,刘池洋,赵红格等.贺兰山西麓中生代构造反转及意义[J].石油实验地质,2005,28(3):206-209
[43]王锋,赵红格.鄂尔多斯地块西部构造研究中几个值得注意的问题[J].中国地质,2007,34(3)
[44]夏义平,徐礼贵,郑良合.鄂尔多斯盆地西缘逆冲断裂带构造特征及油气勘探方向[J].中国石油勘探,2005.10(5):17-20
[45]杨兴科.鄂尔多斯盆地东西缘热力构造特点及其SHRIMP测年意义.鄂尔多斯盆地及邻区中新生代演化动力学及其资源效应学术研讨会论文.2005
[46]杨俊杰.鄂尔多斯盆地构造演化与油气分布规律[M].北京:石油工业出版社,2002:1-36
[47]赵红格,刘池洋,王锋.鄂尔多斯盆地西缘的构造分区性探讨[J].地学前缘,2005,12(4):542
[48]赵红格,刘池洋,王锋.贺兰山隆升时限及其演化[J].中国科学,2007,1(增刊)37:185-192
[49]张学文,穆桂松,孟方等.宁夏汝箕沟矿区煤层气地质学特征[J].煤田地质与勘探,2005,3(33)
[50]张进,马宗晋,任文军.贺兰山南部构造特征及其与固原-青铜峡断裂的关系[J].吉林大学学报,2004,2(34)
[51]张进,马宗晋,任文军.再论贺兰山南部北西向构造成因[J].地球科学与环境学报,2005,1(27)
[52]王锋,刘池洋,赵红格.鄂尔多斯地块西部南北向拆离滑覆构造[J].地球科学与环境学报, 2004,1(23)
[53]张树明,王方正.玄武岩在研究岩石圈深部过程及构造背景中的应用[J].地球科学进展,2002,17(5):690-695
[54]郑海飞等.元素比值和元素丰度模式法的可靠性实验研究[J].矿物学岩石学地球化学研究新进展.兰州大学出版社.1994
[55]张成江,汪云亮,侯增谦.蛾眉山玄武岩系的Th、Ta、Hf特征及岩浆源区大地构造环境探讨[J].地质论评,1999,45(增刊):858-860
[56]张进,马宗晋,任文军.再论贺兰山地区新生代之前拉张活动的性质[J].石油学报,2004,25(6):8-11
[57]张泓等.鄂尔多斯聚煤盆地的形成及构造环境[J].煤田地质与勘探,1995,23(3):1-9
[58]张慧,晋香兰,张泓,李小彦,吴传荣.鄂尔多斯盆地西缘汝箕沟煤矿区的石英脉及其地质意义[J].地质学报,2006,79(6):757-773
[59]张泓,何宗莲,晋香兰.鄂尔多斯盆地构造演化与成煤作用[M].北京:地质出版社,2005,17-24
[60]张庆龙,解国爱,任文军等.鄂尔多斯盆地西缘南北向断裂的发育及其地质意义[J].石油实验地质,2002,24(2):119-125
[61]赵红格,刘池洋,王锋.鄂尔多斯盆地西缘构造分区及其特征[J].石油与天然气地质,2006,27(2):173-178
[62]长庆油田地质志编写组.中国石油地质志(卷十二)一长庆油田[M].北京:石油工业出版社,1992
[63]长安大学(原西安地质学院).呼鲁斯太、古拉本幅1:5万区域地质调查报告[R].1991
[64]西安地质学院区调队,1:5万区域地质调查报告[R].1991
[65]宁夏地质矿产局区调队,阿左旗幅1:20万区域地质调查报告[R].1983
[66]久野.火山及火山岩[C].刘德权,常子文译.北京:地质出版社,1978
[67]Davis J and Hawkesworth C.The petrogenesis of 30-20 Mabasic and intermediate volcanics from the Mogollon-Datil Volcanic Field,New Mexico,U.S.A.Contrib[J].Miner.Petrol.,1993,115:165-183
[68]Hawkesworth CJ,O'Nions RK,Pankhurst RJet al..A geochemical study of island-are and back-arc tholeiites from Scotia Sea[J].Earth Planet.Sci.Lett.,1977,36:253-262
[69]Ormerod DS,Rogers NW and Hawkesworth CJ.Melting inthe lithospheric mantle.Inverse modelling of alkali olivine basalt from the Big Pine volcanic field,California.Contrib[J].Miner.Petrol, 1991,108:305-317
[70]ShinjoR,Chung S L,KatoY,etal.Geochemical and Sr-Nd i-sotopic characteristics of volcanic rocks from theOkinawa Troughand Ryukyu Arc:Implications for the evolution of a young,intracontinental back arc basin[J].Journal ofGeophysicalResearch,1999,104(B5):10 591-10 608