全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
地球学报  2004 

阿尔金造山带中、新生代的演化

Keywords: 阿尔金造山带,塔里木盆地,敦煌盆地,柴达木盆地,走滑断裂

Full-Text   Cite this paper   Add to My Lib

Abstract:

塔里木盆地东缘的阿尔金造山带中、新生代经历了一个复杂的大地构造演化历程:中生代早期(T)为隆升夷平,中生代中后期(J-K)为裂陷沉积阶段;自古新世一中新世因塔里木盆地向东挤压使得阿尔金造山带东南缘出现了右行走滑仰冲,柴达木壳体向阿尔金造山带之下俯冲,阿尔金造山带隆起。塔里木盆地相对柴达木盆地向北移动,最大距离可达400~500km,使得原来统一的塔里木-敦煌-柴达木联合盆地裂解。由于逆冲走滑使阿尔金造山带内部发育了一系列小型的走滑盆地,形成了复杂的盆地沉积建造,并伴有动力变质及火山作用;中新世末,东西向挤

References

[1]  Yang Sennan;Yang Weiran,Regional geotectonics in China,北京:地质出版社,1985.
[2]  Yang Fan;Ye Sujuan;Cao Chunchao,Right lateral characteristics of the middle eastern segment of altun fault in Cenozoic Era,Geologica Sinica,1994(04).
[3]  Xun Zhiqin;Yang Jingsui;Zhang Jianxin,A comparison between the tectonic units on the two sides of the Altun sinistral strike-slip Fault and the mechanism of lithospheric shearing,Acta Geologica Sinica,1999(03).
[4]  高锐;李廷栋;吴功建,青藏高原岩石圈演化与地球动力学过程—亚东—格尔木—额济纳旗地学断面的启示,地质论评,1998(04).
[5]  刘训;姚建新;王永,再论塔里木板块的归属问题,地质论评,1997(01).
[6]  黄汲清,中国大地构造特征的新研究,中国地质科学院院报,1984.
[7]  黄汉纯;王长利,阿尔金构造带及其对塔里木和柴达木盆地的影响,中国地质科学院院报,1987.
[8]  ZHOU Yong;Pan Yusheng,Determination of the dextral slip of mangya-subei segment of altun fault,Scientia Geologica Sinica,1998(01).
[9]  Sun Yong;Liu Chiyang;Che Zicheng,The proterozoic rift volcanic series in the lapeiquan area, the Altun mountains and its tectonic significance,Geological Review,1997(01).
[10]  Ren Jishun;Jiang Chunfa;Zhang Zhengkun,Geotectonics in China and its evolution,北京:科学出版社,1980.
[11]  Ma Zongjin;Zhang Jiasheng;Wang Yipeng,The 3-D deformational movement episodes and neotectonic domains in the Qinghai-Tibet plateau,Acta Geologica Sinica,1998(03).
[12]  Liu Xun;Yao Jianxin;Wang Yong,The review of tectonic attribution of the tarim plate,Geological Review,1997(01).
[13]  Huang Jiqing;Ren Jishun;Jiang Chunfa,Basic outline of geotectonics in China,Acta Geologica Sinica,1987(02).
[14]  Huang Hanchun;Wang Changli,Altun structural belt and its influence on the Tarim and the Qaidam basin,Bulletin of the Chinese Academy of Geological Sciences(in Chinese),1987(17).
[15]  Ge Xiaohong;Zhang Haisheng;Liu Yongjiang,Scientific problems and thought for research of the Altun fault,Geologica Sinila,1998(02).
[16]  陈正乐;万景林;王小凤.阿尔金断裂带8 Ma左右的快速走滑及其地质意义[J].地球学报,2002(04)
[17]  Chen Zhengle;Wan Jinglin;Wang Xiaofeng.Rapid strike-slip of the Altun Tagh fault at 8 Ma and its geological implications[J].Acta Geoscientia Sinica,2002(04)
[18]  Cai Xuelin;Wei Xianggui;Lin Yuanchao,Tectonic style of strike-slip fault in Altun mountains,Journal of Chengdu College of Geology,1992(01).
[19]  周勇;潘裕生,茫崖-肃北段阿尔金断裂右旋走滑运动的确定,地质科学,1998(01).
[20]  郑剑东,阿尔金断裂带的几何学研究,中国区域地质,1991(01).
[21]  余辉龙;邓宏文;胡勇.从古地磁资料看柴达木盆地古构造环境[J].石油勘探与开发,2002(06)
[22]  许志琴;杨经绥;张建新,阿尔金断裂两侧构造单元的对比及岩石圈构造机制,地质学报,1999(03).
[23]  魏国齐;贾承先;施央申.塔里木新生代复合再生前陆盆地构造特征与油气[J].地质学报,2000(02)
[24]  任纪舜;姜春发;张正坤,中国大地构造及其演化,北京:科学出版社,1980.
[25]  潘桂棠;焦淑沛;徐光耀,阿尔金造山带新生代构造及造山性质,北京:地质出版社,1984.
[26]  Chen Zhengle;Zhang Yueqiao;Wang Xiaofeng.Fission track dating of apatite constrains on the Cenozoic of the Altun Tagh mountain[J].Acta Geoscientia Sinica,2001(05)
[27]  陈正乐;张岳桥;王小凤.新生代阿尔金山脉隆升历史的裂变径迹证据[J].地球学报,2001(05)
[28]  焦淑沛,塔里木-柴达木地洼区的地史演化特征及其归属问题,北京:地质出版社,1984.
[29]  黄汲清;任纪舜;姜春发,中国大地构造基本轮廓,地质学报,1977(02).
[30]  葛肖虹;张梅生;刘永江,阿尔金断裂研究的科学问题与研究思路,现代地质,1998(12).
[31]  ZHOU Yong;Pan Yusheng,The initial shear sense of the Altun fault and its timing,Geological Review,1999(01).
[32]  Zheng Jiandong,Research on the geometry of the Altun fault zone,Regional Geology in China,1991(01).
[33]  Zhang Jianxin;Xu Zhiqin;Cui Junwen,Deformation partitioning of ductile transpressional zones: an example from the eastern segment of the Altun fault zone,Geological Review,1998(04).
[34]  Yu Huilong;Deng Hongwen;Hu Yong.Paleo-stuctutal environment study by paleomagnetism data in Qaidam basin[J].Petroleum Exploration and Development,2002(06)
[35]  Xie Xiaoan;Hu Suyun;Lu Huafu,Positive inversion structure in the Bachu fault-uplit in the Tarim basin,Geological Review,1998(01).
[36]  Wei Guoqi;Jia Chengxian;Shi Yangshen,Tectonic characteristics and petroleum prospects of Cenozoic compound rejuvenated foreland basin in Tarim,Acta Geologica Sinica,2000(74).
[37]  Pan Guitang;Jiao Shupei;Xu Guangyao,The Cenozoic tectonics and its orogeny in Altun,北京:地质出版社,1984.
[38]  Huang Jiqing,New reserches on the tectonic characteristics of China,Bulletin of the Chinese Academy of Geological Sciences(in Chinese),1984(15).
[39]  Gao Rui;Li Tingdong;Wu Gongjian,Lithospheric evolution and geodynamic process of the Qinghai-Tibet plateau:an inspiration from the Yadong-Golmud-Ejin geoscience transect,Geological Review,1998(04).
[40]  Zhou D. ;Graham SA.,EXTRUSION OF THE ALTYN TAGH WEDGE - A KINEMATIC MODEL FOR THE ALTYN TAGH FAULT AND PALINSPASTIC RECONSTRUCTION OF NORTHERN CHINA,Geology?,1996, 24(5).
[41]  蔡学林,阿尔金造山带走滑断裂构造样式,成都地质学院学报,1992(01).
[42]  周勇;潘裕生,阿尔金断裂早期走滑运动方向及其活动时间探讨,地质论评,1999(01).
[43]  张建新;许志琴;崔军文,一个韧性转换挤压带的变形分解作用-以阿尔金断裂东段为例,地质论评,1998(04).
[44]  杨森楠;杨巍然,中国区域大地构造学,北京:地质出版社,1985.
[45]  杨藩;叶素娟;曹春潮,新生代阿尔金断层中、东段右行走滑特征,地质科学,1994(04).
[46]  谢晓安;胡素云;卢华复,探讨塔里木盆地巴楚断隆的正反转构造,地质论评,1998(01).
[47]  孙勇;刘池阳;车自成,阿尔金造山带拉配泉地区元古宙裂谷火山岩及其构造意义,地质论评,1997(01).
[48]  马宗晋;张家声;汪一鹏,青藏高原三维变形运动学的时段划分和新构造区,地质学报,1998(03).

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133