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...
地质通报  2004 

晚白垩世以来沿阿尔金断裂带的阶段性走滑隆升

, PP. 926-932

Keywords: 阿尔金断裂,阶段性,走滑隆升,青藏高原

Full-Text   Cite this paper   Add to My Lib

Abstract:

年代学和沉积学特征表明,与印度板块约55MaBP以来沿喜马拉雅东、西构造结缝合带碰撞后青藏高原的阶段性隆升相对应,沿阿尔金断裂带阿尔金山地区亦发生阶段性走滑隆升,时间段大致为55~30MaBP、约20MaBP、约10MaBP和1~0.8MaBP.始新世-渐新世期间,阿尔金断裂大型左行走滑活动的发生,对中国西北大陆构造格架产生巨大的影响,不仅改造了古老的盆地和褶皱带,而且控制了新生代的走滑拉分盆地和两侧盆地的沉积速率,并对青藏高原的阶段性隆升和地壳物质东向蠕散起到调节作用.

References

[1]  Chen Yan, Gilder S, Halim N, et al. New paleomagnetic constraints on central Asian kinematics: Displacement along the Altyn Tagh fault and rotation of the Qaidam basin [J]. Tectonics,2002, 21(5):1042.
[2]  Matte P, Tapponnier P, Arnaud N, et al. Tectonics of Western Tibet, between the Tarim and the Indus [J]. Earth and Planetary Science Letters, 1996,142: 311~330.
[3]  葛肖虹,刘永江,任收麦,等.对阿尔金断裂科学问题的再认识[J].地质科学,2001,36(3):319~325.
[4]  International Union of the Geological Science. International Stratigraphic Chart[S]. 2000.
[5]  杨藩,马志强,许同春,等.柴达木盆地第三纪磁性地层柱[J].石油学报,1992,13(2):97~101.
[6]  贾承造,张师本,吴绍祖,等.塔里木盆地及周边地层(下册)[M].北京:科学出版社,2004.475~495.
[7]  Meng Qingren, Hu Jianmin, Yang Fuzhong. Timing and magnitude of displacement on the Altyn Tagh fault constraints from stratigraphic correlation of adjoining Tarim and Qaidam basins,NW China[J]. Terra Nova, 2001,13:86~91.
[8]  丁林,钟大赉,潘裕生,等.东喜马拉雅构造结上新世以来快速抬升的裂变径迹证据[J].科学通报,1995,40(16):1497~1500.
[9]  施雅风,李吉均,李炳元,等.晚新生代青藏高原的隆升与东亚环境变化[J].地理学报,1999,54(1):10~20.
[10]  方小敏,史正涛,杨胜利,等.天山黄土和古尔班通古特沙漠发育及北疆干旱化[J].科学通报,2001,47(7):540~545.
[11]  刘永江,葛肖虹,叶慧文,等.晚中生代以来阿尔金断裂的走滑模式[J].地球学报,2001,22(1):23~28.
[12]  靳久强,赵文智,薛良清,等.中国西北地区侏罗纪原型盆地与演化特征[J].地质论评,1999,45(1):92~104
[13]  葛肖虹.对中国西北部找油的战略思考[A].见:地质矿产部石油地质研究所编.石油与天然气地质文集第6集[C].北京:地质出版社,199712~18.
[14]  赵越,徐守礼,杨振宇.沿大型走滑断裂系的隆升[J].地质科学,1996,31(1):1~14.
[15]  李海兵,杨经绥,史仁灯,等.阿尔金走滑断陷盆地的确定及其与山脉的关系[J].科学通报,2002,47(1):63~67.
[16]  Wang Chengshan, Li Weifang. Sedimentary response in the Tertiary southwest Tarim basin to uplift history, northwest part of the Qinghai-Tibet Plateau[A]. In: 16th Himalaya-Karakorum-Tibet Workshop, Austria. Abstracts[Cl.2001.9.
[17]  Fang X M, H J J, Song C H, et al. pliocene synchronous rapid uplift of the Tibet Plateau: a summary of K-Ar and paleomagnetic dating of the Main Tibet surface rivers terraces and basin sediments[A]. In:16th Himalaya-Karakorum-Tibet Workshop, Austria. Abstracts[C]. 2001.16.
[18]  Chen Wangping, Chen Chuyyung, Nabelek J L. Present-day deformation of the Qaidam basin with implications for intracontinental tectonics[J]. Tectonophysics,1999,305:165~181.
[19]  李廷栋.青藏高原的深部构造和隆升机制[A].见:中国地质科学院主编.地质专报第7号?喜马拉雅岩石圈构造演化?总论[C].北京:地质出版社,1988.174~185.
[20]  Li Tingdong. The process and mechanism of the rise of the Qinghai-Tibet Plateau[J]. Tectonophysics, 1996,260 (1~3): 45~53.
[21]  Tapponnier P,Xu Zhiqin,Francoise R,et al.Oblique stepwise rise and growth of the Tibet plateau[J].Science,2001,294(23):1670~1677.
[22]  葛肖虹,刘永江,任收麦.青藏高原隆升动力学与阿尔金断裂[J].中国地质,2002,29(4):346~350.
[23]  葛肖虹,任收麦,刘永江,等中国西部的大陆构造格架[J].石油学报,2001,22(5):1~5.
[24]  Klootwijk C T. A review of Indian Phanerozoic paleomagnetism:implications for the India-Asia collision[J]. Tectonophysics, 1984,105: 331~353.
[25]  Rowley D B. Age of initiation of collision between India and Asia: A review of stratigraphic data[J]. Earth and Planetary Science Letters, 1996,145:1~13.
[26]  Spencer D A, Tonarini S, Pognante U. Geochemical and SrNd isotopic characterization of Higher Himalayan eclogites (andassociated metabasites)[J]. Eur. J. Mineral, 1995,7: 89~102.
[27]  Zeitler P K, Chamberlian C P. Petrogenetic and tectonic significance of young leucogranites from the northwest Himalaya,Pakistan[J]. Tectonics,1991,10:729~741.
[28]  刘永江,葛肖虹,叶慧文,等.阿尔金断裂变形岩激光微区 40Ar/39Ar年龄及其构造意义[J].科学通报,2000,45(19):2101~2104.
[29]  Liu Yongjiang, Genser J, Ge Xiaohong, et al. 40Ar/39Ar age evidence for Altyn fault tectonic activities in western China [J].Chinese Science Bulletin, 2003,48(18) :2024~2030.
[30]  Jolivet M, Brunel M, Seward D, et al. Mesozoic and Cenozoic tectonics of the northern edge of the Tibetan plateau:tission-track constraints[J]. Tectonophysics,2001,343:111~134.
[31]  王菲,罗清华,李齐,等.柴达木盆地北缘30Ma左右的去顶剥蚀作用-40Ar/39Ar热年代学定量制约[J].矿物岩石地球化学通报,2001,20(4):228~230.
[32]  Mock C, Arnaud N O, Cantagrel J M. An early unroofing in northeastern Tibet? Constraints from 40Ar/39Ar thermochronology on granitoids from the eastern Kunlun range (Qinghai, NW China)[J]. Earth and Planetary Science Letters, 1999, 171(1):107~122.
[33]  陈正乐,张岳桥,王小凤,等.新生代阿尔金山脉隆升历史的裂变径迹证据[J].地球学报,2001,22(5):413~418.
[34]  万景林,王瑜,李齐,等.阿尔金山北段晚新生代山体抬升的裂变径迹证据[J].矿物岩石地球化学通报,2001,20(4):222~224.
[35]  Arnaud N, Tapponnier P, Roger F, et al. Evidence for Mesozoic shear along the western Kunlun and Altyn-Tagh fault,northern Tibet (China) [J]. Journal of Geophysical Research,2003,108(B1) :ETG12-1 to 12~27.
[36]  葛肖虹,刘俊来.被肢解的"西域克拉通"[J].岩石学报,2000,16(1):59~66.
[37]  赵文津,纳尔逊K D.印度板块俯冲到藏南之下的深反射证据[J].地球学报,1996,17(2):131~137.
[38]  Zhang Jianxin, Zhang Zheming, Xu Zhiqin, et al. Petrology and geochronology of eclogites firom the western segment of the Altyn Tagh, northwestern China[J]. Lithos., 2001,56:187~206.
[39]  钟大赉,丁林.青藏高原的隆起及其机制探讨[J].中国科学(D辑),1996,26(4):289~295.
[40]  施雅风,李吉均,李炳元.青藏高原晚新生代隆升与环境变化[M].广州:广东科技出版社,1998.305.
[41]  Guo Z T, R uddiman W F, Hao Q Z, et al. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China[J]. Nature, 2002,416:159~163.
[42]  George A D, Marshallsea S J,Wyrwoll K H, et al. Miocene cooling in the northern Qilian Shan, northeastern margin of the Tibetan Plateau, revealed by apatite fission-track and vitrinitereflectance analysis[J]. Geology, 2001, 29(10): 939~942.
[43]  贾承造.中国塔里木盆地构造特征与油气[M].北京:石油工业出版社,1997.257.
[44]  Wang Xiaofeng, Chen Xuanhua, Chen Zhengle, et al. Timing of some important geological events in Altyn Tagh area, NW China [A]. In: 16th Himalaya-Karakorum-Tibet Workshop,Austria. Abstracts[C].2001.76.
[45]  Sun Jimin, Liu Tungsheng. Stratigraphic evidence for the uplift of the Tibetan Plateau between ~1.1 and ~0.9 Myr ago [J].Quaternary Research, 2000,54:309~320.
[46]  Liu Zechun, Wang Yongjin, Chen Ye, et al. Magnetostratigraphy and sedimentologically derived geochronology of the Quaternary lacustrine deposits of a 3000m thick sequence in the central Qaidam basin, western China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1998,140:459~473.
[47]  钱方,张金起.昆仑山口羌塘组磁性地层与新构造运动[J].地质力学学报,1997,3(1):50~56.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133