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地球学报  2006 

西藏札达盆地形成演化与喜马拉雅山隆升

DOI: 10.3975/cagsb.2006.03.01

Keywords: 西藏札达,上新世—早更新世,盆地演化,山脉隆升,喜马拉雅山

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Abstract:

通过野外地质调查、实测地层剖面和室内综合研究,笔者将札达盆地上新世—早更新世形成演化划分为6个阶段①盆地初始断陷阶段;②盆地加速断陷阶段;③盆地强烈断陷阶段;④盆地断陷止息阶段;⑤盆地二次初始断陷阶段;⑥盆地二次加速断陷阶段。并以札达盆地形成演化为基础将喜马拉雅山此阶段的隆升划分为5个阶段①慢速隆升阶段(5.4~4.4Ma);②中速隆升阶段(4.4~3.5Ma);③快速隆升阶段(3.5~3.2Ma);④停止隆升阶段(3.2~2.7Ma);⑤快速隆升阶段(2.7Ma)。研究表明,喜马拉雅山的隆升是一个多阶段、不等速和非均变的复杂过程。

References

[1]  Zhu Xiaomin,Principium and Application of Sequenc Stratigraphy,北京:石油工业出版社,1998.
[2]  潘桂棠;王培生;徐耀荣,青藏高原新生代构造演化,北京:地质出版社,1990.
[3]  西藏自治区地质矿产局,西藏自治区岩石地层,武汉:中国地质大学出版社,.
[4]  Zhao W;Nelson K D,Project INDEPTH Team,Deep seismic reflection evidence for continental underthrusting beneath southern Tibet,Nature,1993.
[5]  Zhang Qingsong;Wang Fubao;Li Binyuan,Pliocene strata of Zhada basin,Tibet,Journal of Stratigraphy,1981(02).
[6]  Yin A;Harrison T M;Murphy M A;Grove,M Nie,S Ryerson,F.J Wang,X and Chen,Z,Tertiary deformation history of southeastern and southwestern Tibet during the Indo-Asian Collision,Geological Society of America Bulletin? ,1999, 111.
[7]  Wang Chengshan;Ding Xuelin,New progress of the study on Himalaya uplift and its sedimentary response,Geological Science and Technology Information,1998(01).
[8]  ,腹足类化石由中国地质科学院地质研究所李子舜研究员鉴定,2005.
[9]  ,孢粉分析由中国地质科学院水文地质研究所童国榜研究员鉴定,2004.
[10]  ,鼠兔臼齿化石由中国科学院古脊椎与古人类研究所金昌柱研究员、孙承凯博士鉴定,2005.
[11]  ,ESR年龄由成都理工大学ESR实验室梁兴中教授测试,2004.
[12]  ,古地磁年龄由地质力学研究所古地磁实验室测定,2004.
[13]  Rea D K,Delivery of Himalayan sediment to the northern Indian Ocean and its relation to global climate,sea level,uplift,and seawater strontium,Geophysical Monograph,1992.
[14]  Zhu Dagang;Meng Xiangang;Shao Zhaogang.Discovery of two unconformities in Pliocene-early Pleistocene fluvio-lacustrine deposits in the Zanda basin,Ngari,Tibet[J].Geological Bulletin of China,2004(5-6)
[15]  Pan Guitang;Wang Peisheng;Xu Yaoru,Cenozoic tectonic evolution of Qinghai-Xizang plateau,北京:地质出版社,1990.
[16]  Li Bingyuan;Wang Fubao;Zhang Qingsong,Quaternary Geology in Xizang,in the Series of the Scientific Expedition to the Qinghai-Xizang Plateau,北京:科学出版社,1983.
[17]  Bureau of Geology and Mineral Resources of Xizang Autonomous Region,Strtigraphy (Lithostratic) of Xizang Autonomous Region,武汉:中国地质大学出版社,1997.
[18]  朱筱敏,层序地层学原理及应用,北京:石油工业出版社,1998.
[19]  朱大岗;赵希涛;孟宪刚.从冰川剥蚀作用看念青唐古拉山脉(中段)的隆升[J].地球学报,2005(02)
[20]  赵政璋;李永铁;叶和飞,青藏高原地层,北京:科学出版社,2001.
[21]  张青松;王富葆;李炳元,西藏札达盆地的上新世地层,地层学杂志,1981(02).
[22]  李炳元;王富葆;张青松,西藏第四纪地质,北京:科学出版社,1983.
[23]  钱方,用古地磁方法对西藏阿里上新世以来水平运动的初步研究,北京:地质出版社,1990.
[24]  Zhu Dagang;Zhao Xitao;Meng Xiangang.A discussion on the uplifting of the central part of the Nyainqenlanglha range in the light of glacier denudation[J].Acta Geoscientia Sinica,2005(02)
[25]  王富葆;李生峰;申旭辉,吉隆盆地的形成演化、环境变化与喜马拉雅山隆起,中国科学D辑,1996(04).
[26]  王成善;丁学林,喜马拉雅的隆起及其沉积反映新进展,地质科技情报,1998(01).
[27]  钱方.青藏高原晚新生代磁性地层研究[J].地质力学学报,1999(04)
[28]  Yin An.Geological evolution of orogenic belt in Himalaya-Tibet[J].Acta Geoscientia Sinica,2001(03)
[29]  Willems H,Sedimentary history of the Tibetan Tethys Himalaya continental shelf in south Tibet (Gamba,Tingni) during Upper Cretaceous and Lower Teriary (Xizang Autonomous Region,P R China),Berichte Fachhereich Geowissenschaften Universitat Bremen,1993.
[30]  Wang Fubao;Li Shenghui;Shen Xuhui,The formatiom and evolution of the Jilong basin,environment evolution and Himalaya Uplift,Science in China(Earth Sciences),1996(04).
[31]  ,介形类化石由中国地质科学院地质力学研究所田国强副研究员鉴定,2004.
[32]  ,植物化石由北京大学史前生命与环境研究所古植物室蒋进庄博士鉴定,2003.
[33]  Qian Fang.Study on magnetostratigraphy in Qinghai-Tibetan plateau in late Cenozoic[J].Journal of Geomechanics,1999(04)
[34]  Qian Fang,The primary study of Pliocene level movement of Zhada,Tibet by paleomagnetism,北京:地质出版社,1990.
[35]  孟宪刚;朱大岗;邵兆刚.西藏阿里札达盆地上新统犀类化石的发现及意义[J].地质通报,2004(5-6)
[36]  Zhu Dagang;Meng Xiangang;Shao Zhaogang.Features of Pliocene-Lower Pleistocene sedimentary facies and tectonic evolution in the Zhada basin,Ngari area,Tibet[J].Journal of Geomechanics,2004(03)
[37]  Zhao Zhengzhang;Li Yongtie;Ye Hefei,Strata of Qinghai-Tibetan Plateau,北京:科学出版社,2001.
[38]  Meng Xiangang;Zhu Dagang;Shao Zhaogang.Discovery of rhinoceros fossils in the Pliocene in the Zanda basin,Ngari,Tibet[J].Geological Bulletin of China,2004(5-6)
[39]  Guo Tieying;Liang Dingyi;Zhang Yizhi,Geology of Ngari Tibet (Xizang),武汉:中国地质大学出版社,1991.
[40]  Brookfield M E,The Himalayan passive margin from Precambrian to Cretaceous sedimentary,Geology,1993.
[41]  朱大岗;孟宪刚;邵兆刚.西藏阿里札达盆地上新世-早更新世河湖相沉积中两个不整合面的发现及意义[J].地质通报,2004(5-6)
[42]  朱大岗;孟宪刚;邵兆刚.西藏阿里札达盆地上新世-早更新世沉积相及其构造演化特征[J].地质力学学报,2004(03)
[43]  尹安.喜马拉雅-青藏高原造山带地质演化[J].地球学报,2001(03)
[44]  郭铁鹰;梁定益;张宜智,西藏阿里地质,武汉:中国地质大学出版社,1991.

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