2016年04月08日 星期五

高级专业技术职务

张进

张进  男,研究员

研究方向:新构造变形和油气盆地研究

Add:北京市西城区阜外百万庄大街26号地质研究所,100037

Tel: 010-68999687      E-mail:zhangjinem@sina.com


个人经历: 

1992-1996年期间于南京大学地球科学系构造地质专业学习,分别获得理学学士和硕士学位。

2002年毕业于中国地震局地质研究所固体地球物理专业,获理学博士学位,师从马宗晋院士。

2002-2004年,进入北京大学地球与空间科学学院博士后流动站,从事青藏高原东北缘新生代盆地的分析研究,合作导师何国琦教授。

承担项目: 

2000年以来先后参加了重点自然科学基金项目“中国大陆典型地区构造变形和现今构造应力场研究”、“准噶尔盆地构造分析与盆山耦合研究”、“中国岩石圈三维结构数据库-中国岩石圈三维构造格架与全国性图件数据子库专题”、“ 鄂尔多斯西缘构造沉积演化”、“雪峰山陆内造山带形成机制研究”、中国地质调查局国土资源大调查项目“中国北方及其邻区大型断裂活动历史及其对古构造-成矿格局的改造”、国家重点基础研究发展规划(973)“中亚造山带大陆动力学过程与成矿作用”等项目。2008年起,受国家自然基金和单位基本业务费项目资助分别就阿拉善东缘韧性剪切带、断裂面指向构造、青藏高原东北缘基底变形特征与机制以及西宁盆地属性及与青藏高原的关系展开研究。2008年-2009年受英国皇家学会的资助,赴英国Leicester大学地质学系,与D. Cunningham博士合作,针对青藏高原北缘变形和北山二叠系叠加褶皱的形成与构造背景进行了联合研究。2010年10月,进入中国地质科学院地质研究所工作,2011年被聘为研究员,开始参与国土资源部地质大调查项目“天山-兴蒙造山区基本构造格局的综合调查和研究”以及“中国主要陆块晚前寒武纪以来裂解重组过程的再造及其对成矿作用的制约”的研究。2012年获得自然科学基金项目的支持,从事阿拉善南缘下古生界地层物源以及属性的相关研究。

代表性论著: 

目前以第一作者或通讯作者发表文章46篇,其中SCI检索文章14篇,EI检索文章2篇,与他人合作60余篇。发表主要文章:
1. Zhang Jin,D.Cunningham,Cheng Hongyi. 2010. Sedimentary characteristics of Cenozoic strata in central-southern Ningxia, NW China: Implications for the evolution of the NE Qinghai–Tibetan Plateau. Journal of Asian Earth Sciences, 39, 740-759 (DOI:10.1016/j.jseaes.2010.05.008)
2. Zhang Jin, Li Jinyi, Li Yanfeng, Ma Zongjin. 2009. How did the Alxa Block respond to the Indo-Eurasian collision? International Journal of Earth Sciences, 98(6):1511-1528, DOI 10.1007/s00531-008-0404-2
3. Zhang Jin,D. Cunningham. 2013. Polyphase transpressional development of a NNE-striking basement-cored anticline in the Xining Basin, northeastern Qinghai–Tibetan Plateau. Geological Magazine, 150(4): 626-638, doi:10.1017/S0016756812000866
4. Zhang Jin, Li Jinyi, Ma Zongjin, REN Wenjun. 2011. Structural traces of secondary faults (fractures) along main faults and their reliability as kinematic indicators. Acta Geologica Sinica (English Edition), 85(5):1137-1149
5. Zhang Jin, Li Jinyi, Liu Jianfeng, Feng Qianwen. 2011. Detrital zircon U–Pb ages of Middle Ordovician flysch sandstones in the western ordos margin: New constraints on their provenances, and tectonic implications. Journal of Asian Earth Sciences, 42, 1030–1047
6. Zhang Jin, Dickson Cunningham. 2012. Kilometer-scale refolded folds caused by strike-slip reversal and intraplate shortening in the Beishan region, China. Tectonics, 31, TC3009, 1-19, doi:10.1029/2011TC003050
7.张进,李锦轶,刘建峰,李岩峰,曲军峰,冯乾文. 2012. 早古生代阿拉善地块与华北地块之间的关系:来自阿拉善东缘中奥陶统碎屑锆石的信息. 岩石学报,28(9):2912-2934
8.Zhang Jin, Li Jinyi, Xiao Wenxia, Feng Qianwen, Ma Zongjin. 2013. Multistage deformation in the northeastern segment of Jiangshao Fault (Suture) Belt: constraints for the relationship between the Yangtze Plate and the Cathaysia Old Land. Acta Geologica Sinica (English Edition), 87(4):948-978.
9.Zhang Jin, Li Jinyi, Xiao Wenxia, Li Yanfeng, Liu Jianfeng, Qu Junfeng. 2014. Mesozoic-Cenozoic multi-stage intraplate deformations in the Langshan region and their tectonic implication. Acta Geologica Sinica (English Edition), 88(1):78-102
10. Zhang Jin, Li Jinyi, Wenxia Xiao, Yannan Wang, Wenhua Qi. 2013. Kinematics and geochronology of multistage ductile deformation along the eastern Alxa block, NW China: New constraints on the relationship between the North China Plate and the Alxa block. Journal of Structural Geology, 57, 38-57. Doi: 10.1016/j.jsg.2013.10.002
11.Wang Yannan, Zhang Jin*, Qi Wenhua, Guo Shan. 2015. Exhumation History of the Xining Basin Since the Mesozoic and its Tectonic Implications. Acta Geologica Sinica (English Edition), 89(1):145-162.
12.Zhang Jin, Zhang Yiping, Xiao Wenxia, Wang Yannan. Linking the Alxa Terrane to the eastern Gondwana during the Early Paleozoic: Constraints from detrital zircon U–Pb ages and Cambrian sedimentary records. Gondwana Research, doi: 10.1016/j.gr.2014.09.012.
13.Zhang Jin, Wang Yannan, Zhang Beihang, Zhao Heng. 2015. Evolution of the NE Qinghai–Tibetan Plateau, constrained by the apatite fission track ages of the mountain ranges around the Xining Basin in NW China. Journal of Asian Earth Sciences, 97 :10–23, doi: http://dx.doi.org/10.1016/j.jseaes.2014.10.002.
14.Zhang Jin, Wang Yannan, Zhang Beihang, Zhao Heng. 2015. Tectonics of the Xining Basin in NWChina and its implications for the evolution of the NEQinghai-Tibetan Plateau. Basin Research, doi: 10.1111/bre.12104.
15. Wang Zongxiu, Zhang Jin, Li Tao, Xie Guoai and Ma Zongjin. Structural Analysis of the Multi-layer Detachment Folding in Eastern Sichuan Province. Acta Geologica Sinica 2010,84(3):497-514
16. Ma Zongjin,Wang Chien-Ying,Xu Jie,Nie Fengjun,Zhang Jin. Study on the transverse structures across Taiwan Strait. Science in China(Serie D),2002,45(12):1114-1126
17. Ma Zongjin,Ren Jinwei,Zhang Jin. Global tectonics and the plate motion obtained from the ITRF97 station velocity vectors. Science in China,(Ser.D),2003, 46 (3): 193-199
18. Yang, T.N., J.Y. Li, J. Zhang, K.J. Hou. 2011. The Altai-Mongolia terrane in the Central Asian Orogenic Belt (CAOB): A peri-Gondwana one ? Evidence from zircon U–Pb, Hf isotopes and REE abundance. Precambrian Research, 187, 79–98
19.Wang Zongxiu, Zhang Jin, Li Tao, Zhou Xingui, Ma Zongjin, Tang Liangjie, Xiao Weifeng,Yan Xili. 2012. Structural traps in detachment folds: a case study from the ‘comb-and trough-like” deformation zone/s, East Sichuan, China. Acta Geologica Sinica (English Edition), 86(4):828-841.
20.Xiao Qibin, Zhang Jin, Wang Jijun, Zhao Guoze, Tang Ji. 2012. Electrical resistivity structures between the Northern Qilian Mountains and Beishan Block, NW China, and tectonic Implications. Physics of the Earth and Planetary Interiors, 200-201, 92-104
21. Xiao Qibin, Zhang Jin, Wang Jijun. 2013. Electrical resistivity structures northeast of the Eastern Kunlun Fault in the Northeastern Tibet: tectonic implications. Tectonophysics 601:125–138, http://dx.doi.org/10.1016/j.tecto.2013.05.003.
22.Xiao Qibing, Shao Guihang, Liu-Zeng Jing, Oskin, Michael E., Zhang Jin, Zhao Guoze, Wang Jijun . 2015. Eastern termination of the Altyn Tagh Fault, western China: Constraints from a magnetotelluric survey. Journal of Geophysical Research - Solid Earth, DOI:10.1002/2014JB011363.