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Late Mesozoic-Cenozoic decollement structure and its deep geological background in western Shandong, China

文献类型：期刊论文

作者Li, Li1; Zhong, Dalai2; Shi, Xiupeng1; Tang, Zibo1; Hu, Qiuyuan1; Xu, Yi2; Li, Zhiwei2
刊名PROGRESS IN NATURAL SCIENCE
出版日期2009-05-10
卷号19期号:5页码:603-613
关键词Decollement structure Late Mesozoic-Cenozoic Western Shandong Tancheng-Lujiang fault
ISSN号1002-0071
DOI10.1016/j.pnsc.2008.08.006
文献子类Article
英文摘要Data from seismic reflection profiles, drilling, stratigraphy, structural deformation studies and physical rock properties reveal the existence of decollement structures in both shallow and deep levels in western Shandong, China. The most outstanding shallow decollement structures occur along the regional unconformity surface between the Cambrian and Archean, and the disconformity surface between the Carboniferous and Ordovician. The decollement structure surface manifests as a fault zone with cataclastic rocks and asymmetrical folds. Some of the cataclastic rocks underwent dynamic metamorphism and hydrothermal alteration, including silicification, marbleization and specularite mineralization. Above the decollement structure, the bottom of the Cambrian might be missing or overprinted because of decollement. The striations, asymmetrical folds and boudinage structures indicate the direction of the main decollement to the NNW and NNE. A deep level decollement structure occurs at a depth of 12-22 km and up to 30 km distance to the south. The early Cretaceous and Eocene are two main periods of activity, with the Cretaceous decollement probably initiated by mantle upwelling derived from subduction and collision of the Yangtze Plate with the North China Plate along the Tancheng-Lujiang Fault in the late Triassicearly Jurassic. This circumstance implies a multidirection of subduction and collision of these two plates in the early late Mesozoic. (C) 2009 National Natural Science Foundation of China and Chinese Academy of Sciences. Published by Elsevier Limited and Science in China Press. All rights reserved.
WOS关键词SEISMIC TOMOGRAPHY ; UPPER-MANTLE ; LITHOSPHERE ; STRENGTH ; OROGEN ; SHEAR ; CRUST
WOS研究方向Materials Science ; Science & Technology - Other Topics
语种英语
WOS记录号WOS:000264659800011
出版者ELSEVIER SCIENCE INC
资助机构National Natural Science Foundation of China(40772132) ; National Natural Science Foundation of China(40772132) ; National Natural Science Foundation of China(40772132) ; National Natural Science Foundation of China(40772132) ; National Natural Science Foundation of China(40772132) ; National Natural Science Foundation of China(40772132) ; National Natural Science Foundation of China(40772132) ; National Natural Science Foundation of China(40772132)
源URL[http://ir.iggcas.ac.cn/handle/132A11/71384]  
专题中国科学院地质与地球物理研究所
通讯作者Li, Li
作者单位1.China Univ Petr, Inst Earth Resource & Informat, Dongying 257061, Shandong, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714		 Li, Li,Zhong, Dalai,Shi, Xiupeng,et al. Late Mesozoic-Cenozoic decollement structure and its deep geological background in western Shandong, China[J]. PROGRESS IN NATURAL SCIENCE,2009,19(5):603-613.
APA Li, Li.,Zhong, Dalai.,Shi, Xiupeng.,Tang, Zibo.,Hu, Qiuyuan.,...&Li, Zhiwei.(2009).Late Mesozoic-Cenozoic decollement structure and its deep geological background in western Shandong, China.PROGRESS IN NATURAL SCIENCE,19(5),603-613.
MLA Li, Li,et al."Late Mesozoic-Cenozoic decollement structure and its deep geological background in western Shandong, China".PROGRESS IN NATURAL SCIENCE 19.5(2009):603-613.

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来源：地质与地球物理研究所

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