中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The lower crust conductor from Nanjing (Ning) - Wuhu (Wu) area in the Middle and Lower Reaches of Yangtze River: Preliminary results from 3D inversion of magnetotelluric data

文献类型:期刊论文

作者Zhang, Kun1,2; Lu, Qingtian1; Yan, Jiayong1
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2015-04-01
卷号101页码:20-29
关键词Deep Conductivity Structure 3d Inversion Magnetotelluric
DOI10.1016/j.jseaes.2015.01.007
文献子类Article
英文摘要A series of long magnetotelluric (MT) profiles across the Ning-Wu Basin and adjacent areas were deployed by SINOPROBE-03 deep drilling project and 3D exploration technology integration project from 2011 to 2012. Broadband MT data were acquired at 349 sites with a frequency range of 0.0003-320 Hz. Preliminary three-dimensional inversion of this dataset revealed a striking feature of extensive areas with high conductivity in the lower crust. Combined with regional heat flow results, relative water content was calculated from the resistivity model, suggesting that a 'local melt' or 'shear fracture' may exist in the lower crust, which is likely to be hot and weak. The location of the upper mantle uplift and Yangtze River deep fault were hence inferred from the electrical properties. Furthermore, the Yangtze River Fault may be composed of a number of minor faults. (C) 2015 Elsevier Ltd. All rights reserved.
WOS关键词METALLOGENIC BELT ; CONJUGATE GRADIENTS ; TECTONIC HISTORY ; CHINA ; DEFORMATION ; DYNAMICS ; MANTLE ; TENSOR ; MO ; AU
WOS研究方向Geology
语种英语
WOS记录号WOS:000352042700003
资助机构(12120114053301) ; (12120114053301) ; (12120114053301) ; (12120114053301) ; (K1318) ; (K1318) ; (K1318) ; (K1318) ; (2011BAB04B01) ; (2011BAB04B01) ; (2011BAB04B01) ; (2011BAB04B01) ; (41304100) ; (41304100) ; (41304100) ; (41304100) ; (12120114053301) ; (12120114053301) ; (12120114053301) ; (12120114053301) ; (K1318) ; (K1318) ; (K1318) ; (K1318) ; (2011BAB04B01) ; (2011BAB04B01) ; (2011BAB04B01) ; (2011BAB04B01) ; (41304100) ; (41304100) ; (41304100) ; (41304100)
源URL[http://ir.iggcas.ac.cn/handle/132A11/62573]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
作者单位1.Chinese Acad Geol Sci, Inst Mineral Resources, MLR Key Lab Metallogeny & Mineral Assessment, Beijing 100037, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
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Zhang, Kun,Lu, Qingtian,Yan, Jiayong. The lower crust conductor from Nanjing (Ning) - Wuhu (Wu) area in the Middle and Lower Reaches of Yangtze River: Preliminary results from 3D inversion of magnetotelluric data[J]. JOURNAL OF ASIAN EARTH SCIENCES,2015,101:20-29.
APA Zhang, Kun,Lu, Qingtian,&Yan, Jiayong.(2015).The lower crust conductor from Nanjing (Ning) - Wuhu (Wu) area in the Middle and Lower Reaches of Yangtze River: Preliminary results from 3D inversion of magnetotelluric data.JOURNAL OF ASIAN EARTH SCIENCES,101,20-29.
MLA Zhang, Kun,et al."The lower crust conductor from Nanjing (Ning) - Wuhu (Wu) area in the Middle and Lower Reaches of Yangtze River: Preliminary results from 3D inversion of magnetotelluric data".JOURNAL OF ASIAN EARTH SCIENCES 101(2015):20-29.

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来源:地质与地球物理研究所

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