Lithosphere architecture and geodynamic model of Middle and Lower Reaches of Yangtze Metallogenic Belt: A review from SinoProbe | |
Lu QingTian1; Dung ShuWen2; Shi DaNian1; Tang JingTian3; Jiang GuoMing4; Zhang YongQian1; Xu Tao5; SinoProbe-03-CJ Group | |
刊名 | ACTA PETROLOGICA SINICA
![]() |
2014-04-01 | |
卷号 | 30期号:4页码:889-906 |
关键词 | Middle and Lower Yangtze Metallogenic Belt Teleseismic tomography Deep reflection seismic Intro-continental subduction Lithosphere delamination Geodynamic model |
ISSN号 | 1000-0569 |
文献子类 | Article |
英文摘要 | The lithosphere structure and deep processes are keys to understanding the formation of ore-district and metallogenic province. Lithosphere-scale process could create big footprints or signatures which can be observed by geophysics methods. To better understand the deep dynamic of the major metallogenic province, the authors has conducted an integrated deep exploration across Middle and Lower Reaches of Yangtze Metallogenic Belt (YMB) in eastern China, these included broadband seismic, deep reflection seismic, wide-angle reflection seismic and magnetotelluric sounding. The findings based on the data processing and inversion of these integrated geophysical exploration include: (1) Lower velocity body at the top of upper mantle and a SW dipping high velocity body with center depth at 300km, were imaged by teleseismic tomography beneath YMB; (2) S-wave receive function evidence the thinning of the lithosphere beneath the YMB to 50 similar to 70km; and SKS, SKKS shear wave splitting results show NE parallel fast-wave polarization direction which parallel with the regional tectonic lineament; (3) The reflection seismic data reveals strong NW-SE upper crustal contraction deformation, characterized as tight fold, thrust fault and nappe. The "crocodile" reflection structures are found beneath the Ningwu volcanic basin, Changjiang deep fault and Tan-Lu fault, indicating the decoupled deformation process of the upper and lower crust. Overall, the seismic data show evidence for an introcontinental orogen with lower crust and upper mantle subduction and imbrication; (4) Refraction seismic and MT data provide velocity and resistivity distribution across the YMB, and show a general agreement with the tectonic units. Based on the results of the integrated geophysical exploration, combining with the recent geochemistry results, a geodynamic model is proposed for the YMB. The model suggests that Middle and Later Jurassic introcontinental subduction, lithosphere delamination, mantle-derived magmatic underplating and MASH process are responsible for the formation of this world-class metallogenic belt. |
WOS关键词 | SURROUNDING AREAS CONSTRAINTS ; CRUSTAL STRUCTURE BENEATH ; SOURCE SEISMIC EXPERIMENT ; LOWER CONTINENTAL-CRUST ; CU-AU MINERALIZATION ; LU FAULT ZONE ; EASTERN CHINA ; SOUTH CHINA ; TAN-LU ; SOUTHEASTERN CHINA |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | SCIENCE PRESS |
WOS记录号 | WOS:000335541600001 |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/86672] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Lu QingTian |
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 Geol Sci, Beijing 100037, Peoples R China 3.Cent S Univ, Sch Geosci & Infophys, Key Lab Metallogen Predict Nonferrous Met, Minist Educ, Changsha 410083, Hunan, Peoples R China 4.China Univ Geosci, Sch Geophys & Informat Technol, Beijing 100083, Peoples R China 5.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China |
推荐引用方式 GB/T 7714 | Lu QingTian,Dung ShuWen,Shi DaNian,et al. Lithosphere architecture and geodynamic model of Middle and Lower Reaches of Yangtze Metallogenic Belt: A review from SinoProbe[J]. ACTA PETROLOGICA SINICA,2014,30(4):889-906. |
APA | Lu QingTian.,Dung ShuWen.,Shi DaNian.,Tang JingTian.,Jiang GuoMing.,...&SinoProbe-03-CJ Group.(2014).Lithosphere architecture and geodynamic model of Middle and Lower Reaches of Yangtze Metallogenic Belt: A review from SinoProbe.ACTA PETROLOGICA SINICA,30(4),889-906. |
MLA | Lu QingTian,et al."Lithosphere architecture and geodynamic model of Middle and Lower Reaches of Yangtze Metallogenic Belt: A review from SinoProbe".ACTA PETROLOGICA SINICA 30.4(2014):889-906. |
个性服务 |
查看访问统计 |
相关权益政策 |
暂无数据 |
收藏/分享 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。
修改评论