中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The Crustal and Uppermost Mantle Vs Structure of the Middle and Lower Reaches of the Yangtze River Metallogenic Belt: Implications for Metallogenic Process

文献类型:期刊论文

作者Zhang, Yongqian1,2; Lu, Qingtian1,2; Shi, Danian1,2; Yang, Yingjie3,6; Afonso, Juan Carlos4,6; Xu, Yao1,2; Yan, Jiayong1,2; Gong, Xuejing1,2; Xu, Tao5
刊名JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
出版日期2023-08-01
卷号128期号:8页码:14
ISSN号2169-9313
关键词middle and lower reaches of the Yangtze River metallogenic belt ambient noise tomography shear wave velocity metallogenic model
DOI10.1029/2023JB026817
英文摘要The Middle and Lower Reaches of the Yangtze River metallogenic belt (MLYMB) is one of the most important Fe-Cu polymetallic belts in China. However, the mechanism and deep geodynamical process for the formation of this belt are still controversial. Here, we obtain the crustal and the uppermost mantle structures using ambient noise data from a dense seismic profile. A low velocity zone is revealed beneath the Moho of MLYMB, interpreted as the source of the deep mineralization materials. In addition, a low velocity layer (LVL) and a high velocity layer (HVL) are observed in the crust of the southern segment of the profile. The LVL is interpreted as a tectonic detachment layer between the upper and the lower crust, and the HVL is interpreted as the aggregation zone for mineralizing melts or crystallized magma chambers. Based on the observed velocity features, we propose a three-stage model for the formation of ore deposits in MLYMB. Our model suggests that an upwelling of asthenosphere triggered by the delamination of a previously thickened lithosphere leads to the partial melting of upper mantle rocks, which eventually ponders under the Moho. The magma then infiltrates through the ductile lower crust and reaches a depth of similar to 7-13 km, forming a minerals-enriched magma chamber. Minerals-rich hot fluids originating from the magma chamber continue to move upward along the pre-existent faults and the minerals finally precipitate in dense veinlets when reaching shallow depths, forming the ore deposits in and around the MLYMB. Plain Language Summary The formation of large-scale mineral deposits is closely related to the lithosphere structure. The Middle and Lower Reaches of the Yangtze River metallogenic belt (MLYMB) is an ideal place to study the mineral system, as it is one of the most important Fe-Cu polymetallic metallogenic belts in Eastern China and contains more than 200 ore deposits. Yet the mechanism and deep geodynamical process for the formation of this belt are still controversial. In this study, we construct a high-resolution seismic model of the crust and the uppermost mantle using ambient noise data from a dense seismic profile. Our result reveals velocity features closely related to the metallogenic process in this region. Based on the observed velocity features, we propose a three-stage model for the formation of the ore deposits in MLYMB, which is of great importance for the development of "mineral system" approaches to the exploration of minerals worldwide.
WOS关键词WAVE VELOCITY STRUCTURE ; SURROUNDING AREAS CONSTRAINTS ; SHOSHONITIC IGNEOUS ROCKS ; SOURCE SEISMIC EXPERIMENT ; AMBIENT NOISE ; CONTINENTAL-CRUST ; STRUCTURE BENEATH ; SOUTH CHINA ; MINERAL SYSTEMS ; VOLCANIC-BASIN
资助项目National Natural Science Foundation of China[42074099] ; National Natural Science Foundation of China[42074069] ; National Natural Science Foundation of China[41574082] ; National Key Research and Development Program of China[2016YFC0600201] ; China Geological Survey Project[DD20221643] ; China Geological Survey Project[DD20190012]
WOS研究方向Geochemistry & Geophysics
语种英语
出版者AMER GEOPHYSICAL UNION
WOS记录号WOS:001042083600001
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; China Geological Survey Project ; China Geological Survey Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; China Geological Survey Project ; China Geological Survey Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; China Geological Survey Project ; China Geological Survey Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; China Geological Survey Project ; China Geological Survey Project
源URL[http://ir.iggcas.ac.cn/handle/132A11/111363]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Lu, Qingtian; Yang, Yingjie
作者单位1.China Geol Survey, China Deep Explorat Ctr, SinoProbe Ctr, Beijing, Peoples R China
2.Chinese Acad Geol Sci, Beijing, Peoples R China
3.Southern Univ Sci & Technol, Guangdong Prov Key Lab Geophys High Resolut Imagin, Shenzhen, Peoples R China
4.Univ Twente, Fac Geoinformat Sci & Earth Observat ITC, Enschede, Netherlands
5.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
6.Southern Univ Sci & Technol, Dept Earth & Space Sci, Shenzhen, Peoples R China
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Zhang, Yongqian,Lu, Qingtian,Shi, Danian,et al. The Crustal and Uppermost Mantle Vs Structure of the Middle and Lower Reaches of the Yangtze River Metallogenic Belt: Implications for Metallogenic Process[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2023,128(8):14.
APA Zhang, Yongqian.,Lu, Qingtian.,Shi, Danian.,Yang, Yingjie.,Afonso, Juan Carlos.,...&Xu, Tao.(2023).The Crustal and Uppermost Mantle Vs Structure of the Middle and Lower Reaches of the Yangtze River Metallogenic Belt: Implications for Metallogenic Process.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,128(8),14.
MLA Zhang, Yongqian,et al."The Crustal and Uppermost Mantle Vs Structure of the Middle and Lower Reaches of the Yangtze River Metallogenic Belt: Implications for Metallogenic Process".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 128.8(2023):14.

入库方式: OAI收割

来源:地质与地球物理研究所

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