Institutional Repository of State Key Laboratory of Lithospheric Evolution
| Upper crustal structure beneath the Qin-Hang and Wuyishan metallogenic belts in Southeast China as revealed by a joint active and passive seismic experiment | |
| Zheng, Mengjie1,2; Xu, Tao1,3; Lu, Qingtian4; Lin, Jiyan1,2,5; Huang, Minfu1,2; Bai, Zhiming1; Deng, Yangfan6; Zhang, Yongqian4; Badal, Jose7 | |
| 2022-09-16 | |
| Source Publication | GEOPHYSICAL JOURNAL INTERNATIONAL
 |
| ISSN | 0956-540X |
| Volume | 232Issue:1Pages:190-200 |
| Abstract | Southeast China is one of the most important polymetallic metallogenic provinces in the world. However, distinct differences in the type and origin of the mineral deposits are present between the major metallogenic belts in this province. To deepen our knowledge of this regional metallogenic setting, investigate the factors controlling its metallogenic differences and explore the feasibility of active and passive seismic imaging, we performed a multibatch seismic experiment using active and passive sources with the help of 437 short-period seismographs deployed across the Qin-Hang and Wuyishan metallogenic belts in Southeast China. We resolved the S-wave velocity structure beneath the profile using ambient noise tomography and derived a Vp/Vs model by combining with a published P-wave model. A good correlation between the obtained seismic velocity models and geological observations is observed. The Proterozoic volcanic-sedimentary rock series and the Fuzhou-Yongfeng sedimentary basin are identified by low P- and S-wave velocities, high Vp/Vs ratios and low S-wave velocity perturbations. Within the core of the Wuyishan Metallogenic Belt, several narrow, elongated and low seismic velocity anomalies are considered to be signs of the nearby fault zones, and these anomalies provide reference information on the extension and pattern of these faults at depth. Combined with the geological and mineralogical evidence, we propose that theses faults function as ore-guiding structures and facilitate the formation of regionally representative mineral species and metal assemblages. |
| Keyword | Crustal imaging Seismic interferometry Crustal structure |
| DOI | 10.1093/gji/ggac337 |
| Funding Organization | 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 ; 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 ; 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 ; 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 |
| WOS Keyword | SURFACE-WAVE DISPERSION ; YANGTZE BLOCK ; MINERALIZATION ; TOMOGRAPHY ; CONSTRAINTS ; MAGMATISM ; INVERSION ; GRANITE ; TERRANE ; NOISE |
| Language | 英语 |
| Funding Project | National Natural Science Foundation of China[42130807] ; National Natural Science Foundation of China[41974048] ; National Key Research and Development Program of China[2016YFC0600201] |
| Funding Organization | 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 ; 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 ; 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 ; 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 |
| WOS Research Area | Geochemistry & Geophysics |
| WOS Subject | Geochemistry & Geophysics |
| WOS ID | WOS:000855482200005 |
| Publisher | OXFORD UNIV PRESS |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.iggcas.ac.cn/handle/132A11/106783 |
| Collection | 岩石圈演化国家重点实验室 |
| Corresponding Author | Xu, Tao |
| Affiliation | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China 4.Chinese Acad Geol Sci, Beijing 100037, Peoples R China 5.China Earthquake Adm, Geophys Explorat Ctr, Zhengzhou 450002, Peoples R China 6.Chinese Acad Sci, Guangzhou Inst Geochem, Staie Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China 7.Univ Zaragoza, Sci B, Phys Earth, Pedro Cerbuna 12, Zaragoza 50009, Spain |
| First Author Affilication | State Key Laboratory of Lithospheric Evolution |
| Corresponding Author Affilication | State Key Laboratory of Lithospheric Evolution |
| Recommended Citation GB/T 7714 | Zheng, Mengjie,Xu, Tao,Lu, Qingtian,et al. Upper crustal structure beneath the Qin-Hang and Wuyishan metallogenic belts in Southeast China as revealed by a joint active and passive seismic experiment[J]. GEOPHYSICAL JOURNAL INTERNATIONAL,2022,232(1):190-200. |
| APA | Zheng, Mengjie.,Xu, Tao.,Lu, Qingtian.,Lin, Jiyan.,Huang, Minfu.,...&Badal, Jose.(2022).Upper crustal structure beneath the Qin-Hang and Wuyishan metallogenic belts in Southeast China as revealed by a joint active and passive seismic experiment.GEOPHYSICAL JOURNAL INTERNATIONAL,232(1),190-200. |
| MLA | Zheng, Mengjie,et al."Upper crustal structure beneath the Qin-Hang and Wuyishan metallogenic belts in Southeast China as revealed by a joint active and passive seismic experiment".GEOPHYSICAL JOURNAL INTERNATIONAL 232.1(2022):190-200. |
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