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The Southwestern area of Fujian Province in China contains a major metallogenic belt. There have been three major tectonic movements since the Late Paleozoic, and the thrusts here are the main mineral deposits. These occurred between the Early Carboniferous and Late Permian eras. Due to dramatic undulations in the surface and associated complex underground structures, a single geophysical method cannot provide reliable imaging results. This is largely due to difculties in data acquisition and processing. Seismic exploration provides one example. Using this method, raw shot gathers have a low signal-to-noise ratio because of the undulations in the topography. Furthermore, strong lateral velocity variation makes the migration process exceedingly difcult. This means that interpretations of the resulting refection seismic profle give rise to uncertainty. For this reason, two-dimensional refection seismology and controlled source audio-frequency magnetotel lurics (CSAMT) electromagnetic sounding techniques were performed. After initially completing conventional processing on the seismic refection data, subsequent pre-stack depth migration (PSDM) over the rugged topography yielded a much better image. It was able to identify thrust faults and magma intrusions. Then, using CSAMT, inversion was conducted with the same topography as the seismic refection. By combining the migrated seismic profle, inverted resistivity profle, and borehole data, a vertical geological model was constructed. This proved the existence of an overlapped thrust, and it also indicated the possible presence of deeper mineralization.
Wydawca
Czasopismo
Rocznik
Tom
Strony
1373--1385
Opis fizyczny
Bibliogr. 28 poz.
Twórcy
autor
- School of Geophysics and Information Technology, China University of Geosciences, Beijing 100083, China
autor
- School of Geophysics and Information Technology, China University of Geosciences, Beijing 100083, China
autor
- School of Geophysics and Information Technology, China University of Geosciences, Beijing 100083, China
autor
- School of Geophysics and Information Technology, China University of Geosciences, Beijing 100083, China
autor
- The Eighth Geology Team of Fujian Province, Fujian, China
autor
- Integrative Geosciences Center, University of Connecticut, Mansfeld, CT 06269, USA
Bibliografia
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- 9. Lin CH, Tan HD, Wang WW, Tong T, Peng M, Wang M, Zeng WH (2017) Three-dimensional inversion of CSAMT data in the presence of topography. Explor Geophys 49:253–267
- 10. Lin CH, Zhong S, Auken E, Cai H, Tan H, Peng M, Kong W (2018) The effects of 3D topography on controlled-source audio-frequency magnetotelluric responses. Geophysics 83:WB97–WB108
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Typ dokumentu
Bibliografia
Identyfikator YADDA
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