Moho depth of the northern Vietnam and Gulf of Tonkin from 3D inverse interpretation of gravity anomaly data

被引:8
|
作者
Nguyen Nhu Trung [1 ,2 ]
Phan Thi Hong [3 ]
Bui Van Nam [1 ]
Nguyen Thi Thu Huong [1 ]
Tran Trong Lap [1 ]
机构
[1] VAST, Inst Marine Geol & Geophys, Hanoi, Vietnam
[2] Grad Univ Sci & Technol, VAST, Hanoi, Vietnam
[3] Hanoi Univ Geol & Min, Hanoi, Vietnam
关键词
Moho depth; Gulf of Tonkin; Red River fault; 3D gravity inverse; SOUTH-CHINA-SEA; RIVER SHEAR ZONE; RED RIVER; CONSTRAINTS; EXTENSION; YUNNAN; FIELD;
D O I
10.1088/1742-2140/aabf48
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
In this paper, the authors present the result of three-dimensional (3D) direct inversion of gravity data to determine the Moho depth along the Red River Fault (RRF) zone and adjacent areas in the land territory of Vietnam and the Gulf of Tonkin. The Moho depth was calculated by 3D Parker inversion supplemented with the gravity anomaly power density spectrum. The given Moho depth and the available teleseismic and magnetotelluric Moho depth are well matched. A structural Moho map of the study region was constructed from the interpretation results. The Moho surface was uplifted along the RRF zone. The shallowest Moho depth was determined in the Red River Basin (RRB), where it ranges from 22 +/- 1.0 km to 24 +/- 1.0 km in the depocenter of the RRB in the Gulf of Tonkin to 27 +/- 1.0 km to 29 +/- 1.0 km in the Red River Delta. It is 29 +/- 1.0 km to 32 +/- 1.0 km from Vietri to Laocai provinces. The deepest Moho depth was found in the northwesternmost and northernmost land territory of Vietnam, where it ranges from 33 +/- 1.0 km to 35.8 +/- 1.0 km. A percentage of the Earth's crustal compensation is also investigated. The obtained crustal thickness and compensation state are useful for their implications regarding the geodynamics and tectonics of the RRF and surrounding region.
引用
收藏
页码:1651 / 1662
页数:12
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