Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Bai‐Min Zhao"'
Publikováno v:
Journal of Asian Earth Sciences. 111:31-43
A series of drilling, dredge, and seismic investigations indicate that Mesozoic sediments exist in the South China Sea (SCS) which shows a bright prospect for oil and gas exploration. In order to study the distribution of Mesozoic strata and their re
Publikováno v:
Chinese Journal of Geophysics. 54:1138-1148
In order to assess the oil and gas resources potential of Pre-Cenozoic strata in the South China Sea (SCS), macro-distribution of Pre-Cenozoic residual basins is studied by using integrated geophysical methods. Based on the analysis of rock physical
Publikováno v:
Chinese Journal of Geophysics. 54:1169-1177
Bohai bay basin is the center area of the destruction of North China Craton (NCC). The deep structure study of the Bohai Sea plays a key role in understanding the scope and dynamic process of the destruction of NCC. In this paper, we studied the crus
Investigation of igneous rocks in Huanghua depression, North China, from magnetic derivative methods
Publikováno v:
Journal of Geophysics and Engineering. 8:74-82
The igneous rock study plays an important role in understanding the tectonic evolution of sedimentary basins. The distribution of igneous rocks is one of the basic aspects in the igneous rock study. Based on the magnetic susceptibility contrast of ig
Autor:
Wei‐Wei Jiang, Li‐Li Zhang, Shu‐Qin Yuan, Yi Xu, Tianyao Hao, Bai‐Min Zhao, Jun Li, Bei‐Bei Wang, Li‐Hong Zhou, Ya Xu
Publikováno v:
Chinese Journal of Geophysics. 51:332-346
Using geophysical data to delimitate the macroscopic distribution of residual basins is one of the important techniques in residual basin oil/gas research. Taking Dagang area as an example this paper presents the method of integrated geophysical rese
Publikováno v:
Chinese Journal of Geophysics. 50:539-546
In this paper, the author introduces the method of separation of magnetic field step by step, which supposes the field arises from an equivalent unit-thickness layer, whose equivalent magnetization is variable, then the equivalent magnetization of th