某典型剖面综合地质地球物理解释

杨辉; 王永涛; 吕金海; 黄卫宁

Volume 25 Issue 1

Jan. 2000

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Article Navigation > Earth Science > 2000 > 25(1): 88-92

YANG Hui, WANG Yongtao, Lü Jinhai, HUANG Weining, 2000. COMPREHENSIVE GEOLOGICAL-GEOPHYSICAL INTERPRETATION OF ONE TYPICAL SECTION. Earth Science, 25(1): 88-92.

Citation:

YANG Hui, WANG Yongtao, Lü Jinhai, HUANG Weining, 2000. COMPREHENSIVE GEOLOGICAL-GEOPHYSICAL INTERPRETATION OF ONE TYPICAL SECTION. Earth Science, 25(1): 88-92.

YANG Hui, WANG Yongtao, Lü Jinhai, HUANG Weining, 2000. COMPREHENSIVE GEOLOGICAL-GEOPHYSICAL INTERPRETATION OF ONE TYPICAL SECTION. Earth Science, 25(1): 88-92.

Citation:

YANG Hui, WANG Yongtao, Lü Jinhai, HUANG Weining, 2000. COMPREHENSIVE GEOLOGICAL-GEOPHYSICAL INTERPRETATION OF ONE TYPICAL SECTION. Earth Science, 25(1): 88-92.

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COMPREHENSIVE GEOLOGICAL-GEOPHYSICAL INTERPRETATION OF ONE TYPICAL SECTION

1.
Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
2.
Geophysical Research Institute, Bureau of Geophysical Prospecting, Zhuozhou 072751, China

Received Date: 1999-04-23
Publish Date: 2000-01-25

Abstract

Abstract

The comprehensive geological and geophysical interpretation of one measuring line in Basin C is applied to the determination of the distribution pattern of the Tertiary, the Cretaceous, the Jurassic and the Upper Triassic, a target stratum, and to the identification of several masses of igneous rocks, and several local structures. This section is classified as southern and northern parts along a reverse fault. A great difference arises between the southern and the northern parts of the section. The Upper Triassic in the northern part is thinner in thickness, shallower in burial depth, and weaker in deformation than that in the southern part. In conclusion, the deeper understanding of the comprehensive geological and geophysical interpretation may help us to obtain a better geological result.
- geology,
- geophysics,
- comprehensive interpretation

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References(3)

References

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