东营凹陷负反转构造样式及其运动学特征

阳怀忠; 任建业; 陆金波

Volume 34 Issue 3

May 2009

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YANG Huai-zhong, REN Jian-ye, LU Jin-bo, 2009. Tectonic Styles and Kinematic Characteristics of Negative Inversion Structure in Dongying Depression. Earth Science, 34(3): 493-501.

Citation:

YANG Huai-zhong, REN Jian-ye, LU Jin-bo, 2009. Tectonic Styles and Kinematic Characteristics of Negative Inversion Structure in Dongying Depression. Earth Science, 34(3): 493-501.

YANG Huai-zhong, REN Jian-ye, LU Jin-bo, 2009. Tectonic Styles and Kinematic Characteristics of Negative Inversion Structure in Dongying Depression. Earth Science, 34(3): 493-501.

Citation:

YANG Huai-zhong, REN Jian-ye, LU Jin-bo, 2009. Tectonic Styles and Kinematic Characteristics of Negative Inversion Structure in Dongying Depression. Earth Science, 34(3): 493-501.

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Tectonic Styles and Kinematic Characteristics of Negative Inversion Structure in Dongying Depression

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
College of Resources and Information, China University of Petroleum, Beijing 102249, China

Received Date: 2008-12-26
Publish Date: 2009-05-25

Abstract

Abstract

The strong negative inversion structure in Mesozoic-Cenozoic is a prominent characteristic during the tectonic evolution of Dongying depression.In order to understand the significance of the negative inversion structure in the process of Mesozoic-Cenozoic basin formation in Dongying depression, this paper describes in detail the geometry styles of negative inversion structures in Dongying depression on the basis of the interpretation of the new high resolution 3D seismic profiles.And by utilizing the methods of calculating the fault activity velocity, negative inversion ratio, and displacement-distance curve, the authors quantitatively analyse the kinematic characteristics of the negative inversion structures in Dongying depression.The result indicates that in the Dongying depression, the extension basins developed in J₃-K₁ and Ek-Es₄ stages were mainly controlled by the negative inversion of the thrust faults formed in Indo-Chinese epoch.The total negative inversion ratio is 3.367-8.3, and the ratio in J₃-K₁ stage is 1.388-3.904.The negative inversion structures accomplished ultimately in the Es₃-Es₂ stage.The distribution of the negative inversion ratios indicates an increase in deformational degree from SW to NE in the whole region.The research of negative inversion structures in Dongying depression has important theoretic and practical significance in the exploration of the deep hydrocarbon reservoirs.
- Dongying depression,
- negative inversion structure,
- tectonic style,
- quantitative analysis

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References(46)

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Tectonic Styles and Kinematic Characteristics of Negative Inversion Structure in Dongying Depression

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