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Volume 22 Issue 3
Jun.  2011
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倪金龙, 郭颖, 王智敏, 刘俊来, 林玉祥, 李月. Tectonics and Mechanisms of Uplift in the Central Uplift Belt of the Huimin Depression. Journal of Earth Science, 2011, 22(3). doi: 10.1007/s12583-011-0183-8
Citation: 倪金龙, 郭颖, 王智敏, 刘俊来, 林玉祥, 李月. Tectonics and Mechanisms of Uplift in the Central Uplift Belt of the Huimin Depression. Journal of Earth Science, 2011, 22(3). doi: 10.1007/s12583-011-0183-8

Tectonics and Mechanisms of Uplift in the Central Uplift Belt of the Huimin Depression

doi: 10.1007/s12583-011-0183-8
  • Received Date: 2018-07-15
  • Rev Recd Date: 2018-07-15
  • Publish Date: 2018-07-15
  • The Huimin (惠民) depression is a third-level tectonic element of the Bohai (渤海) Bay basin in eastern China. The central uplift belt is the most important oil and gas accumulation zone in the depression, but the lack of adequate geological studies in the area has greatly hindered exploration and development. In this article, using seismic data, fracture mechanics, and a combination of data on fault growth indices and fault throws, we present an analysis of tectonic activity in the central uplift belt and adjacent regions. The amount of extension is calculated along balanced N-S cross-sections, along with the thickness of strata eroded from the fourth, third, and second members of the Shahejie (沙河街) Formation (Es4–Es2) in the uplift belt, by analyzing porosity and stratigraphic correlations...
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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Tectonics and Mechanisms of Uplift in the Central Uplift Belt of the Huimin Depression

doi: 10.1007/s12583-011-0183-8

Abstract: The Huimin (惠民) depression is a third-level tectonic element of the Bohai (渤海) Bay basin in eastern China. The central uplift belt is the most important oil and gas accumulation zone in the depression, but the lack of adequate geological studies in the area has greatly hindered exploration and development. In this article, using seismic data, fracture mechanics, and a combination of data on fault growth indices and fault throws, we present an analysis of tectonic activity in the central uplift belt and adjacent regions. The amount of extension is calculated along balanced N-S cross-sections, along with the thickness of strata eroded from the fourth, third, and second members of the Shahejie (沙河街) Formation (Es4–Es2) in the uplift belt, by analyzing porosity and stratigraphic correlations...

倪金龙, 郭颖, 王智敏, 刘俊来, 林玉祥, 李月. Tectonics and Mechanisms of Uplift in the Central Uplift Belt of the Huimin Depression. Journal of Earth Science, 2011, 22(3). doi: 10.1007/s12583-011-0183-8
Citation: 倪金龙, 郭颖, 王智敏, 刘俊来, 林玉祥, 李月. Tectonics and Mechanisms of Uplift in the Central Uplift Belt of the Huimin Depression. Journal of Earth Science, 2011, 22(3). doi: 10.1007/s12583-011-0183-8

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