东篱科研大数据发现系统（DRDS）

位置：成果数据库 > 期刊 > 期刊详情页

Calculation of Depth to Detachment and Its Significance in the Kuqa Depression

ISSN号：0371-5736
期刊名称：《地质论评》
时间：0
分类：P618.13[天文地球—矿床学;天文地球—地质学] P631.4[天文地球—地质矿产勘探;天文地球—地质学]
作者机构：[1]Key Laboratory of Education Ministry for Hydrocarbon Accumulation Mechanism, China University of Petroleum, Beijing 102249, China, [2]Basin ＆ Reservoir Research Center, China University of Petroleum, Beijing 102249, China, [3]Institute of Petroleum Exploration and Development, SINOPEC, Beijing 100083, China, [4]Research Institute of Tarim Oilfield, Korla, Xinjiang 840000, China
相关基金：This research was jointly funded by the National Natural Science Foundation of China （No.40472107, 40172076）, the Foundation of Key Laboratory of Education Ministry for Hydrocarbon Accumulation Mechanism （China University of Petroleum）（Grant No. 2003-02）, the National Major Fundamental Research and Development Project （2005CB422107, G1999043305） and the Tarim 0ilfield Company Project （Grant No.41004050009）. We would like to thank Professor Lu Xiuxiang, Associate Professors Chen Shuping and Wang Simin, Senior engineers Xie Huiwen, Wu Shixiang and Ma Yujie. Special thanks are also given to Lei Ganglin, Zhang Jingzhou, Liang Shunjun, Wu Chao and Ye Lin for their guidance in this research.

作者： Yu Yixin[1,2], Tang Liangjie[1,2], Yin Jinyin[3], Wang Qinghua[4], Yang Wenjing[4], Peng Gengxin[4]

关键词：结构模型, 早第三纪, 深度计算, 地震勘探, 油气勘探, Detachment, excess area, structural modeling, Kuqa depression

中文摘要：

到分开水平的深度是影响在褶层和戳带的结构的建模的质量的一个关键因素。有层次在 Kuqa 消沉开发了的几个分队。基于过量区域图，这份报纸主要在 Kuqa 消沉使深度的计算担心到分开。结果证明分开层次位于在改变地区的不同阶层，例如 Paleogene Kugeliemu 形成，古生代并且水晶的地下室。到分开水平的计算深度对测试结构的解释是否是合理的并且为定义没在地震侧面被认出的更深的分开层次的深度很有用。

英文摘要：

The depth to detachment level is a critical factor affecting the quality of structural modeling in fold and thrust belts. There are several detachment levels developed in the Kuqa depression. Based on the excess-area diagram, this paper concerns mainly the calculation of the depth to detachment in the Kuqa depression. The result demonstrates that the detachment levels are situated in different strata in varying zones, such as the Paleogene Kugeliemu Formation, the Paleozoic and the crystalline basement. The calculated depth to detachment level is very helpful for testing whether a structural interpretation is reasonable and for defining the depth of deeper detachment levels which were not discerned in seismic profiles.

同期刊论文项目