Joint development and paleostress field in Mesozoic strata of the southeastern Ordos Basin
文献类型：期刊论文
| 作者 | Jiang Lin1,2; Wang QingChen1; Wang XiangZeng3; Jiang ChengFu3; Zhang LiXia3; Xue ZhenHua1,2; Chu Yang1 |
| 刊名 | ACTA PETROLOGICA SINICA
 |
| 出版日期 | 2013-05-01 |
| 卷号 | 29期号:5页码:1774-1790 |
| 关键词 | Ordos Basin Mesozoic Orthogonal joint system Paleostress field |
| ISSN号 | 1000-0569 |
| 文献子类 | Article |
| 英文摘要 | Six trends of joint sets (E-W, N-S, ENE-WSW, NNW-SSE, WNW-ESE, NNE-SSW) and three groups of orthogonal joints systems (EW and SN, ENE-WSW and NNW-SSE, NWW-SEE and NNE-SSW) are recognized in the Mesozoic strata within the southeastern Ordos Basin. The orthogonal joint systems developed in three sequences; D1 with E-W and N-S trening joints, D2 with SEE-NWW and NNE-SSW trending joints, and D3 with ENE-WSW and NNW-SSE trending joints. The fracture spacing index (FSI) of three sets of joints (E-W, N-S, ENE-WSW) shows that joint development is controlled by mechanical layer thickness, as well as regional stress. The fracture spacing ratio (FSR) values of the joint sets (E-W, N-S, ENE-WSW) indicate regional variation in joint development. Furthermore, the FSR values of the dominant joint sets (E-W) exceeds the critical ratio of spacing/height, while FSR value of subdominate joint sets (N-S) are less than the critical value, as indicating that the orthogonal joint system of E-W and N-S trending joint sets developed earlier than others. Three sets of orthogonal joints systems correspond to three paleostress fields respectively. (1) The Ordos Basin experienced E-W compression in the Late Jurassic, and the first phase of orthogonal joints systems with the E-W and N-S trending joint sets developed resulting from the far-field effect of NW-directed subduction of the Pacific plate; (2) In the Late Cretaceous, the second phase of orthogonal joints system with WNW-ESE and NNE-SSW trending joint sets developed as a result of the continuing subduction of the Pacific plate; (3) From the Late Cretaceous to Cenozoic, the third phase of orthogonal joints system with ENE-WSW and NNW-SSE trending joint sets developed in responding to the NE-SW compression as a far-field effect of the Indian plate collision to the Eurasian plate. |
| WOS关键词 | NORTH CHINA BLOCK ; EXTENSIONAL TECTONICS ; LAYERED ROCKS ; STRESS-FIELD ; CROSS JOINTS ; NE CHINA ; CONTEMPORARY STRESS ; APPALACHIAN PLATEAU ; NEOTECTONIC JOINTS ; SEDIMENTARY-ROCKS |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000321226200022 |
| 出版者 | SCIENCE PRESS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/87436]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Jiang Lin |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.Shaanxi Yanchang Petr Grp CO LTD, Xian 710075, Peoples R China |
| 推荐引用方式 GB/T 7714 | Jiang Lin,Wang QingChen,Wang XiangZeng,et al. Joint development and paleostress field in Mesozoic strata of the southeastern Ordos Basin[J]. ACTA PETROLOGICA SINICA,2013,29(5):1774-1790. |
| APA | Jiang Lin.,Wang QingChen.,Wang XiangZeng.,Jiang ChengFu.,Zhang LiXia.,...&Chu Yang.(2013).Joint development and paleostress field in Mesozoic strata of the southeastern Ordos Basin.ACTA PETROLOGICA SINICA,29(5),1774-1790. |
| MLA | Jiang Lin,et al."Joint development and paleostress field in Mesozoic strata of the southeastern Ordos Basin".ACTA PETROLOGICA SINICA 29.5(2013):1774-1790. |
入库方式： OAI收割
来源：地质与地球物理研究所
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