Research on fine crustal structure using deep seismic reflection profile in Beijing region
文献类型：期刊论文
| 作者 | Liu Bao-Jin1,2; Hu Ping1,3; Meng Yong-Qi3; Feng Shao-Ying2; Shi Jin-Hu2; Ji Ji-Fa2 |
| 刊名 | CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
 |
| 出版日期 | 2009-09-01 |
| 卷号 | 52期号:9页码:2264-2272 |
| 关键词 | Beijing region Deep seismic reflection profile Crustal fine structure Sanhe-Pinggu earthquake area Deep-shallow tectonic feature |
| ISSN号 | 0001-5733 |
| DOI | 10.3969/j.issn.0001-5733.2009.09.010 |
| 文献子类 | Article |
| 英文摘要 | The fine crustal structure and deep-shallow tectonic features of Beijing region are explored by using a 100 km long, NW-trending deep seismic reflection profile. This profile passed through the Sanhe-Pinggu earthquake (M8.0) area and main faults in Beijing region. The results show that the crust beneath the investigated area is divided into upper and lower crust by a strong reflective zone at about 6 similar to 7 s TWT. The thickness of the upper and lower crust is about 1821 km and 13 similar to 15 km, respectively. There are rich reflective layers and clear structural patterns above 3 similar to 4 s TWT as well as obviously different structural features along the profile. In the western region of Sanhe-Pinggu earthquake area, the stacked deep seismic reflection section shows 2 similar to 3 groups of strong reflective layers and a series of basement faults. In the eastern region of Sanhe-Pinggu earthquake area, there is a set of dense, westward-dipping, reflective strata with relatively strong energy, which have the typical characteristics of sedimentary basin. The largest depth of the sedimentary basin is about 8 similar to 9 km. The crustal deep fault revealed by deep seismic reflection profile has a steep fault plane, and it cuts and disturbs the lower crust and crust-mantle transitional zone. This deep fault extends upwards into the upper crust, and joins the crustal deep structure to the shallow fault. The profile reveals that the deep-shallow fault system, represents the major deep-shallow tectonic feature in the study region. |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| WOS记录号 | WOS:000270377100010 |
| 出版者 | SCIENCE PRESS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/71162]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Liu Bao-Jin |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.China Earthquake Adm, Geophys Prospecting Ctr, Zhengzhou 450002, Peoples R China 3.Earthquake Adm Beijing City, Beijing 100080, Peoples R China |
| 推荐引用方式 GB/T 7714 | Liu Bao-Jin,Hu Ping,Meng Yong-Qi,et al. Research on fine crustal structure using deep seismic reflection profile in Beijing region[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2009,52(9):2264-2272. |
| APA | Liu Bao-Jin,Hu Ping,Meng Yong-Qi,Feng Shao-Ying,Shi Jin-Hu,&Ji Ji-Fa.(2009).Research on fine crustal structure using deep seismic reflection profile in Beijing region.CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,52(9),2264-2272. |
| MLA | Liu Bao-Jin,et al."Research on fine crustal structure using deep seismic reflection profile in Beijing region".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 52.9(2009):2264-2272. |
入库方式： OAI收割
来源：地质与地球物理研究所
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