在 subduction 开始上测试地质上可试验的假设
- ISSN号:1000-5641
- 期刊名称:《华东师范大学学报:自然科学版》
- 时间:0
- 分类:P731.2[天文地球—海洋科学] P618.130.2[天文地球—矿床学;天文地球—地质学]
- 作者机构:[1]Department of Earth Sciences, Durham University,Durham DH1 3LE, UK, [2]Institute of Oceanology, Chinese Academy of Sciences,Qingdao 266071, China, [3]Qingdao National Laboratory for Marine Science andTechnology (Marine Geology), Qingdao 266061, China, [4]College of Earth Sciences, Jilin University, Changchun 130061,China
- 相关基金:Acknowledgments This work was supported by National Natural Science Foundation of China (41130314, 91014003), Chinese Acad- emy of Sciences Innovation Grant (Y42217101L), Qingdao National Laboratory for Marine Science and Technology (2015ASKJ03) and Marine Geological Process and Environment (U 1606401). Discussion with Shuo Chen and Pu Sun was useful. We thank Professors Shuguang Song and Zhidan Zhao for careful reading of earlier version of this paper.
中文摘要:
<正>Niu et al.[1]recently show that the basement of the Chinese continental shelf(beneath East China Sea and South China Sea)is geologically unrelated to the continental lithosphere of eastern China,but is of exotic origin.This
英文摘要:
Niu et al. [1] recently show that the basement of the Chinese continental shelf (beneath East China Sea and South China Sea) is geologically unrelated to the continental lithosphere of eastern China, but is of exotic origin. This alien/exotic terrane of a sizeable mass with large compositional buoyancy (either an oceanic plateau or a micro continent) was transported along with the Pacific plate that spread in the course of NW direction and subducted beneath the eastern margin of the continental China in the Mesozoic.