Potential link between antigorite dehydration and shallow intermediate-depth earthquakes in hot subduction zones
文献类型：期刊论文
| 作者 | Shao, Tongbin3,4,5; Song, Maoshuang3,5; Ma, Xi4; Ding, Xing3,5; Liu, Shirong2; Zhou, Yongsheng4; Wu, Jie1; Wang, Xiaoning3,5; Li, Jianfeng3,5 |
| 刊名 | AMERICAN MINERALOGIST
 |
| 出版日期 | 2023 |
| 卷号 | 108期号:1页码:127-139 |
| 关键词 | HIGH-PRESSURE SERPENTINE DEHYDRATION HIGH-TEMPERATURE FLUID-PRESSURE KINETICS WATER DEFORMATION MANTLE SEISMICITY STABILITY |
| ISSN号 | 0003-004X |
| DOI | 10.2138/am-2022-8271 |
| 英文摘要 | The distribution of earthquakes at intermediate depths corresponding to pressures ?6 and 4.69 × 10?5 m3fluidmrock-3 s-1, respectively, which are much faster than those of mantle deformation, causing high fluid pressure in hot subducting mantle but not necessarily embrittlement. We emphasize the role of kinetic mechanisms in controlling the grain sizes of reaction products, which likely determine the mechanical behavior of serpentinized fault zones. Superplasticity or velocity weakening of fine-grained forsterite and velocity weakening of antigorite by water and/or talc may be responsible for earthquake nucleation and propagation in a heterogeneous system, which can be either dehydration products within a serpentinized fault zone or the mixture of antigorite fault and surrounding peridotite in hot subduction zones ( ? 2023 De Gruyter. All rights reserved. |
| WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
| 语种 | 英语 |
| WOS记录号 | WOS:000923813700011 |
| 源URL | [http://ir.gig.ac.cn/handle/344008/80297]  |
| 专题 | 同位素地球化学国家重点实验室 |
| 作者单位 | 1.College of Earth Sciences, Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration, Guilin University of Technology, Guilin; 541004, China 2.State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang; 550003, China 3.CAS Center for Excellence in Deep Earth Science, Guangzhou; 510640, China 4.State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing; 100029, China 5.State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou; 510640, China |
| 推荐引用方式 GB/T 7714 | Shao, Tongbin,Song, Maoshuang,Ma, Xi,et al. Potential link between antigorite dehydration and shallow intermediate-depth earthquakes in hot subduction zones[J]. AMERICAN MINERALOGIST,2023,108(1):127-139. |
| APA | Shao, Tongbin.,Song, Maoshuang.,Ma, Xi.,Ding, Xing.,Liu, Shirong.,...&Li, Jianfeng.(2023).Potential link between antigorite dehydration and shallow intermediate-depth earthquakes in hot subduction zones.AMERICAN MINERALOGIST,108(1),127-139. |
| MLA | Shao, Tongbin,et al."Potential link between antigorite dehydration and shallow intermediate-depth earthquakes in hot subduction zones".AMERICAN MINERALOGIST 108.1(2023):127-139. |
入库方式： OAI收割
来源：广州地球化学研究所
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