A complex magmatic system beneath the middle and northern Okinawa Trough: evidence from pyroxene characteristics | |
Liao, Renqiang1,3![]() | |
2017-11-01 | |
发表期刊 | GEOLOGICAL JOURNAL
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卷号 | 52期号:6页码:1059-1068 |
文章类型 | Article |
摘要 | The Okinawa Trough is an initial marginal back-arc basin. In this paper, we present a comparative study of pyroxenes in white and black pumice from the Okinawa Trough to explore the magmatic evolution of the region and the characteristics of the magmatic system. The results show two species of pyroxenes in the white pumice (clinopyroxene and orthopyroxene) but only one species in the black pumice (orthopyroxene). Many isomorphic replacements among the cations occurred during clinopyroxene crystallization. Clinopyroxene-melt thermobarometry yielded a temperature of 847-988 degrees C and a pressure of 2.73-7.42kbar, which vary considerably and correspond to a maximum depth of approximately 24km. All of the orthopyroxenes in both the white and black pumice crystallized at similar pressures ranging from 0.67 to 4.59kbar, which correspond to a maximum depth of approximately 15km. The clinopyroxenes crystallized mainly in the lower crust, whereas the orthopyroxenes formed at the boundary depth between the upper crust and the lower crust. The similarities in the pyroxene chemical compositions and the whole-rock characteristics between the two types of pumice indicate that both types of pumice are linked to the same magmatic system at depth. The pyroxenes crystallized from genetically related melts within a magmatic system that had undergone various degrees of differentiation. The physicochemical characteristics of the pyroxenes show that the magma chamber module changed during the crystallization process from clinopyroxenes to orthopyroxenes. This change most likely resulted from local characteristics of the near-surface structure. These observations support the model of a two-layered magma chamber' in the northern Okinawa Trough. Copyright (c) 2016 John Wiley & Sons, Ltd. |
关键词 | Okinawa Trough Pumice Pyroxene Magma System Magma Chamber Physical Process |
DOI | 10.1002/gj.2873 |
收录类别 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000414915500012 |
引用统计 | |
文献类型 | 期刊论文 |
版本 | 出版稿 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/143056 |
专题 | 海洋地质与环境重点实验室 |
作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Peoples R China 3.Univ Chinese Acad Sci, Beijing, Peoples R China 4.State Ocean Adm, Inst Oceanog 1, Key Lab Marine Sedimentary & Environm Geol, Qingdao, Peoples R China |
第一作者单位 | 中国科学院海洋研究所 |
推荐引用方式 GB/T 7714 | Liao, Renqiang,Huang, Peng,Hu, Ningjing. A complex magmatic system beneath the middle and northern Okinawa Trough: evidence from pyroxene characteristics[J]. GEOLOGICAL JOURNAL,2017,52(6):1059-1068. |
APA | Liao, Renqiang,Huang, Peng,&Hu, Ningjing.(2017).A complex magmatic system beneath the middle and northern Okinawa Trough: evidence from pyroxene characteristics.GEOLOGICAL JOURNAL,52(6),1059-1068. |
MLA | Liao, Renqiang,et al."A complex magmatic system beneath the middle and northern Okinawa Trough: evidence from pyroxene characteristics".GEOLOGICAL JOURNAL 52.6(2017):1059-1068. |
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文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
A complex magmatic s(497KB) | 期刊论文 | 出版稿 | 限制开放 | CC BY-NC-SA | 浏览 |
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