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Factors controlling the geochemical differences between two types of rhyolites in the middle Okinawa Trough
Zhang, Yuxiang1,3; Zeng, Zhigang1,2,3; Wang, Xiaoyuan1,2; Chen, Shuai1; Yin, Xuebo1
2020-02-01
发表期刊GEOSCIENCES JOURNAL
ISSN1226-4806
卷号24期号:1页码:35-48
通讯作者Zeng, Zhigang(zgzeng@qdio.ac.cn)
摘要The origin of the felsic volcanic rocks in the Okinawa Trough (OT) remains uncertain. In the middle Okinawa Trough (MOT), two types of rhyolites (type 1 and type 2 rhyolites) have been recognized. Research on the diverse volcanic rocks should be prioritized to determine the magmatic origins of these rocks. Consequently, in this article, the geochemical differences and controlling factors for these two types of MOT rhyolites are systematically discussed. Type 2 rhyolites have higher Dy/Yb and Nb/Ta ratios than type 1 rhyolites, implying that the former might be influenced by a greater contribution of amphibole. Quantitative models suggest that type 1 rhyolites could have formed via the remelting of andesites when amphiboles remain in the source, whereas type 2 rhyolites could have formed without residual amphiboles. These two distinct melting models effectively explain most discrepancies between the major and trace element compositions of type 1 and 2 rhyolites. Additionally, the lower Mg# and delta Eu values of type 2 rhyolites are partly caused by significant magmatic differentiation. Quasi-linear correlations between some major oxides, trace element ratios and Sr-Nd isotopic ratios for type 2 rhyolites suggest that these rhyolites might have been contaminated by crustal rocks or melts with compositions similar to those of the Kueishantao (KST) andesites or the Middle Miocene upper crustal rocks of SW Japan. Therefore, isotopically enriched crustal materials likely remain in the OT crust.
关键词Okinawa Trough rhyolite amphibole crustal contamination magmatic differentiation
DOI10.1007/s12303-018-0084-2
收录类别SCI
语种英语
资助项目National Natural Science Foundation of China[41325021] ; National Natural Science Foundation of China[41306053] ; National Natural Science Foundation of China[41476044] ; National Natural Science Foundation of China[41706052] ; National Basic Research Program of China[2013CB429700] ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA11030302] ; International Partnership Program of Chinese Academy of Sciences[133137KYSB20170003] ; Special Fund for the Taishan Scholar Program of Shandong Province[ts201511061] ; AoShan Talents Program by Qingdao National Laboratory for Marine Science and Technology[2015ASKJ03] ; AoShan Talents Program by Qingdao National Laboratory for Marine Science and Technology[2016ASKJ13] ; AoShan Talents Program by Qingdao National Laboratory for Marine Science and Technology[2015ASTP-0S17] ; Innovative Talent Promotion Program[2012RA2191] ; Science and Technology Development Program of Shandong Province[2013GRC31502] ; National High Level Talent Special Support Program
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:000511879100003
出版者GEOLOGICAL SOCIETY KOREA
引用统计
被引频次:3[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/165269
专题海洋地质与环境重点实验室
通讯作者Zeng, Zhigang
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Seafloor Hydrothermal Act Lab, 7 Nanhai Rd, Qingdao 266071, Shandong, Peoples R China
2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao 266071, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
第一作者单位中国科学院海洋研究所
通讯作者单位中国科学院海洋研究所
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Zhang, Yuxiang,Zeng, Zhigang,Wang, Xiaoyuan,et al. Factors controlling the geochemical differences between two types of rhyolites in the middle Okinawa Trough[J]. GEOSCIENCES JOURNAL,2020,24(1):35-48.
APA Zhang, Yuxiang,Zeng, Zhigang,Wang, Xiaoyuan,Chen, Shuai,&Yin, Xuebo.(2020).Factors controlling the geochemical differences between two types of rhyolites in the middle Okinawa Trough.GEOSCIENCES JOURNAL,24(1),35-48.
MLA Zhang, Yuxiang,et al."Factors controlling the geochemical differences between two types of rhyolites in the middle Okinawa Trough".GEOSCIENCES JOURNAL 24.1(2020):35-48.
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