Mineral Chemistry Indicates the Petrogenesis of Rhyolite From The Southwestern Okinawa Trough

doi:10.1007/s11802-017-3344-2

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	Mineral Chemistry Indicates the Petrogenesis of Rhyolite From The Southwestern Okinawa Trough
	Chen Zuxing 1,3; Zeng Zhigang 1,2,3; Wang Xiaoyuan 1,2; Zhang Yuxiang 1,3; Yin Xuebo 1; Chen Shuai 1,2; Ma Yao1 ; Li Xiaohui 1,3; Qi Hanyan 1
刊名	JOURNAL OF OCEAN UNIVERSITY OF CHINA
	2017-12-01
卷号	16 期号:6 页码:1097-1108
关键词	Geothermobarometry Oxygen Fugacity Xenocrysts Magma Evolution Rhyolite Okinawa Trough
DOI	10.1007/s11802-017-3344-2
文献子类	Article
英文摘要	To reveal the petrogenesis of rhyolite from the southwestern Okinawa Trough, the mineral chemistry of plagioclase, orthopyroxene, amphibole, quartz and Fe-Ti oxide phenocrysts were analyzed using an electron microprobe, and in suit Sr and Ba contents of plagioclase analysed by LA-ICPMS were chosen for fingerprinting plagioclases of different provenances. Results indicate an overall homogeneous composition for each of the mineral phases except for plagioclase phenocrysts which have a wide range of composition (An=39 similar to 88). Plagioclase crystals characterized by An contents of >70 are not in equilibrium with their whole-rock compositions, and coarse-sieved plagioclase phenocryst interiors record high An contents (>70) and Sr/Ba ratios (>7), which are similar to the those of plagioclase crystals in basalt. Therefore, these crystals must have been introduced to the rhyolitic magma from a more mafic source. Equilibrium temperatures estimated using orthopyroxene-liquid, iron-titanium oxide, titanium-in-quartz and amphibole geothermometers show consistent values ranging from 792 to 869.. The equilibrium pressure calculated using amphibole compositions is close to 121 MPa which corresponds to an approximate depth of 4 km. The fO(2) conditions estimated from Fe-Ti oxides and amphiboles plot slightly above the NNO buffer, which indicates that the rock formed under more oxidized conditions. Our results suggests that petrogenesis of the rhyolite due to basaltic magma ascend with the high An and Sr/Ba plaigoclases from deep magma chamber into the shallow chamber where the fractional crystallization and crustal assimilation happened. It also indicates that a two-layer magma chamber structure may occur under the southwestern Okinawa Trough.
语种	英语
WOS记录号	WOS:000414791700019
内容类型	期刊论文
版本	出版稿
源URL	[http://ir.qdio.ac.cn/handle/337002/143041]
专题	海洋研究所_海洋地质与环境重点实验室
作者单位	1.Chinese Acad Sci, Key Lab Marine Geol & Environm, Inst Oceanol, Qingdao 266071, 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
推荐引用方式 GB/T 7714	Chen Zuxing,Zeng Zhigang,Wang Xiaoyuan,et al. Mineral Chemistry Indicates the Petrogenesis of Rhyolite From The Southwestern Okinawa Trough[J]. JOURNAL OF OCEAN UNIVERSITY OF CHINA,2017,16(6):1097-1108.
APA	Chen Zuxing.,Zeng Zhigang.,Wang Xiaoyuan.,Zhang Yuxiang.,Yin Xuebo.,...&Qi Hanyan.(2017).Mineral Chemistry Indicates the Petrogenesis of Rhyolite From The Southwestern Okinawa Trough.JOURNAL OF OCEAN UNIVERSITY OF CHINA,16(6),1097-1108.
MLA	Chen Zuxing,et al."Mineral Chemistry Indicates the Petrogenesis of Rhyolite From The Southwestern Okinawa Trough".JOURNAL OF OCEAN UNIVERSITY OF CHINA 16.6(2017):1097-1108.