The magma plumbing system in the Mariana Trough back-arc basin at 18 degrees N

doi:10.1016/j.jmarsys.2016.11.008

CORC > 深海科学与工程研究所 > 中国科学院深海科学与工程研究所 > 深海科学研究部 > 深海地质与地球化学研究室

	The magma plumbing system in the Mariana Trough back-arc basin at 18 degrees N
	Liu, Bo 1,5; Lai, Zhiqing(Minist Educ, Key Lab Submarine Geosci & Prospecting Tech, Qingdao 266100, Peoples R China); Han, Zongzhu 1,5; Zhao, Guangtao(Minist Educ, Key Lab Submarine Geosci & Prospecting Tech, Qingdao 266100, Peoples R China); Lai, Zhiqing 1,5; Zhao, Guangtao 1,5; Li, Min 3; Huang, Bo 2; Tian, Liyan4 ; Bu, Xuejiao 1,5
刊名	JOURNAL OF MARINE SYSTEMS
	2018-04-01
卷号	180 页码:132-139
关键词	Mariana Trough Back-arc Basin Plagioclase Thermobarometry Magma Evolution
DOI	10.1016/j.jmarsys.2016.11.008
产权排序	第1完成单位 ; 第2完成单位 ; 第3完成单位 ; 第4完成单位 ; 第5完成单位
文献子类	Article
英文摘要	Mafic magmas are common in back-arc basin, once stalled in the crust, these magmas may undergo different evolution. In this paper, compositional and textural variations of plagioclase as well as mineral-melt geothermobarometry are presented for basalts erupted from the central Mariana Trough (CMT). These data reveal crystallization conditions and we attempt a reconstruction of the magma plumbing system of the CMT. Plagioclase megacrysts, phenocrysts, microphenocrysts, microlites, olivine, spinel, and clinopyroxene have been recognized in basalt samples, using BSE images and compositional features. The last three minerals are homogeneous as microphenocrysts. Mineral-melt barometry indicates that plagiodase crystals crystallized and eventually grew into phenocrysts and megacrysts in mush zone with depth of 5-9 km, in which the normal zoning plagioclases crystallized in the interval of various batches of basic magma recharging. Plagioclase megacrysts and phenocrysts were dissolved and/or resorbed, when new basic magmas injected into the mush zone near Moho depth. It is inferred that magma extracted from the mush zone, and adiabatically ascended via different pathways. Some basaltic magmas underwent plagioclase and clinopyroxene microphenocrysts crystallization in low-pressure before eruption. Plagioclase microlites and outermost rims probably crystallized after eruption. (C) 2016 Elsevier B.V. All rights reserved.
URL标识	查看原文
WOS关键词	PLAGIOCLASE PHENOCRYSTS ; OKINAWA TROUGH ; BASALTS ; VOLCANO ; EVOLUTION ; BENEATH ; MANTLE ; LAVAS ; RIDGE ; CRUST
语种	英语
WOS记录号	WOS:000429514700012
内容类型	期刊论文
源URL	[http://ir.idsse.ac.cn/handle/183446/5928]
专题	深海科学研究部_深海地质与地球化学研究室
通讯作者	Lai, Zhiqing(Minist Educ, Key Lab Submarine Geosci & Prospecting Tech, Qingdao 266100, Peoples R China); Zhao, Guangtao(Minist Educ, Key Lab Submarine Geosci & Prospecting Tech, Qingdao 266100, Peoples R China); Lai, Zhiqing; Zhao, Guangtao
作者单位	1.Minist Educ, Key Lab Submarine Geosci & Prospecting Tech, Qingdao 266100, Peoples R China 2.Natl Oceanog Ctr, Qingdao 266071, Peoples R China 3.Shandong Inst Ocean Resources Explorat, Qingdao 266555, Peoples R China 4.Chinese Acad Sci, Inst Deep Sea Sci & Engn, Sanya 572000, Peoples R China 5.Ocean Univ China, Coll Marine Geosci, 238 Songling Rd, Qingdao 266100, Peoples R China
推荐引用方式 GB/T 7714	Liu, Bo,Lai, Zhiqing,Han, Zongzhu,et al. The magma plumbing system in the Mariana Trough back-arc basin at 18 degrees N[J]. JOURNAL OF MARINE SYSTEMS,2018,180:132-139.
APA	Liu, Bo.,Lai, Zhiqing.,Han, Zongzhu.,Zhao, Guangtao.,Lai, Zhiqing.,...&Bu, Xuejiao.(2018).The magma plumbing system in the Mariana Trough back-arc basin at 18 degrees N.JOURNAL OF MARINE SYSTEMS,180,132-139.
MLA	Liu, Bo,et al."The magma plumbing system in the Mariana Trough back-arc basin at 18 degrees N".JOURNAL OF MARINE SYSTEMS 180(2018):132-139.