| The magma plumbing system in the Mariana Trough back-arc basin at 18 degrees N | |
Lai, Zhiqing1,2; Zhao, Guangtao1,2; Han, Zongzhu1,2; Huang, Bo3; Li, Min4; Tian, Liyan5 ; Liu, Bo1,2; Bu, Xuejiao1,2; 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)
| |
| 2018-04-01 | |
| Source Publication | JOURNAL OF MARINE SYSTEMS
 |
| Volume | 180Pages:132-139 |
| Contribution Rank | 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 |
| Abstract | 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. |
| Subtype | Article |
| Keyword | Mariana Trough Back-arc Basin Plagioclase Thermobarometry Magma Evolution |
| WOS Headings | Science & Technology ; Physical Sciences ; Life Sciences & Biomedicine |
| DOI | 10.1016/j.jmarsys.2016.11.008 |
| URL | 查看原文 |
| Indexed By | SCI |
| Language | 英语 |
| WOS Keyword | PLAGIOCLASE PHENOCRYSTS ; OKINAWA TROUGH ; BASALTS ; VOLCANO ; EVOLUTION ; BENEATH ; MANTLE ; LAVAS ; RIDGE ; CRUST |
| WOS Subject | Geosciences, Multidisciplinary ; Marine & Freshwater Biology ; Oceanography |
| WOS ID | WOS:000429514700012 |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.idsse.ac.cn/handle/183446/5928 |
| Collection | 深海科学研究部_深海地质与地球化学研究室 |
| Corresponding Author | Lai, Zhiqing; Zhao, Guangtao; 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) |
| Affiliation | 1.Minist Educ, Key Lab Submarine Geosci & Prospecting Tech, Qingdao 266100, Peoples R China 2.Ocean Univ China, Coll Marine Geosci, 238 Songling Rd, Qingdao 266100, Peoples R China 3.Natl Oceanog Ctr, Qingdao 266071, Peoples R China 4.Shandong Inst Ocean Resources Explorat, Qingdao 266555, Peoples R China 5.Chinese Acad Sci, Inst Deep Sea Sci & Engn, Sanya 572000, Peoples R China |
| Recommended Citation GB/T 7714 | Lai, Zhiqing,Zhao, Guangtao,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 | Lai, Zhiqing.,Zhao, Guangtao.,Han, Zongzhu.,Huang, Bo.,Li, Min.,...&Zhao, Guangtao.(2018).The magma plumbing system in the Mariana Trough back-arc basin at 18 degrees N.JOURNAL OF MARINE SYSTEMS,180,132-139. |
| MLA | Lai, Zhiqing,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. |
| Files in This Item: | There are no files associated with this item. | |||||
Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.
Edit Comment