Multiphase solid inclusions in UHP eclogite from the Dabie orogen: Constraints on the nature of metamorphic fluid/melt during continental subduction-zone metamorphism

被引：0

|

作者：

Gao, Xiao-Ying ^{[1
]}

Zheng, Yong-Fei ^{[1
]}

机构：

[1] Univ Sci & Technol China, Sch Earth & Space Sci, Hefei 230026, Peoples R China

来源：

GEOCHIMICA ET COSMOCHIMICA ACTA | 2010年 / 74卷 / 12期

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D O I：

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中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

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页码：A319 / A319

页数：1

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[41] Decoupling of fluid and trace element release in subducting slab? Comment on “Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies; implications for deep subduction-zone processes” by C. Spandler et al. (Contrib Mineral Petrol 146:205–222, 2003)
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Contributions to Mineralogy and Petrology, 2004, 148 : 502 - 505
[42] Chlorine-rich fluid or melt activity during granulite facies metamorphism in the Late Proterozoic to Cambrian continental collision zone-An example from the Sor Rondane Mountains, East Antarctica
Higashino, Fumiko
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Satish-Kumar, M.
Ishikawa, Masahiro
Maki, Kenshi
Tsuchiya, Noriyoshi
Grantham, Geoffrey H.
Hirata, Takafumi
PRECAMBRIAN RESEARCH, 2013, 234 : 229 - 246
[43] Decoupling of fluid and trace element release in subducting slab?: Comment on "Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies;: implications for deep subduction-zone processes" by C.!Spandler et al. (Contrib Mineral Petrol 146:205-222, 2003)
Liebscher, A
CONTRIBUTIONS TO MINERALOGY AND PETROLOGY, 2004, 148 (04) : 502 - 505

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