Fluid inclusions in coesite-bearing eclogites and jadeite quartzite at Shuanghe, Dabie Shan (China).

B. Fu; J.L.R. Touret; Y.-F. Zheng

doi:10.1046/j.0263-4929.2001.00327.x

Fluid inclusions in coesite-bearing eclogites and jadeite quartzite at Shuanghe, Dabie Shan (China).

B. Fu
, J.L.R. Touret
, Y.-F. Zheng

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

Fluid inclusions in coesite-bearing eclogites and jadeite quartzite at Shuanghe in Dabie Shan, East-central China, have preserved remnants of early, prograde and/or peak metamorphic fluids, reset during post-UHP (ultrahigh-pressure) metamorphic uplift. Inclusions occur in several minerals (e.g. omphacite and epidote), notably as isolated, primary inclusions in quartz included in various host minerals. Two major fluid types have been identified: non-polar fluid species (N

Original language	English
Pages (from-to)	529-545
Journal	Journal of Metamorphic Geology
Volume	19
DOIs	https://doi.org/10.1046/j.0263-4929.2001.00327.x
Publication status	Published - 2001

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SDG 10 Reduced Inequalities

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abstract = "Fluid inclusions in coesite-bearing eclogites and jadeite quartzite at Shuanghe in Dabie Shan, East-central China, have preserved remnants of early, prograde and/or peak metamorphic fluids, reset during post-UHP (ultrahigh-pressure) metamorphic uplift. Inclusions occur in several minerals (e.g. omphacite and epidote), notably as isolated, primary inclusions in quartz included in various host minerals. Two major fluid types have been identified: non-polar fluid species (N",

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JF - Journal of Metamorphic Geology

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Fluid inclusions in coesite-bearing eclogites and jadeite quartzite at Shuanghe, Dabie Shan (China).

Abstract

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