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 JournalArticleAcademicpeer-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 languageEnglish
    Pages (from-to)529-545
    JournalJournal of Metamorphic Geology
    Volume19
    DOIs
    Publication statusPublished - 2001

    Fingerprint

    Dive into the research topics of 'Fluid inclusions in coesite-bearing eclogites and jadeite quartzite at Shuanghe, Dabie Shan (China).'. Together they form a unique fingerprint.

    Cite this