Fluid inclusions hidden in coesite-bearing zircons in ultrahigh-pressure metamorphic rocks from southwestern Sulu terrane in eastern China |
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Authors: | Email author" target="_blank">Fulai?LiuEmail author Zhiqin?Xu |
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Institution: | (1) Institute of Geology, Chinese Academy of Geological Sciences, 100037 Beijing, China |
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Abstract: | Primary fluid inclusions, together with coesite mineral inclusions, are identified in the same zircon domains by laser Raman
spectroscopy, cathodoluminescence (CL) image and micro-texture analysis in paragneiss and eclogite from the main drilling
hole of Chinese Continental Scientific Drilling Project in southwestern Sulu terrane. Most fluid inclusions are characterized
by CO2 (gas)-H2O (liquid) two-phase, a few by H2O one-phase liquid inclusions. These features indicate that the eclogite and its country-rocks may be located in the “wet
system” rather than in the “dry system” during UHP metamorphism. SHRIMP U-Pb dating indicates that the timing of trapping
the fluid and coesite inclusions in metamorphic zircon domains is about 233.7 ±4.3 Ma, which may represent the age of zircon
growth in the stage of pressure decrease but temperature increase during the retrograde period of UHP metamorphism thus indicating
the fluid activity still under the UHP conditions. The zircons further overgrew at about 213.2 ±5.2 Ma in response to amphibolite-facies
retrogression. Therefore, fluid activity in the Sulu UHP metamorphic rocks principally occurred during the exhumation of UHP
slab in the Middle to Late Triassic. The present results not only provide insight into the fluid property and fluid-rock interaction
mechanism in the Sulu-Dabie UHP terrane, but also present a new means to exactly identify the primary fluid inclusions preserved
in zircons from the UHP metamorphic rocks. |
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Keywords: | fluid inclusion zircon U-Pb dating UHP metamor-phism Continental Drilling |
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