Volume 44 Issue 12
Dec.  2019
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Liu Penglei, Zhang Junfeng, Jin Zhenmin, 2019. Occurrences and Preservation Mechanisms of Coesite in Ultrahigh-Pressure Metamorphic Rocks. Earth Science, 44(12): 4028-4033. doi: 10.3799/dqkx.2019.231
Citation: Liu Penglei, Zhang Junfeng, Jin Zhenmin, 2019. Occurrences and Preservation Mechanisms of Coesite in Ultrahigh-Pressure Metamorphic Rocks. Earth Science, 44(12): 4028-4033. doi: 10.3799/dqkx.2019.231

Occurrences and Preservation Mechanisms of Coesite in Ultrahigh-Pressure Metamorphic Rocks

doi: 10.3799/dqkx.2019.231
  • Received Date: 2019-08-19
  • Publish Date: 2019-12-15
  • Insights into the occurrences and preservation mechanisms of coesite bear important implications for the formation and evolution of ultrahigh-pressure (UHP) metamorphic rocks. Early researches reveal that coesite usually appears as inclusions in strong host minerals in UHP rocks. Thus far,interstitial coesite has only been found in the UHP two-mineral eclogite from Yangkou,Sulu orogen. Two major mechanisms have been proposed for the preservation of coesite:the "pressure-vessel" model involving "tectonic overpressure" and dry metamorphic environment. Interstitial coesite and abundant coesite inclusions in dolomite recently discovered in a UHP metasedimentary rock from the Ganjialing area in Dabieshan highlight the role of dry metamorphic environment and undermine the importance of "pressure-vessel" model in preserving coesite.

     

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