超高压变质岩中柯石英的产出和保存机制

刘鹏雷; 章军锋; 金振民

doi:10.3799/dqkx.2019.231

Volume 44 Issue 12

Dec. 2019

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Article Navigation > Earth Science > 2019 > 44(12): 4028-4033

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

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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

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:

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

doi: 10.3799/dqkx.2019.231

School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2019-08-19
Publish Date: 2019-12-15

Abstract

Abstract

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.
- Dabieshan,
- UHP,
- dolomite,
- interstitial coesite,
- tectonic overpressure,
- petrology

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References(39)

References

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