喜马拉雅造山带两种不同类型榴辉岩与印度大陆差异性俯冲

张泽明; 丁慧霞; 董昕; 田作林

doi:10.3799/dqkx.2019.040

Volume 44 Issue 5

May 2019

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Zhang Zeming, Ding Huixia, Dong Xin, Tian Zuolin, 2019. Two Contrasting Eclogite Types in the Himalayan Orogen and Differential Subduction of Indian Continent. Earth Science, 44(5): 1602-1619. doi: 10.3799/dqkx.2019.040

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Zhang Zeming, Ding Huixia, Dong Xin, Tian Zuolin, 2019. Two Contrasting Eclogite Types in the Himalayan Orogen and Differential Subduction of Indian Continent. Earth Science, 44(5): 1602-1619. doi: 10.3799/dqkx.2019.040

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Two Contrasting Eclogite Types in the Himalayan Orogen and Differential Subduction of Indian Continent

doi: 10.3799/dqkx.2019.040

1.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2019-02-15
Publish Date: 2019-05-15

Abstract

Abstract

The core of the Himalayan orogen, resulting from the Cenozoic collision between the Indian and Asian continents, consists of high-pressure (HP) and ultrahigh-pressure metamorphic rocks. The ultrahigh-pressure (UHP) eclogites occur in the western segment of the Himalayan orogen, and contain garnet, omphacite, coesite, phengite, zoisite/epidote, kyanite and rutile. The UHP eclogites record a peak metamorphic condition of 2.6-2.8 GPa and 600-620℃, and a late stage of amphibolite-facies retrogression and slight partial melting. The prograde, peak and retrograde metamorphic times of the UHP eclogites are~50 Ma, ~45-47 Ma and~35-40 Ma, respectively, indicating that the UHP eclogites underwent a rapid subduction and rapid exhumation. The HP eclogites occur in the east-central segment of the Himalayan orogen, and contain garnet, omphacite, phengite, quartz and rutile. The HP eclogites have a peak metamorphic condition of > 2.1 GPa and > 750℃, and experienced a late stage of granulite-facies retrogression and extensive anataxis. The peak and retrograde metamorphic times of the HP eclotites are~38 Ma and~14-17 Ma, respectively, indicating that the HP eclogites underwent a slow subduction and slow exhumation. The presence of two contrasting eclogite types in the Himalayan orogen shows that, after the India collided with Asia at around 51-53 Ma, the north-western margin of Indian continental crust deeply subducted into the mantle, and underwent UHP metamorphism, and while the north-eastern margin of Indian continental crust shallowly subducted beneath the Asian continent, and experienced HP metamorphism.
- high-pressure eclogite,
- ultrahigh-pressure eclogite,
- metamorphic P-T-t path,
- continental subduction,
- Himalayan orogen,
- metamorphic rock,
- petrology

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References(120)

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Two Contrasting Eclogite Types in the Himalayan Orogen and Differential Subduction of Indian Continent

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