Journal
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
Volume 18, Issue 1, Pages 266-279Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1002/2016GC006576
Keywords
subduction erosion; P-T-t path; subduction channel; Paleo-Tethys; Tibet
Categories
Funding
- DREAM project of MOST China [2016YFC0600407]
- Chinese Academy of Sciences [XDB03010600]
- National Natural Science Foundation of China [41502054, 41372066, 41630208, 41573027, 41421062]
- Key Program of the Chinese Academy of Sciences [QYZDJ-SSW-DQC026]
- talent project of Guangdong Province [2014TX01Z079]
- Guangzhou Institute of Geochemistry, Chinese Academy of Sciences [135TP201601]
- Institute of Geology and Geological Survey Project of China [1212011121243]
- China Postdoctoral Science Foundation [2015M572374]
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Subduction erosion is confirmed as a crucial geodynamic process of crustal recycling based on geological, geochemical, and geophysical observations at modern convergent plate margins. So far, not a single metamorphic record has been used for constraining a general tectonic evolution for subduction erosion. Here we first revealed metamorphic records for a subduction erosion process based on our study of the Late Paleozoic garnet-staurolite-muscovite schists in the central Qiangtang block, Tibet. Provenance analyses suggest that the protoliths of garnet-staurolite-muscovite schists have the Northern Qiangtang-affinity and were deposited in an active continental margin setting. Mineral inclusion data show that the early metamorphic stage (M-1) recorded blueschist facies pressure-temperature (P-T) conditions of 0.8-1.1 GPa and 402-441 degrees C, indicating that a part of the material from the overriding plate had been abraded into the subduction channel and undergone high-pressure/low-temperature metamorphism. The peak metamorphic stage (M-2) recorded amphibolite facies P-T conditions of 0.3-0.5 GPa and 470-520 degrees C. The 40Ar/39Ar cooling ages (263-259 Ma) yielded from muscovite suggest the amphibolite facies metamorphism (>263 Ma) occurred at oceanic subduction stage. The distinctly staged metamorphism defines a clockwise and warming decompression P-T-t path which reveals an underplating process following the early subduction erosion. During the tectonic process, the eroded low-density material escaped from the cold subduction channel and rise upward into the warm middle-lower crust of the upper plate, undergoing amphibolite facies metamorphism. Our new results revealed a complete evolutional process from the early subduction erosion to the subsequent underplating during the northward subduction of the Paleo-Tethys Ocean.
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