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DEEP Neoarchean Subduction Indicated by Ultra-high Pressure TiO_(2)(Ⅱ) Inclusion in Ophiolitic Podiform Chromitite Block in Mélange, Central(Taihang) Orogenic Belt, North China
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作者 Tim KUSKY WANG Lu +2 位作者 Paul ROBINSON Richard WIRTH HUANG Yang 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2021年第S01期85-87,共3页
Understanding crust-mantle recycling through time,especially into the Archean,is crucial for understanding how the crust has grown from the mantle,and in turn how crustal material returned to the mantle alters the man... Understanding crust-mantle recycling through time,especially into the Archean,is crucial for understanding how the crust has grown from the mantle,and in turn how crustal material returned to the mantle alters the mantle reservoir.Recycling of crustal material,such as C-H-O-NS-P are especially important for understanding how processes such as subduction,melting,volcanism,and the release of volatiles have regulated climate and life on Earth over billions of years. 展开更多
关键词 Archean tectonics ophiolitic mélange ultrahigh-pressure minerals suduction carbon cycle
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