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《ACTA PETROLOGICA SINICA》 1999-03
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Mesozoic potassic magmatism in the Dabie Mountains: Implication for exhumation mechanism of ultrahigh pressure metamorphic terranes

Ma Changqian, Yang Kunguang, Xu Changhai, Li Zhichang and Carl Ehlers  
The Dabie Mountains are unique among ultrahigh pressure (UHP) metamorphic terranes in having the most profound post collisional plutonism The Mesozoic shoshonitic and calc alkaline intrusive rocks can be divided into three groups with different isotopic ages, rock assemblages and chemical features Group I consists of late Triassic (~ 210 Ma) mafic monzodiorites It could have been generated by partial melting of enriched subcontinental lithosphere mantle due to slab breakoff Group II consists mainly of middle Jurassic early Cretaceous (160 ~ 120 Ma ) hornblende quartz monzonitic, biotite monzogranitic, and syenogranitic plutons, and could have been produced mainly from crustal assimilation/melting and fractional crystallization of mantle derived magmas Group III is presented by Cretaceous (125 ~ 95 Ma ) granitic stocks and granitic porphyry, and its magmas could have derived from anatexis of the Dabie complex and was highly evolved in a hot doming setting The late Triassic early Jurassic slab breakoff may be responsible for the exhumation of UHP rocks through the mantle The voluminous granitic emplacement together with an episode of rapid denudation suggests that mafic magmatic underplating and inflation could have played a role in the Middle Jurassic Early Cretaceous rapid exhumation of UHP rocks
【Fund】: 国家自然科学基金
【CateGory Index】: P588.121
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