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Titlebook: Archean-Mesoproterozoic Crustal Evolution and Crust-Mantle Geodynamics of Western Liaoning-Northeast; Wei Wang Book 2018 Springer Nature S

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期刊全称Archean-Mesoproterozoic Crustal Evolution and Crust-Mantle Geodynamics of Western Liaoning-Northeast
影响因子2023Wei Wang
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发行地址Establishes Neoarchean subduction-related crust-mantle geodynamic regimes for Western Liaoning Province, North China Craton (NCC).Proposes island arc subduction and arc-continent accretion as major re
学科分类Springer Theses
图书封面Titlebook: Archean-Mesoproterozoic Crustal Evolution and Crust-Mantle Geodynamics of Western Liaoning-Northeast;  Wei Wang Book 2018 Springer Nature S
影响因子.This thesis presents geological, petrological, geochemical, and zircon U–Pb–Lu–Hf isotopic field data for representative Precambrian lithologies in the Western Liaoning-Northeastern Hebei Provinces along the northern margin of the North China Craton (NCC). It describes late Neoarchean (2.64–2.48 Ga) supracrustal metavolcanic rocks and granitoid gneisses; late Paleoproterozoic (1.72–1.68 Ga) Jianping alkaline plutons and Pinggu alkaline volcanic rocks; and newly discovered ~1.23 Ga mafic dykes. The nature of magma sources and genesis of each magmatic episode are investigated, and the Precambrian (~2.6–1.2 Ga) lithospheric mantle evolution and crust-mantle interaction processes are established for the first time –aspects that provide important constraints in our understanding of the Precambrian crustal evolution and geodynamic processes in the region studied.. .
Pindex Book 2018
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The Myth of Fat Redistribution,estern Liaoning Province (WLP) along the northern margin of Eastern Block. It is suggested that magmatic precursors of the metavolcanic rocks in the Fuxin greenstone belt were erupted during ~2640–2534 Ma, and they show dominantly positive zircon εHf(t.) values of +2.7 to +9.7. These metavolcanic ro
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The Myth of Fat Redistribution,Paleoproterozoic eastward subduction processes of Trans-North China Orogen, resulting in the formation of a potassic and enriched lithospheric mantle; and (3) at ~1671–1625 Ma and ~1230 Ma, this enriched lithospheric mantle witnessed two episodes of “vertical” accretion processes, which were ascribe
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Paleo- to Mesoproterozoic Magmatic Rock Assemblage and Crust-Mantle Geodynamic Processes,with the parental magmas subjected to different degrees of fractional crystallization. In comparison, the Pinggu K-rich volcanic rocks in the Tuanshanzi and Dahongyu Formations of Changcheng Group were erupted during ~1671–1625 Ma, and they were considered to have been derived dominantly from the pa
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