Titlebook: Main Tectonic Events and Metallogeny of the North China Craton; Mingguo Zhai,Yue Zhao,Taiping Zhao Book 2016 Springer Science+Business Med

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Book 2016llogeny. It provides asystematic review and new results on the growth and evolution of the NorthChina Craton and metallogeny. It will be of broad interest to the earthscientists working in the fields ofeconomic geology, geochemistry, and tectonics of the North China Craton andeastern Asian.

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Hirsutism

Corresponding Main Metallogenic Epochs to Key Geological Events in the North China Craton: An Exampin the Earth generated in Precambrian and records complicated geotectonic processes. The most important geological events in Precambrian tectonic evolution include Neoarchean enormous crustal growth, tectonic regime inversion from pre-plate tectonics to plate tectonics, and Great Oxidention Event (G

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Archean Continental Crust in the Southern North China Cratontonic complexes, naming, the Sushui, Dengfeng and Taihua complexes. Their equivalents probably extend into the Huoqiu and Bengbu areas of Anhui Province in the southeastern margin of the NCC, and the Longshan area of Gansu Province in the southwestern margin. In the last decade, a large number of th

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Structural Architecture and Spatial-Temporal Distribution of the Archean Domains in the Eastern Nortcommonly greenstone belts), which metamorphosed to greenschist facies, but less commonly up to granulite facies. However, the Archean domains in the Eastern North China craton were mostly metamorphosed to high-grades. For example, the majority of the Anshan-Qingyuan region was built at 2570–2500?Ma

dry-eye

Formation Ages and Environments of Early Precambrian Banded Iron Formation in the North China Craton of the Neoarchean, the most important period of BIF formation. There are three ancient terranes (>2.6?Ga) in the NCC. Most BIFs are distributed along the western margin of the Eastern Ancient Terrane, accounting for about 89?% of the total identified BIF iron ore resources in the NCC. They are cons

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Neoarchean Banded Iron Formations in the North China Craton: Geology, Geochemistry, and Its Implicat deposits occur mainly in greenstone belts area such as Anshan-Benxi, eastern Hebei, Wutai, Guyang, western Shandong and Huoqiu; formation ages of BIFs in NCC show a wide range spanning from Mesoarchean to early Paleoproterozoic, with a peak in the late Neoarchean (2.6–2.5?Ga); BIFs can be divided i

Control-Group

Archean Continental Crustal Accretion and Banded Iron Formations, Southeastern North China Cratonus metasediments. Geochemical characteristics of TTG gneisses such as high Sr/Y and (La/Yb). with steep REE patterns and trace element modeling suggest that they are generated by partial melting of hydrous meta-basalts (amphibolites) at the base of a thickened mafic continental crust, leaving a ruti