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Dong Fu

Researcher at China University of Geosciences (Wuhan)

Publications -  21
Citations -  701

Dong Fu is an academic researcher from China University of Geosciences (Wuhan). The author has contributed to research in topics: Zircon & Craton. The author has an hindex of 11, co-authored 17 publications receiving 409 citations.

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Insights into the tectonic evolution of the North China Craton through comparative tectonic analysis: A record of outward growth of Precambrian continents

TL;DR: In this article, the authors present an actualistic tectonic division and evolution of the North China Craton based on the Wilson Cycle and comparative analysis that uses a multi-disciplinary approach to define sutures, their ages, and the nature of the rocks between them, to determine their mode of formation and means of accretion or exhumation.
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Paired metamorphism in the Neoarchean: A record of accretionary-to-collisional orogenesis in the North China Craton

TL;DR: In this article, the authors investigated the Neoarchean Dengfeng Complex, a typical granite-greenstone belt in the southern part of the North China Craton (NCC), using petrography, geochronology, and phase equilibrium constraints on rocks from different lithostructural units.
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Geochronology and geochemistry of late Carboniferous volcanic rocks from northern Inner Mongolia, North China: Petrogenesis and tectonic implications

TL;DR: Zircon U-Pb ages, geochemical and Sr-Nd isotopic data are presented for the late Carboniferous Baoligaomiao Formation (BG Fm) and Delewula Formation (DW Fm.) volcanic rocks, widely distributed in northern Inner Mongolia, in the northern part of the Xing'an-Mongolia Orogenic Belt (XMOB) as mentioned in this paper.
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Sedimentary provenance in response to Carboniferous arc-basin evolution of East Junggar and North Tianshan belts in the southwestern Central Asian Orogenic Belt

TL;DR: Li et al. as discussed by the authors carried out an investigation on the provenance of Carboniferous sandstones from the Yaomoliang Formation in East Junggar and the Qijiaojing Formation in North Tianshan.