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Songjie Wang

Researcher at Shandong University of Science and Technology

Publications -  28
Citations -  656

Songjie Wang is an academic researcher from Shandong University of Science and Technology. The author has contributed to research in topics: Craton & Zircon. The author has an hindex of 13, co-authored 25 publications receiving 502 citations. Previous affiliations of Songjie Wang include China University of Geosciences (Wuhan) & University of Maryland, College Park.

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Partial melting of deeply subducted eclogite from the Sulu orogen in China

TL;DR: Partial melting of an ultrahigh pressure eclogite in the Mesozoic Sulu orogen, China is reported, using zircon U–Pb dating and petrological analyses, to show that partial melting occurred at 228–219 Myr ago, shortly after peak metamorphism at 230 Myr ago.
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A late Archean tectonic mélange in the Central Orogenic Belt, North China Craton

TL;DR: Laterally extensive belts of melange characterize Phanerozoic convergent plate margins, but are rare in Archean terranes as mentioned in this paper, and the Zanhuang melange separates a passive margin to foreland basin sequence developed on the western edge of the Eastern Block of the NCC from an arc terrane consisting of trondhjemitic, tonalitic and granodioritic (TTG) gneisses in the Central Orogenic Belt (COB).
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Fluid generation and evolution during exhumation of deeply subducted UHP continental crust: Petrogenesis of composite granite–quartz veins in the Sulu belt, China

TL;DR: In this paper, the authors presented the results of a study at the State Key Laboratory of Geological Processes and Mineral Resources and Center for Global Tectonics, School of Earth Sciences, China University of Geosciences, Wuhan, China Laboratory for Crustal Petrology, Department of Geology, University of Maryland, College Park, MD, USA.
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Structural relationships along a Neoarchean arc-continent collision zone, North China craton

TL;DR: Zhang et al. as mentioned in this paper used zircon U-Pb dating of various types of blocks from the Zanhuang melange to show that the formation and associated deformation occurred in the Neo-archean (ca. 2.5 Ga).