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Xiao-Long Huang

Researcher at Chinese Academy of Sciences

Publications -  87
Citations -  5077

Xiao-Long Huang is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Zircon & Craton. The author has an hindex of 34, co-authored 86 publications receiving 3996 citations. Previous affiliations of Xiao-Long Huang include Nanjing University & Center for Excellence in Education.

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Ages and magnetic structures of the South China Sea constrained by deep tow magnetic surveys and IODP Expedition 349

TL;DR: In this paper, the authors combined analyses of deep tow magnetic anomalies and International Ocean Discovery Program Expedition 349 cores to show that seafloor spreading started around 33 Ma in the northeastern South China Sea (SCS), but varied slightly by 1-2 Myr along the northern continent-ocean boundary.
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Age and duration of the Emeishan flood volcanism, SW China: Geochemistry and SHRIMP zircon U–Pb dating of silicic ignimbrites, post-volcanic Xuanwei Formation and clay tuff at the Chaotian section

TL;DR: In this article, the authors used SHRIMP zircon U-Pb dating on rare felsic ignimbrite in the uppermost of the Emeishan lava succession, the Xuanwei Formation which immediately overlies the EMEishan basalts and a clay tuff at the Middle-Late Permian boundary at Chaotian.
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Crust-mantle interaction during the tectono-thermal reactivation of the North China Craton: constraints from SHRIMP zircon U–Pb chronology and geochemistry of Mesozoic plutons from western Shandong

TL;DR: In this article, chronological, geochemical and Sr-Nd-Pb isotopic analyses have been carried out on the Mesozoic plutons in western Shandong with the aim of characterizing crustal-mantle evolution during the tectono-thermal reactivation of the craton.
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Zircon U–Pb and Hf isotope constraints on crustal melting associated with the Emeishan mantle plume

TL;DR: In this paper, the authors provided new constraints on the petrogenesis and protolith of peralkaline, metaluminous and peraluminous intrusions and rhyolitic tuffs in Emeishan large igneous province, with significant bearing on crustal melting associated with mantle plumes.
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Neoproterozoic adakitic rocks from Mopanshan in the western Yangtze Craton: Partial melts of a thickened lower crust

TL;DR: Zhou et al. as discussed by the authors proposed that the Neoproterozoic adakites from Xuelongbao and Datian along the western margin of the Yangtze Craton are the melting products of a subducted oceanic slab.