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Xiang Bai

Researcher at Peking University

Publications -  34
Citations -  1847

Xiang Bai is an academic researcher from Peking University. The author has contributed to research in topics: Craton & Zircon. The author has an hindex of 21, co-authored 30 publications receiving 1568 citations. Previous affiliations of Xiang Bai include China Earthquake Administration & University of Texas Health Science Center at San Antonio.

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Zircon U–Pb chronology of the Jianping Complex: Implications for the Precambrian crustal evolution history of the northern margin of North China Craton

TL;DR: In this article, the authors present results from LA-ICPMS zircon U-Pb isotope dating from various lithological units in this complex, which reveal that the magmatic precursors of the metavolcanic rocks associated with the supracrustal sequence were generated during 2555-2550, and up to 2615-Ma.
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Neoarchean intra-oceanic arc system in the Western Liaoning Province: Implications for Early Precambrian crustal evolution in the Eastern Block of the North China Craton

TL;DR: In this paper, a comprehensive analysis of the basement terranes in the EB, a late Neoarchean (~ 2.5-2.6 ǫ) intra-oceanic arc system with relict MORB-like basaltic rocks bordering the northwestern margin of the continental nucleus is presented.
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Geochemistry, zircon U–Pb geochronology and Lu–Hf isotopes of metavolcanics from eastern Hebei reveal Neoarchean subduction tectonics in the North China Craton

TL;DR: Based on whole rock geochemistry, the authors classified intermediate-mafic volcanic rocks into four groups: back-arc MORB basalts (Group #1), arc-related andesites-basalts (Groups #2 and #3), NEB-enriched basalts and typical arc volcanic rocks at 2523-±-6-Ma to 2614−±-18-Ma.
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Geochemistry and zircon U-Pb-Hf isotopic systematics of the Neoarchean Yixian-Fuxin greenstone belt, northern margin of the North China Craton: Implications for petrogenesis and tectonic setting

TL;DR: The Yixian-Fuxin greenstone belt in the Western Liaoning metamorphic terrane is situated in the middle segment of the northern margin of the North China Craton (NCC) and is composed mainly of plagioclase amphibolites, pyroxene amphibolite and hornblende plagioclase gneisses as mentioned in this paper.
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Petrogenesis and geochronology of Precambrian granitoid gneisses in Western Liaoning Province: Constraints on Neoarchean to early Paleoproterozoic crustal evolution of the North China Craton

TL;DR: In this paper, the authors investigated the geochemical precursors of granitoid gneisses in the North Chaoyang-Fuxin-Yixian granite-greenstone belt (NCFY-GGB).