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Shuwen Liu
Researcher at Peking University
Publications - 45
Citations - 3722
Shuwen Liu is an academic researcher from Peking University. The author has contributed to research in topics: Zircon & Craton. The author has an hindex of 31, co-authored 45 publications receiving 3361 citations. Previous affiliations of Shuwen Liu include Chinese Ministry of Education.
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Contrasting Late Carboniferous and Late Permian–Middle Triassic intrusive suites from the northern margin of the North China craton: Geochronology, petrogenesis, and tectonic implications
Shuan-Hong Zhang,Yue Zhao,Biao Song,Jian Min Hu,Shuwen Liu,Yue-Heng Yang,Fukun Chen,Xiaoming Liu,Jian Liu +8 more
TL;DR: In this paper, two contrasting intrusive suites have been identified from the northern margin of the North China craton: a Late Carboniferous dioritegranodiorite suite mainly made up of quartz diorites, dioritic granitoids, tonalite, and hornblende gabbro, and a Late Permian-middle Triassic suite of granitoid intrusions consisting of monzogranite, syenogranites, and quartz monzonite.
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Th–U–Pb monazite geochronology of the Lüliang and Wutai Complexes: Constraints on the tectonothermal evolution of the Trans-North China Orogen
TL;DR: In this paper, the authors apply the electron microprobe Th-U-Pb monazite dating technique to determine the ages of the peak metamorphic event and subsequent exhumation of the low- to medium-grade Luliang and Wutai complexes in the Trans-North China Orogen.
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Archean geodynamics in the Central Zone, North China Craton: constraints from geochemistry of two contrasting series of granitoids in the Fuping and Wutai complexes
TL;DR: The Wutai granitoids have higher K 2 O, LILE and Rb/Sr but lower Sr/Y and La N /Yb N than the Fuping TTG gneisses, are characterized by Nd T DM from 2.5 to 2.8 and e Nd( t ) from 0.49 to 3.34 as mentioned in this paper.
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Geological and isotopic geochemical constraints on the evolution of the Fuping Complex, North China Craton
TL;DR: The Fuping Complex as discussed by the authors comprises three major lithological assemblages: the ∼2.50 Ga trondhjemite-tonalite-granodiorite (TTG) gneisses, the Wanzi paragneisses and the 2.02 Ga Nanying granitic gneises.
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Geochemistry and U–Pb zircon ages of metamorphic volcanic rocks of the Paleoproterozoic Lüliang Complex and constraints on the evolution of the Trans-North China Orogen, North China Craton
TL;DR: In this article, U-Pb zircon dating on two metamorphosed volcanic rocks from the Yejishan and Luliang groups reveals that they formed at 2210−±−13−Ma and 2213−±-47−Ma, respectively, and were metamorphous at ∼1832−Ma.