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Guochun Zhao
Northwest University (United States)
423Publications
97H-index
30.6kCitations
Publications 426
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#1Pei-yuan Hu (Northwest University (United States))H-Index: 6
#2Qing-guo Zhai (Ontario Ministry of Natural Resources)H-Index: 3
Last.Hao Wu (Ontario Ministry of Natural Resources)H-Index: 2
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Abstract It was commonly accepted that the North Lhasa terrane of the present-day central Tibetan Plateau in Asia came from the northern Gondwana, but the timing of its northward drifting away from the Gondwana remains controversial. Here we present for the first time U–Pb age and Hf isotope data on detrital zircons from the Cambrian metasedimentary rocks in the North Lhasa terrane. The detrital zircons display age peaks at ca. 505, 548, 926, and 1104 Ma, and are interpreted to have Gondwanan so...
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#1Yigui Han (Northwest University (United States))H-Index: 21
#2Guochun Zhao (Northwest University (United States))H-Index: 97
Last.Jinlong Yao (Northwest University (United States))H-Index: 11
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#1Chaohui LiuH-Index: 19
#2Guochun Zhao (HKU: University of Hong Kong)H-Index: 97
Last.Jia CaiH-Index: 13
view all 4 authors...
1 CitationsSource
#1Chaohui LiuH-Index: 19
#2Guochun ZhaoH-Index: 97
Last.Jia CaiH-Index: 13
view all 4 authors...
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#1Jinlong Yao (Northwest University (United States))H-Index: 11
#2Peter A. Cawood (St And: University of St Andrews)H-Index: 70
Last.Guochun Zhao (Northwest University (United States))H-Index: 97
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Abstract The Neoproterozoic Jiangnan Orogen in South China records a succession of arc-trench-basin assemblages culminating in accretion of the bounding Yangtze and Cathaysia blocks to form the stabilized South China Craton. The orogen can be traced over some 1500 km and extends up to 100 km across strike. It is divisible into three domains: the northeast domain (also referred to as the Huaiyu or Shuangxiwu Terrane), the central domain (Jiuling Terrane), and an undifferentiated southwest domain....
2 CitationsSource
#1Hai Zhou (Northwest University (United States))H-Index: 1
#2Guochun Zhao (Northwest University (United States))H-Index: 97
Last.Bo Wang (HKU: University of Hong Kong)H-Index: 11
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Abstract Late Paleozoic tectonic evolution of the northern margin of the North China Craton (NCC) remains controversial, especially for the mechanism and time during the late-stage oceanic consumption of the Paleo-Asian Ocean (PAO). We address this issue through geochronological, geochemical and Lu-Hf isotopic studies on felsic-mafic volcanic rock suites and granite plutons from the Damao area in the western segment of the NCC's northern margin. Zircon U-Pb dating reveals that the volcanic suite...
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#1Xiaohan Dong (CAS: Chinese Academy of Sciences)H-Index: 1
#2Touping Peng (CAS: Chinese Academy of Sciences)H-Index: 25
Last.Lin-Li Chen (CAS: Chinese Academy of Sciences)H-Index: 3
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Abstract Early Cretaceous granitoids are widespread on the Tibetan Plateau and record the tectonic evolution of several Tethyan oceans. We describe Early Cretaceous high-Mg (Mg # > 50) and low-Mg (Mg # Pb dating reveals two episodes of granitoid emplacement at ~122 and ~117 Ma. High-Mg series rocks have higher Mg # and compatible element concentrations (e.g., Cr and Ni) than low-Mg series samples. Their Mg # and compatible element abundances are also elevated relative to an experimental melt gen...
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#1Jinlong Yao (Northwest University (United States))H-Index: 11
#2Liangshu Shu (NU: Nanjing University)H-Index: 44
Last.Guochun Zhao (HKU: University of Hong Kong)H-Index: 97
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1 CitationsSource
#1Wenzhu Hou (CUHK: The Chinese University of Hong Kong)H-Index: 16
#2Guochun Zhao (HKU: University of Hong Kong)H-Index: 97
Last.Qian Liu (HKU: University of Hong Kong)H-Index: 16
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