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Jinlong Yao
Northwest University (United States)
17Publications
11H-index
648Citations
Publications 18
Newest
#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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#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
view all 4 authors...
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...
Source
#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
view all 4 authors...
1 CitationsSource
#1Liangshu Shu (NU: Nanjing University)H-Index: 44
#2Jingqiang Wang (Guilin University of Technology)H-Index: 1
Last.Jinlong Yao (NU: Nanjing University)H-Index: 11
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Abstract The Jiangnan orogenic belt in South China, formed by the collision of the Yangtze and Cathaysia sub-blocks, represents a key to reconstruct the assembly of the Rodinia supercontinent. Here we investigated the Fuchuan ophiolite melange and Shexian magmatic units in the eastern Jiangnan belt, and report the first findings of anorthosite and leucogranite that are dated at 848 ± 4 and 840 ± 5 Ma, respectively. The anorthosites yield positive eNd(t) values (2.3–4.2) and lower initial 87Sr/86...
3 CitationsSource
#1Jinlong YaoH-Index: 11
Last.G Zhao
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#1Peter A. Cawood (St And: University of St Andrews)H-Index: 70
#2Guochun Zhao (HKU: University of Hong Kong)H-Index: 97
Last.Yuejun Wang (SYSU: Sun Yat-sen University)H-Index: 49
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Abstract The history of the South China Craton and the constituent Yangtze and Cathaysia blocks are directly linked to Earth's Phanerozoic and Precambrian record of supercontinent assembly and dispersal. Exposed Archean rocks are limited to isolated fragments in the Yangtze Block that preserve a record of Meso- to Neo-Archean magmatism, sedimentation and metamorphism associated with a period of global craton formation and stabilization that corresponds with the assembly of the Kenor supercontine...
71 CitationsSource
#1Jinlong Yao (NU: Nanjing University)H-Index: 11
#2Liangshu Shu (NU: Nanjing University)H-Index: 44
Last.Jinyi LiH-Index: 12
view all 4 authors...
We acknowledge the financial support by the Major State Research Development Program of China (Grant No. 2016YFC0600202), National Natural Science Foundation of China (Nos. 41330208 and 41572200) and State Key Laboratory for Mineral Deposits Research (Nanjing University) (ZZKT-201603).
10 CitationsSource
#1Jinlong Yao (NU: Nanjing University)H-Index: 11
#2Peter A. CawoodH-Index: 70
Last.Jinyi Li (CAS: Chinese Academy of Sciences)H-Index: 12
view all 5 authors...
AbstractThe Neoproterozoic Jiangnan orogenic belt delineates the suture zone between the Cathaysia and Yangtze blocks of the South China Craton. The western part of the belt, in the Longsheng region, consists of a disrupted mafic-ultramafic assemblage of pillow basalt, gabbro, diabase, and peridotite along with siliceous marble, ophicalcite, and jasper mixed with basalt. Significant talc deposits occur on the margins of the ultramafic bodies as well as in the transition zone between marble and b...
15 CitationsSource
#1Jinlong Yao (NU: Nanjing University)H-Index: 11
#2Liangshu Shu (NU: Nanjing University)H-Index: 44
Last.Jinyi LiH-Index: 12
view all 4 authors...
The authors acknowledge the financial support provided by the National Basic Research Program of China (973 Program, No. 2012CB416701), the National Natural Science Foundation of China (Nos. 41330208, 41572200, 41272226) and the Bureau of China Geological Survey (No. 1212011121064-01).
24 CitationsSource
12