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Bin Xia
Chinese Academy of Sciences
Structural basinGeomorphologyGeologyGeochemistryOphiolite
57Publications
9H-index
494Citations
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Publications 59
Newest
#1Weiyan Chen (PetroChina)H-Index: 1
#2Guangyou Zhu (PetroChina)H-Index: 23
Last. Bin Xia (SYSU: Sun Yat-sen University)H-Index: 9
view all 8 authors...
Abstract Late Neoproterozoic extensive rifting in Tarim has been intensely debated regarding an intracontinental or a back-arc environment, which forms a key aspect for elucidating the Precambrian basement architecture and evolution of the Tarim craton. Recently, a deep well called Tarim Geological Survey Well (X1) was drilled from the northwest Tarim basin. Sixty-six samples were collected from the Sugetbrak Formation of the X1 well, including 6 sandstone samples, 29 mudstone samples and 31 bas...
1 CitationsSource
#1Hui‐Chuan Liu (China University of Petroleum)
#2Qiangtai Huang (SYSU: Sun Yat-sen University)H-Index: 5
Last. Peng Yang (SYSU: Sun Yat-sen University)H-Index: 1
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Abstract Bangong-Nujiang Suture Zone (BNSZ) in central Tibet plays an important role in evaluating the formation and uplift mechanism of Tibetan Plateau. However, its Mesozoic tectonic evolution is ambiguous and intensely debated. In this study, Early Cretacesous adakites and sodium-rich arc rocks are identified in Western Qiangtang (WQ) and Northern Lhasa (NL) sub-terranes. Forty-four adakite samples from both WQ and NL have akin geochemical features, and are derived from partial melting of sub...
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#1Weiyan ChenH-Index: 1
#2Yijie ZhangH-Index: 5
Last. Yajuan YuanH-Index: 2
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#1Wei-Liang LiuH-Index: 6
#2Yun ZhongH-Index: 5
Last. Bin Xia (CAS: Chinese Academy of Sciences)H-Index: 9
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Abstract The Zedong ophiolite is the largest ophiolite massif east of Dazhuqu in the Yarlung Zangbo Suture Zone in the southern Tibetan Plateau. However, its age, geodynamic setting and relationship to the Xigaze ophiolite remain controversial. New zircon U–Pb ages, whole-rock geochemical and Nd-Pb isotopic data from ophiolitic units provide constraints on the geodynamic and tectonic evolution of the Zedong ophiolite. U–Pb zircon geochronology of dolerite lavas and late gabbro–diabase dikes yiel...
1 CitationsSource
#1Wei Yan (SYSU: Sun Yat-sen University)
#2Guangxue Zhang (SYSU: Sun Yat-sen University)
Last. Zhenyu Lei (CGS: China Geological Survey)
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#1Chi Xu (SYSU: Sun Yat-sen University)
#2Yajuan Yuan (SCNU: South China Normal University)
Last. Ye Lu
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#1Yun ZhongH-Index: 5
#2Wei-Liang LiuH-Index: 6
Last. Bin XiaH-Index: 9
view all 7 authors...
Abstract The petrogenesis and tectonic evolution of the Mesozoic ophiolitic melanges in the western section of the Yarlung Zangbo suture zone (YZSZ) remain controversial. In this paper, we present the results of whole-rock geochemical and Sr Nd isotope analyses, zircon U Pb ages and in situ Lu Hf isotopic data obtained from mafic rocks of the northern and southern sub-belts of the western YZSZ Mesozoic ophiolitic melanges to help us understand these controversial issues. Diabases and dolerites f...
1 CitationsSource
#1Yong Zhang (NU: Nanjing University)H-Index: 4
#2Adrian R. Muxworthy (Imperial College London)H-Index: 31
Last. Matthew J. Brzozowski (NU: Nanjing University)
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#1Yun ZhongH-Index: 5
#2Wei-Liang LiuH-Index: 6
Last. Bin XiaH-Index: 9
view all 9 authors...
The South Mid-Atlantic Ridge is a typical slow-spreading ridge that represents a modern example to understand mantle composition and the evolution of mid-ocean ridge magmatism. In this paper, we investigate basalt samples dredged from four locations along the South Mid-Atlantic Ridge ranging from 18.0° to 20.6°S. The basalts belong to the tholeiitic series and exhibit normal mid-ocean ridge basalt (N-MORB) geochemical features with variable enrichments of Rb, Th, U, and Pb and depletions of Ba a...
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#1Peng Yang (SYSU: Sun Yat-sen University)H-Index: 1
#2Qiangtai Huang (SYSU: Sun Yat-sen University)H-Index: 5
Last. Xingxin Lu (SYSU: Sun Yat-sen University)H-Index: 1
view all 7 authors...
The middle of the Bangong–Nujiang Suture (BNS) in the central Tibetan Plateau hosts a series of dismembered ophiolitic fragments that document the evolution of part of the Tethys Ocean. However, the origin of these ophiolitic fragments in the Zangbei lakes region remains debated. Using new and existing field observations and petrographic, geochronologic, isotopic, and whole-rock chemical data from ophiolitic rocks in the Zangbei lakes region, we evaluate their origins and constrain the tectonic ...
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