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DINGLin
GeomorphologyGeologyTerraneSubductionPlateau
190Publications
48H-index
9,275Citations
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Publications 212
Newest
#1Shun Li (SYSU: Sun Yat-sen University)H-Index: 7
#2Changqing Yin (SYSU: Sun Yat-sen University)H-Index: 21
Last. Upendra Baral (CAS: Chinese Academy of Sciences)H-Index: 5
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Abstract Placing precise constraints on the timing of initial Lhasa-Qiangtang collision is essential to understand the assembly processes and uplift mechanism of the Tibetan Plateau prior to the Cenozoic India-Asia collision. Along the over 2000-km-long Bangong-Nujiang suture zone, the timing of initial Lhasa-Qiangtang collision remains highly controversial, with estimates ranging from Middle Jurassic to Late Cretaceous, spanning nearly 100 Myr. Provenance analysis of clastic rocks has been prov...
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#1Hou-Qi Wang (CAS: Chinese Academy of Sciences)
#2DINGLin (CAS: Chinese Academy of Sciences)H-Index: 48
Last. Muhammad Qasim (CAS: Chinese Academy of Sciences)H-Index: 3
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Abstract Field observations, petrology, zircon geochronology, whole-rock geochemistry, and Sr-Nd isotopes were used to reveal the lithology, age, and tectonic setting of the protoliths of the Sangsang mafic schists in the Yarlung Zangbo Suture Zone (YZSZ), central southern Tibet. The mafic schists occur as exotic blocks within the accretionary complex of the YZSZ. Relic amygdaloidal features indicate the schist protoliths were volcanic rocks. The mineral assemblage mainly comprises riebeckite + ...
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#1Yi-chun Zhang (CAS: Chinese Academy of Sciences)H-Index: 13
#2Kyi Pyar AungH-Index: 1
Last. Kyaing SeinH-Index: 1
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#1Jin-Xiang Li (CAS: Chinese Academy of Sciences)H-Index: 13
#2Weiming Fan (CAS: Chinese Academy of Sciences)H-Index: 58
Last. Kyaing SeinH-Index: 3
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Cretaceous mafic–felsic intrusions are extensively distributed in the West Burma terrane (Myanmar), but their petrogenesis and tectonic setting still remain unclear. In this study, whole-rock geochemical and Sr–Nd as well as zircon U–Pb and Hf isotopic data for the Cretaceous mafic–felsic intrusions from the Banmauk–Kawlin area (northern Myanmar) are presented. Precise zircon U–Pb dating results indicate that they emplaced at Cretaceous (~ 110–90 Ma) and likely belong to an eastward extension of...
1 CitationsSource
#1Peiping Song (CAS: Chinese Academy of Sciences)H-Index: 6
#2DINGLin (CAS: Chinese Academy of Sciences)H-Index: 48
Last. Jing Xie (CAS: Chinese Academy of Sciences)
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#1Saif-Ur-Rehman K. Jadoon (CAS: Chinese Academy of Sciences)
#2DINGLin (CAS: Chinese Academy of Sciences)H-Index: 48
Last. Muhammad Owais Zaib (CUI: COMSATS Institute of Information Technology)
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Abstract Surface geological (field and Landsat images) and subsurface geophysical (seismic reflection and borehole) data were analyzed for geometry and development of N-S oriented frontal Zindapir anticlinorium in the Sulaiman Range, Pakistan. The anticlinorium with its four segments of structural relief (salients), north to south as Dhodak, Rodho, Affiband, and Zindapir, extends over about 130 km with east-vergence of the fold axis, of general NS trend, highly oblique to the plate convergence v...
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#1Zhenyu Li (CAS: Chinese Academy of Sciences)H-Index: 6
#2DINGLin (CAS: Chinese Academy of Sciences)H-Index: 48
Last. Yahui Yue (CAS: Chinese Academy of Sciences)H-Index: 15
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Abstract The magnitude and timing of deformation in the form of vertical-axis rotation in the eastern Tibetan Plateau and Southeast Asia during the Cenozoic period are the key to understanding the India-Asia collision and subsequent geological processes. Our new paleomagnetic and geochronological data from Myanmar show that the characteristic remanent magnetization (ChRM) mean directions of sedimentary tuffaceous layers (31 effective specimens) and rhyolites (11 paleomagnetic site-mean direction...
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#1Yaofei Chen (CAS: Chinese Academy of Sciences)
#2DINGLin (CAS: Chinese Academy of Sciences)H-Index: 48
Last. Yahui Yue (CAS: Chinese Academy of Sciences)H-Index: 15
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Abstract Mesozoic strata along northern margin of the Lhasa terrane near Dingqing, Tibet provide a semi-continuous record of the Bangong-Nujiang Ocean closure and the subsequent Lhasa-Qiangtang collision. In this study, we present results of sandstone petrographic, detrital zircon U Pb, and Cr-spinel geochemical data to determine the provenance of the Mesozoic strata (from the Triassic Quehala Group and the Mid-Jurassic to Lower Cretaceous Xihu, Lagongtang, and Duoni Formations, which are young ...
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#1Jin-Xiang Li (CAS: Chinese Academy of Sciences)H-Index: 13
#2Weiming Fan (CAS: Chinese Academy of Sciences)H-Index: 58
Last. Kyaing SeinH-Index: 4
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Abstract There is a strong controversy about the petrogenesis of tourmaline nodules and their relationship with coeval tourmaline-bearing granites, which are commonly associated with magmatic-hydrothermal rare metal deposits (e.g., Sn, Nb, and Ta). In this study, tourmaline is extensively distributed in tourmaline-bearing nodules (NT-type), pegmatite (PT-type), and fine-grained granitic dyke (GT-type), which are hosted by the Late Cretaceous Nattaung biotite granite (Myanmar). Zircon U Pb dating...
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#1Umair Khan Jadoon (CAS: Chinese Academy of Sciences)
#2DINGLin (CAS: Chinese Academy of Sciences)H-Index: 48
Last. Muhammad Qasim (CUI: COMSATS Institute of Information Technology)H-Index: 3
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