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Your search keyword '"Danzeng, Awang"' showing total 8 results
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8 results on '"Danzeng, Awang"'

5. Does inclusion of bioactive n-3 PUFAs in parenteral nutrition benefit postoperative patients undergoing liver surgery? A systematic review and meta-analysis of randomised control trials

Author

He, Zheng-Wei, primary, Wang, Chao, additional, Li, Yong, additional, Danzeng, Awang, additional, Liu, Fu-Bin, additional, Shi, Jia-Yu, additional, Ciren, Pingcuo, additional, Yuan, Xiao-Yin, additional, Wu, Cheng-Xian, additional, Lan, Run-hu, additional, and Zhang, Bin-Hao, additional

Published
2023
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6. Anatomical Resection Improved the Outcome of Intrahepatic Cholangiocarcinoma: A Propensity Score Matching Analysis of a Retrospective Cohort

Author

Wang, Chao, primary, Ciren, Pingcuo, additional, Danzeng, Awang, additional, Li, Yong, additional, Zeng, Cheng-Long, additional, Zhang, Zhi-Wei, additional, Huang, Zhi-Yong, additional, Chen, Yi-Fa, additional, Zhang, Wan-Guang, additional, Zhang, Bi-Xiang, additional, Zhang, Bin-Hao, additional, and Chen, Xiao-Ping, additional

Published
2022
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8. Dating of detrital zircon grains and fossils from Late Palaeozoic sediments of the Baruo area, Tibet: constraints on the Late Palaeozoic evolution of the Lhasa terrane.

Author

Wang, Ming, Zeng, Xiao-wen, Xie, Chao-Ming, Danzeng, Awang, Li, Cai, Fan, Jian-Jun, and Li, Hang

Subjects
GONDWANA (Continent), ZIRCON, FOSSILS, CLASTIC rocks, GRAIN, OROGENIC belts, PALEOGEOGRAPHY
Abstract

To determine the Late Palaeozoic evolution of the Lhasa terrane, we report the results of field mapping, petrological and fossil investigations, and U–Pb dating of detrital zircon grains (n = 474) from lower-greenschist-facies clastic rocks of the Lagar Formation in the Baruo area, Tibet. Our results indicate that the Lagar Formation was deposited during the Late Carboniferous to Early Permian in a shallow-marine environment on the northern margin of Gondwana. Glacial marine diamictites are common within the Lagar Formation and record glaciation of Gondwana during the Late Palaeozoic. Moreover, the detrital materials of the Lagar formation originated mostly from the collision orogenic belt. The ages of detrital zircon grains from the Lagar Formation make up five main groups with ages of 410–540 Ma, 550–650 Ma, 800–1100 Ma, 1600–1800 Ma, and 2300–2500 Ma, which display three characteristic age peaks at ~1150, 2390 and 2648 Ma. We tentatively suggest that the Lhasa terrane was a shallow-marine basin under the influence of the Gondwanan glaciation during the Late Carboniferous–Early Permian. [ABSTRACT FROM AUTHOR]

Published
2020
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