Duan Liang

Professional:Professor

Department:Petrology & Mineralogy Teaching and Research Office

Direction:Sedimentology and Basin Analysis

Email:duanl@nwu.edu.cn

Sedimentary geology is committed to understanding the formation and evolution process of the Earth's shallow surface, with a focus on understanding the impact of sedimentary processes from multiple layers and a global perspective. Response and mutual feedback to major geological events; It is one of the key foundational disciplines supporting the formation of a livable Earth, the coordinated evolution of Earth Environment Life, and the exploration and development of various mineral resources. We attempt to uncover the ups and downs that Mother Earth has experienced throughout its long history through various spectacular, exquisite, and plain sedimentary records. I hope to have the opportunity to get close to nature with interested classmates and experience the beautiful rivers and mountains of our motherland and around the world


Duan Liang, male, doctoral supervisor.

Institute of Geology and Geophysics, Chinese Academy of Sciencescurrently undertakes theSedimentary Geology,Sedimentary Petrology,Earth System ScienceTo engage inbasin evolutionand crustal deformation Research on the response and mutual feedback of sea level rise and fall in the evolution of life. He has successively presided over the projects of the State Key Laboratory of Continental Dynamics, the Young Scientists Fund of the National Natural Science Foundation of China, general projects and national major special tasks, and is the main person who completed or participated in national level projects such as the NSFC's innovative research group project, the major research program integration project of "Tethys Geodynamics", key funds, strategic research projects, and the national key research and development program "Deep Earth Special" tasks

Published more than 20 academic papers, including 11 journal papers by first/corresponding authors such as Basin Research and GSA Bulletin, as well as Tim, the coordinator of Elsevier's geosciences review paper.; Horscroft invited me to write one focus review paper on Gondwana Research. Served as a communication and evaluation expert for the National Science Foundation, Youth Fund, and Regional Science Fund, as well as for Tectonics, Basin Res., Gondwana Res., J. Division Res., Paleo3, J. Geol, J. Asian; Earth Sci, Geosystems and Geoenvironment, Palaeoworld, reviewer for journals such as the Chinese Journal of Earth Sciences and Sedimentary Sciences. Current editorial board member of Geosystems and Environment and young editorial board member of Geological Bulletin


Published articles:

Wang, B., Huang, B., Yang, Z., Zhang, G. Liu, X., Duan, L.,; Armstrong, R., Meng, Q., 2024 Paleomagnetic results from Early Mesozoic strata in the Qaidam Basin and their implications for the formation of the Northern China Domain, Geophysical Journal International, ggad496 https://doi.org/10.1093/gji/gg ad496

Duan, L. *,; Meng, Q.R.,  Zhang, R.,  Wei, R.H., 2023; Detrial record of sedimentation flux in the Triasic Chuxing broker foreland and basin in the Southern Titanium Plateau& Nbsp; Palaeography, Palaeoclimatology, Palaeoecology 632, 111864 https://doi.org/10.1016/j.palaeo.2023.1 11864

Duan, L. *, Christie Blick, N.,  Meng, Q.R.,  Wu, G.L.,  Yang, Z., Wang, B., 2023; A back arc transitional origin for the Nanjiang basin in the pre Northern Triassic, with implications for the broad internal development of South China Basin Research 35, 551-571 https://doi.org/10.1111/bre.12722.

Wei, R.H., Duan, L. *,; Zhang, X.L.,  Meng, Q.R.,  Zhang, R., Ma, C.X., Xu, J., Shi, Y., Zhang, X.Y., 2023; Detrial zircon age signatures of the Basal Cambrian sandstone unit in North China: implications for drainage divisions during global Sauk transgression and separation from Gondwanaland International Geology Review& Nbsp https://doi.org/10.1080/00206814.2022.2098541

Liu, W; Zhang, X.L., < Duan, L.,  Chang, C.,  Liu, X., 2022; Rain shower on a Cambrian mudflat Science Bulletin 67, 2522

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