funded by the National Natural Science Foundation of China(Nos.42007280,42372339);the China Geological Survey Project(No.DD20221816).
The upstream Jinsha River,located in the eastern Tibetan Plateau,has been experiencing intense geological hazards characterized by a high density of ancient landslides,significant deformation and reactivation challeng...
supported by the National Natural Science Foundation of China(Nos.41572002,41830320,and 41661134047)。
Focusing on the Shuixiakou Section(Xikou area,Zhen’an County,Shaanxi Province,southeastern Qinling region,China),the Roadian-Wordian conodonts are investigated.More than 2000 conodont elements including 6 genera and ...
funded by the National Natural Science Foundation of China(Nos.41972033,41830320,41572324)。
The Nanpanjiang Basin is a key area for paleontological and biostratigraphical study of the Middle Triassic.Herein we studied Middle Triassic conodonts from a well-exposed section,the Shaiwa Section,which is located a...
supported by the National Natural Science Foundation of China(Nos.41830320,45172002,41661134047)。
Based on a study of 49 conodont and 57 geochemical samples from the Upper Triassic,carbonate-dominated Dengdengqiao Formation,Qinling Basin,China,the Carnian conodonts and carbon isotope records are first reported.Two...
supported by the grants PRIN to Manuel Rigo(No.2017W2MARE);the China Scholarship Council to Yixing Du(No.201708510096);Development of conodont oxygen isotopic analysis by SHRIMP was supported by Australian Research Council Discovery to Ian S.Williams(No.DP1096252)。
During their last phase of evolution,the pectiniform conodont elements manifested an evident trend of simplification and miniaturization.This phase started from the late Norian(Sevatian)in the Late Triassic and the ev...
supported by the National Natural Science Foundation of China (No. 41302021);the Science and Technology Research Project of Jiangxi Province Education Department (No. GJJ13452);Research by Hao Yu is supported by the National Natural Science Foundation of China (No. 41290260);the Ministry of Education of China (No. 20120001110052)
The Late Paleozoic Ice Age across Carboniferous and Permian had a significant impact on the Kungurian (Upper Cisuralian series of Permian) Chihsia Formation in South China. This re- suited in a unique interval with ...
supported by the Natural Science Foundation of China (Nos. 41372039, 41272044, 41172024);the ‘Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan)’
A continuous sedimentation at the Xinmin Section, Anshun, Guihzou Province, with the Upper Permian Talung Formation dominated by bedded siliceous rocks, and the Lower Triassic Luolou Formation consisting mudstones and...
supported by the National Natural Science Foundation of China(No.41372039)
In the Early Ordovician Zhaogezhuang Section of Tangshan , North China, the Yeli Formation is composed of an entire third-order sequence, with facies ranging from the inner ramp restricted platform and open marine t...
supported by the SINOPEC Forward Looking Projects of China (Nos. YPH08114 and 2009026324)
In Changxing (长兴) stage, Manyue (满月)-Honghua (红花) Section of Kaixian (开县), northeastern Sichuan (四川) Province was located in the platform-margin slope, which was the advantage area of reef-shoal de...
supported by the National Major Science and Technology Project of China (No. 2011ZX05007-002)
The Changxing (长兴) Formation has two sequences (sql and sq2) in the Panlongdong (盘龙洞) Section, Xuanhan (宣汉), northeastern Sichuan (四川). It belongs to the platform edge facies belt, rich in reefs and...