supported by the National Natural Science Foundation of China(Grant No.91955204);National Major Science and Technology Project of China(Grant No.2016ZX05004001)。
Geodynamic drivers for the supercontinent cycle are generally attributed to either top-down(subduction-related)or bottom-up(mantle-related)processes.Compiled geochemical data and U-Pb ages and Hf isotopic signatures f...
jointly supported financially by the National Natural Science Foundation of China(No.41603040);the Natural Science Basic Research Plan in Shaanxi Province of China(No.2023-JC-YB-239);Fundamental Research Funds for the Central Universities(S202310710204)。
The Bijigou intrusion is one of the largest and most well-differentiated Fe–Ti oxide-bearing layered intrusions in the Hannan massif located in the northwestern margin of the Yangtze Block,South China.Besides the min...
We investigate the evolution of stress fields during the supercontinent cycle using the 2D Cartesian geometry model of thermochemical convection with the non-Newtonian rheology in the presence of floating deformable c...
supported by the National Natural Science Foundation of China(Grant No.40072065);MSBRPC(Grant No.2001CB409804).
Granitoid gneisses are widespread in Precambrian metamorphic blocks of eastern segment of the Central Tianshan Tectonic Zone, and they have intrusive contact relationships with their metamorphic sedimentary country ro...
supported by the National Natural Science Foundation of China(Grant No.41872080);the National Basic Research Program of China(Grant No.2015CB452603);the MOST Special Fund from the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences(Beijing)(Grant No.MSFGPMR201804);and the Fundamental Research Funds for the Central Universities of China(Grant Nos.2652016077,2652017223)
The volcanic rocks of the Xiong’er Group are situated in the southern margin of the North China Craton(NCC).Research on the Xiong er Group is important to understand the tectonic evolution of the NCC and the Columbia...
The paper is supported by Key Project ( No .104039) and Special Doc-toral Project (No .20050491506) from the Ministry of Education , China ,the Open Research Program of the Key Laboratory of Continental Dynamics , Northwest University ,and NSFC Special Grant for National Education Base of Geology (No .J0530147) .
U-Pb dating was conducted on different domains of zircons from metamorphosed leucosomes in Delingha ( 德令哈) complex, the lower basement rocks of the Olongbuluke (欧龙布鲁克 ) microcontinent, North Qaidam, in or...
partly supported by a Grant-in-Aid for Scientific Research(B)from Japan Society for the Promotion of Science(JSPS)(No.26302009);by the NIPR General Collaboration Projects(No.26-34)to Tsunogae
The Lützow-Holm Complex(LHC) of East Antarctica has been regarded as a collage of Neoarchean(ca.2.5 Ga), Paleoproterozoic(ca. 1.8 Ga), and Neoproterozoic(ca. 1.0 Ga) magmatic arcs which were amalgamated through the l...
Reconstruction of the Neoproterozoic supercontinent Rodinia shows near neighbour positions of the South Indian Cratons and Western Australian Cratons. These cratonic areas are characterized by extensive Paleoproterozo...
The evolution of the earth is marked by development of more than 70% of the present day continents during Archean. The Archean - Proterozoic boundary is characterized by continental amalgamation, and subsequent breaki...