Zobrazeno 1 - 10
of 80
pro vyhledávání: '"Wen-Chun Ge"'
Publikováno v:
Geological Magazine. 159:1513-1528
Late Palaeozoic igneous rock associations in response to subduction, accretion, and final closure of the eastern Palaeo-Asian Ocean play a significant role in understanding the geodynamic evolution of the southeastern Central Asian Orogenic Belt. Pre
Publikováno v:
Canadian Journal of Earth Sciences. 59:325-345
In this study, we undertook zircon U–Pb dating and Hf isotopic and whole-rock geochemical analysis of Mesozoic granites from the Zhalantun and Arxan areas of the Great Xing’an Range, northeastern China. Zircon U–Pb dating of four samples indica
Figure S1: Photographs (A) and photomicrographs (B) of Weilasituo ZK granites. Figure S2: Photographs of Weilasituo ZK granites. Figure S3: Photomicrographs of Weilasituo (A–C) BD granites and (D–I) ZK granites. Figure S4: Photomicrographs of (A)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5255cebd330a639b211f518a774910eb
https://doi.org/10.1130/gsab.s.22745336.v1
https://doi.org/10.1130/gsab.s.22745336.v1
Publikováno v:
GSA Bulletin.
Much controversy exists regarding the evolution and termination of accretionary orogens where typical continent-continent collision features are lacking. The Central Asian Orogenic Belt provides a key opportunity to explore the genetic relationships
Publikováno v:
Gondwana Research. 103:297-313
Intra-oceanic arcs are potential candidates that generate Earth’s continental crust, and serve as active sites for the mixing of juvenile arc and mature continental material. However, whether continental fragments occur beneath intra-oceanic arcs,
Publikováno v:
Gondwana Research. 103:146-171
There is a broad consensus that the Solonker suture zone marked the final closure of the eastern Paleo-Asian Ocean, which led to the formation of the eastern segment of the Central Asian Orogenic Belt (CAOB). However, when and how the final closure o
Autor:
Wen-chun Ge, Yan Jing
Text: Methods. Figure S1: Diagrams showing chondrite-normalized REEs patterns for zircons from the high-Mg igneous associations in the Qinghe region. Figure S2: Diagrams showing variation of selected elements vs. LOI to check for element mobility dur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bb6e9de43fa27e1f627a4404820bfb55
https://doi.org/10.1130/gsab.s.21445281.v1
https://doi.org/10.1130/gsab.s.21445281.v1
Autor:
Guan-Ying Yu, Hao Yang, Jia-Hao Jing, Xin Ding, Zheng Ji, Yan-Long Zhang, Yu Dong, Wen-chun Ge
Publikováno v:
Lithos. :107141
Publikováno v:
Geological Magazine. 158:1617-1638
Late Mesozoic igneous rocks are important for deciphering the Mesozoic tectonic setting of NE China. In this paper, we present whole-rock geochemical data, zircon U–Pb ages and Lu–Hf isotope data for Early Cretaceous volcanic rocks from the Tulih
Publikováno v:
International Geology Review. 64:564-595
There is a broad consensus that subduction of the Paleo-Pacific oceanic plate has caused extensive magmatism, lithospheric deformation, and metal mineralization in the eastern margin of the Eurasia...