Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Xiangkuan Gong"'
Autor:
Xiangkuan Gong, Nijiati Abuduxun, Xiaoliang Jia, Yuanfeng Cheng, Hongming Cai, Xueqian Wu, Haodong Yang
Publikováno v:
Frontiers in Earth Science, Vol 12 (2024)
Introduction: The early Jurassic granitoids in the Qinling Orogenic Belt (QOB) play a crucial role in understanding the tectonic implications for the geological evolution of China. To elucidate the early Jurassic tectonic setting of QOB, we performed
Externí odkaz:
https://doaj.org/article/bb8c4a1c08c444248b38a613f82e5017
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Introduction: To provide constraints on the Triassic tectonic setting of Eastern Tianshan, an integrated study was conducted on the geochronological and geochemical data for granodiorites, monzogranites, and two-mica granites from the Yamansu area on
Externí odkaz:
https://doaj.org/article/f5bf6a9df34d47c6a528e180a38cd592
Publikováno v:
Geological Journal. 55:7114-7131
Publikováno v:
Journal of Earth Science. 30:323-334
Late Paleozoic mafic-intermediate intrusions are widespread in the central Tianshan belt, but their tectonic settings remain controversial. Petrogenesis of these intrusions can provide insights into the tectonic evolution of the belt and its adjacent
Publikováno v:
Gondwana Research. 42:220-242
Although lawsonite eclogite is predicted to be common at depth of ~ 45–300 km in subduction zones, it is rarely exposed at Earth's surface. In this study, we identified a lawsonite (pseudomorph)-bearing eclogite in Yuka terrane, North Qaidam UHPM b
Publikováno v:
Chinese Science Bulletin. 61:1365-1378
The Qinling orogen lying in between the North and South China blocks is a key for understanding the tectonic framework of China continent. Tectonically, the Qinling orogen is divided into the North Qinling Tectonic Belt (NQTB) and the South Qinling T
Publikováno v:
Precambrian Research. 333:105449
Eclogites documenting two orogenic cycles not only contain essential information on subduction and exhumation mechanisms during the most recent orogenic cycle, but can also provide insights into the earlier cycle. Such rocks are ideal for deciphering