Zobrazeno 1 - 10
of 388
pro vyhledávání: '"Sun‐Lin Chung"'
Publikováno v:
Communications Earth & Environment, Vol 4, Iss 1, Pp 1-9 (2023)
Abstract Ophiolites occur widely in orogenic belts, yet their origins remain controversial. Here we present a modern example with a geodynamic model from Timor, eastern Indonesia, where Earth’s youngest supra-subduction zone (SSZ)-type ophiolitic f
Externí odkaz:
https://doaj.org/article/4f2bf1fe62bb4d2cb6be408409ee9363
Publikováno v:
Journal of Economic Geology, Vol 14, Iss 4, Pp 175-213 (2022)
In the Shourestan area, 14 kilometers west of Sarbisheh city, in South Khorasan province, volcanic rocks with pyroxene-andesite composition belonging to Eocene-Oligocene are exposed. The constituent minerals of these rocks include plagioclase and pyr
Externí odkaz:
https://doaj.org/article/5fec774e60e2493aa13163380eec5fe4
Autor:
Di-Cheng Zhu, Qing Wang, Roberto F. Weinberg, Peter A. Cawood, Sun-Lin Chung, Yong-Fei Zheng, Zhidan Zhao, Zeng-Qian Hou, Xuan-Xue Mo
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-10 (2022)
Gangdese arc magmatism, Tibet, was initially dominated by fractional crystallization of mantle derived magmas, followed by the remelting of these rocks during collision. These two stages lead to the stratification of the juvenile continental crust
Externí odkaz:
https://doaj.org/article/9bafde4de52647d1810b86a31e9cd69c
Autor:
Meng-Hao Gao, Ping-Ping Liu, Sun-Lin Chung, Qiu-Li Li, Bin Wang, Wei Tian, Xian-Hua Li, Hao-Yang Lee
Publikováno v:
Communications Earth & Environment, Vol 3, Iss 1, Pp 1-11 (2022)
Eocene to Oligocene age Himalayan zircons were transported through the Bengal submarine channel, subducted in the Sunda trench, and resurfaced in the arc volcanoes of Sumatra, according to U-Pb-Hf-O isotopes from arc basalts and andesites
Externí odkaz:
https://doaj.org/article/32de944e9fae4b59b406befd1d7ed952
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
The Taiwan mountain belt is the result of an arc-continent collision following the total subduction of the South China Sea and subsequent closure of the Luzon forearc, a process important in the accretionary growth of continents. Due to the oblique c
Externí odkaz:
https://doaj.org/article/6801947e5d084bd388d3e1abd0d1b32b
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 3, Pp n/a-n/a (2023)
Abstract The evolution of the Taiwan orogen, an active arc–continent collision zone between the North Luzon Arc (NLA) and the Eurasian continent, is recorded in arc volcanic and sedimentary rocks from the Taiyuan retro‐foredeep basin of the Coast
Externí odkaz:
https://doaj.org/article/21c4b5f7656f4ceb8d58d0f077d771b0
Publikováno v:
پترولوژی, Vol 11, Iss 4, Pp 1-28 (2021)
In Tighanab area at southeast of Sarbisheh, the intrusion of quartzdioritic subvolcanic bodies into the Paleocene- Eocene limestone and sandstone led to the skarn formation. Plagioclase, hornblende (magnesiohornblende) and quartz are the main mineral
Externí odkaz:
https://doaj.org/article/9c29d4351c1b44afaba61204984c9045
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 31, Iss 4, Pp 383-402 (2020)
Ophiolite-bearing belts mark convergent plate suture zones and are central in reconstructing plate configuration and structures of mountain belts. The active Taiwan mountain belt, product of ongoing convergence between the Eurasian and Philippine Sea
Externí odkaz:
https://doaj.org/article/ef125cc2edbd4dca8c30b44e626ecfdc
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 29, Iss 2, Pp 149-186 (2018)
The complete volcanic sequences restored in the Coastal Range of Taiwan are key archives for better understanding the magmatic and tectonic evolution of the Northern Luzon Arc. This paper reports (1) new zircon U-Pb ages and Hf isotopic data of fourt
Externí odkaz:
https://doaj.org/article/b3678abc72024600a26026a2a7737ac6
Autor:
Chin-Da Huang, Tung-Yi Lee, Ching-Hua Lo, Sun-Lin Chung, Jong-Chang Wu, Ching-Lung Tien, Meng-Wan Yeh, Shiu-Chi Chen, Yu-Lu Chan, Ching-Yi Hu
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 28, Iss 6, Pp 891-922 (2017)
The northern South China Sea (SCS) continental margin was proposed to be an active margin during the Mesozoic. However, only a few papers discussed the Mesozoic structural evolution in this region. Here, we provide information based on the seismic pr
Externí odkaz:
https://doaj.org/article/787bdcb89b0b46e3946b03bab218c9a3