Northward subduction of the South Qilian ocean: Insights from early Paleozoic magmatism in the South-Central Qilian belts

Autor: Jianping Zheng, Yilong Li, Fraukje M. Brouwer, Wenjiao Xiao

Publikováno v: Geosystems and Geoenvironment, 1(1):100013, 1-10. Elsevier
Li, Y, Xiao, W, Zheng, J & Brouwer, F M 2022, ' Northward subduction of the South Qilian ocean: Insights from early Paleozoic magmatism in the South-Central Qilian belts ', Geosystems and Geoenvironment, vol. 1, no. 1, 100013, pp. 1-10 . https://doi.org/10.1016/j.geogeo.2021.100013
Geosystems and Geoenvironment, Vol 1, Iss 1, Pp 100013-(2022)

The Qilian orogen consists of the North Qilian belt, the Central Qilian block and the South Qilian belt and is regarded as part of the northern margin of the Proto-Tethys Ocean. The tectonic mechanism responsible for the early Paleozoic magma generat

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a6821c991acefdde8c885f572803b564
https://research.vu.nl/en/publications/b9bdbcba-8f27-4794-ba20-12d436a9c81f

An origin of ultraslow spreading ridges for the Yarlung-Tsangpo ophiolites

Autor: Tong Liu, Fu-Yuan Wu, Zhen-Yu Zhang, Wu Wei, Y. Lin, Chuan-Zhou Liu, Wei-Qi Zhang, Zhen Zhang, Chang Zhang

Publikováno v: Fundamental Research. 2:74-83

As relics of ancient ocean lithosphere, ophiolites are the most important petrological evidence for marking the sutures and also play a key role in reconstructing plate configuration. They also provide valuable windows for studying crustal accretion

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5db57d2898df104ad1342540e677334b
https://doi.org/10.1016/j.fmre.2021.07.002

Boninitic blueschists record subduction initiation and subsequent accretion of an arc–forearc in the northeast Proto-Tethys Ocean

Autor: Tim E. Johnson, Ali Polat, Fred Jourdan, Timothy M. Kusky, Bo Huang, Zhaochu Hu, Dong Fu, Simon A. Wilde, Brian F. Windley

Publikováno v: Geology. 50:10-15

Subduction of oceanic lithosphere is a diagnostic characteristic of plate tectonics. However, the geodynamic processes from initiation to termination of subduction zones remain enigmatic mainly due to the scarcity of appropriate rock records. We repo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::03b40ee0f9d1d77ee3d427b855c860e9
https://doi.org/10.1130/g49457.1

The great Yanshanian metallogenic event of eastern Asia: Consequences from one hundred million years of plate margin geodynamics

Autor: Jingwen Mao, Richard J. Goldfarb, Kun-Feng Qiu, N. S. Goryachev

Publikováno v: Gondwana Research. 100:223-250

Yanshanian (ca. 200–100 Ma) metallogeny of eastern Asia was dominantly controlled by oblique subduction and rollback of the Izanagi plate, and also, more locally in the north, by closure of the Mudanjiang Ocean basin and accretion of the Bureya-Jia

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::03b62da243028d979649376b2a98d246
https://doi.org/10.1016/j.gr.2021.02.020

Sediment provenance, routing and tectonic linkages in the Nankai forearc region, Japan

Autor: Nicholas W. Hayman, Sean P. S. Gulick, Kitty L. Milliken, Daniel F. Stockli, S. G. Ramirez, H. Masago

Publikováno v: Basin Research. 33:3231-3255

Understanding sedimentary routing systems at continental margins can be challenging in tectonically active regions such as forearc basins. Here, we combine sand modal composition and detrital zircon U‐Pb data from the Kumano Basin and surrounding N

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::6d13f57e0fb7498eaa172e3e2b7ca8a4
https://doi.org/10.1111/bre.12601