Matches in SemOpenAlex for { <https://semopenalex.org/work/W4214542279> ?p ?o ?g. }
- W4214542279 endingPage "103973" @default.
- W4214542279 startingPage "103973" @default.
- W4214542279 abstract "The Jurassic subduction of the Bangong-Nujiang Tethys Ocean is recognized as a significant event in the geotectonic evolution of Tibetan Plateau. This study focuses on the Mesozoic ophiolites, magmatic rocks, sedimentary strata, and metamorphic features, and discusses their relationship with the evolution of the Bangong-Nujiang Ocean. Two stages of Jurassic northward subduction are identified. The first stage is represented by the Early Jurassic subduction of the Amdo-Jiayuqiao subterrane. Slab break-off triggered the Middle-Late Jurassic exhumation of the subducted subterrane as well as the eclogite and high-pressure granulite. This process promoted the initiation of the second stage subduction at the southern margin of the South Qiangtang and Amdo-Jiayuqiao subterranes. For the western-central Bangong-Nujiang Ocean, we interpret the second stage as flat or shallow angle subduction and suggested that it was triggered by break-off of the subducted slab. The Bangong-Nujiang Tethys Ocean experienced southward ocean-continent and intra-oceanic subduction in the eastern and central-western segments, respectively, which are represented by the Shiquanhe-Yongzhu-Jiali mélange zone. The western and central-eastern segments of the Shiquanhe-Yongzhu-Jiali oceanic basin represented an immature to mature back-arc basin. The Bangong-Nujiang Ocean experienced a complex subduction evolution during Jurassic. Both northward and southward subduction zones were initiated during Late Triassic perhaps in response to the closure of the Paleo-Tethys oceans to the south and north." @default.
- W4214542279 created "2022-03-02" @default.
- W4214542279 creator A5002055049 @default.
- W4214542279 creator A5004716253 @default.
- W4214542279 creator A5041468811 @default.
- W4214542279 creator A5042150647 @default.
- W4214542279 creator A5042950207 @default.
- W4214542279 creator A5046703638 @default.
- W4214542279 creator A5052146259 @default.
- W4214542279 creator A5063036305 @default.
- W4214542279 creator A5066207013 @default.
- W4214542279 creator A5075946154 @default.
- W4214542279 creator A5082580072 @default.
- W4214542279 creator A5090862153 @default.
- W4214542279 date "2022-04-01" @default.
- W4214542279 modified "2023-10-01" @default.
- W4214542279 title "Jurassic tectonic evolution of Tibetan Plateau: A review of Bangong-Nujiang Meso-Tethys Ocean" @default.
- W4214542279 cites W1064157222 @default.
- W4214542279 cites W1529815382 @default.
- W4214542279 cites W1579920087 @default.
- W4214542279 cites W1834059286 @default.
- W4214542279 cites W1906201844 @default.
- W4214542279 cites W1968971801 @default.
- W4214542279 cites W1970363584 @default.
- W4214542279 cites W1975539648 @default.
- W4214542279 cites W1977085539 @default.
- W4214542279 cites W1981084711 @default.
- W4214542279 cites W1986335413 @default.
- W4214542279 cites W1989940712 @default.
- W4214542279 cites W1991232046 @default.
- W4214542279 cites W1994354262 @default.
- W4214542279 cites W1996228785 @default.
- W4214542279 cites W2004780129 @default.
- W4214542279 cites W2019748000 @default.
- W4214542279 cites W2029643225 @default.
- W4214542279 cites W2032016952 @default.
- W4214542279 cites W2033542443 @default.
- W4214542279 cites W2034397592 @default.
- W4214542279 cites W2036484456 @default.
- W4214542279 cites W2042407855 @default.
- W4214542279 cites W2042425755 @default.
- W4214542279 cites W2042806383 @default.
- W4214542279 cites W2047938785 @default.
- W4214542279 cites W2052579497 @default.
- W4214542279 cites W2058866622 @default.
- W4214542279 cites W2062347763 @default.
- W4214542279 cites W2065520860 @default.
- W4214542279 cites W2067685960 @default.
- W4214542279 cites W2068157565 @default.
- W4214542279 cites W2068668821 @default.
- W4214542279 cites W2069874655 @default.
- W4214542279 cites W2071483826 @default.
- W4214542279 cites W2081441976 @default.
- W4214542279 cites W2081820875 @default.
- W4214542279 cites W2091484047 @default.
- W4214542279 cites W2092629476 @default.
- W4214542279 cites W2094727526 @default.
- W4214542279 cites W2098454380 @default.
- W4214542279 cites W2105111360 @default.
- W4214542279 cites W2106006247 @default.
- W4214542279 cites W2109373726 @default.
- W4214542279 cites W2113274161 @default.
- W4214542279 cites W2114856901 @default.
- W4214542279 cites W2115518283 @default.
- W4214542279 cites W2121843968 @default.
- W4214542279 cites W212707111 @default.
- W4214542279 cites W2130613780 @default.
- W4214542279 cites W2135830789 @default.
- W4214542279 cites W2136912344 @default.
- W4214542279 cites W2138793204 @default.
- W4214542279 cites W2144625273 @default.
- W4214542279 cites W2146515386 @default.
- W4214542279 cites W2146762922 @default.
- W4214542279 cites W2151685608 @default.
- W4214542279 cites W2165074973 @default.
- W4214542279 cites W2170021670 @default.
- W4214542279 cites W2173595212 @default.
- W4214542279 cites W2175941682 @default.
- W4214542279 cites W2184783801 @default.
- W4214542279 cites W2217851887 @default.
- W4214542279 cites W2225392346 @default.
- W4214542279 cites W2257736200 @default.
- W4214542279 cites W2285539797 @default.
- W4214542279 cites W2298520685 @default.
- W4214542279 cites W2342445191 @default.
- W4214542279 cites W2396231960 @default.
- W4214542279 cites W2465551923 @default.
- W4214542279 cites W2468980968 @default.
- W4214542279 cites W2489149528 @default.
- W4214542279 cites W2491226624 @default.
- W4214542279 cites W2515388358 @default.
- W4214542279 cites W2519498575 @default.
- W4214542279 cites W2541081601 @default.
- W4214542279 cites W2551715547 @default.
- W4214542279 cites W2562243389 @default.
- W4214542279 cites W2589732894 @default.
- W4214542279 cites W2594221245 @default.
- W4214542279 cites W2609114354 @default.