Matches in SemOpenAlex for { <https://semopenalex.org/work/W2936624770> ?p ?o ?g. }
- W2936624770 endingPage "55" @default.
- W2936624770 startingPage "37" @default.
- W2936624770 abstract "The Proto-South China Sea (PSCS) represents the lithosphere that formerly occupied the region southeast of South China where the present-day South China Sea is located. The subduction and demise of the PSCS have attracted wide attention, whereas the pre-subduction history (particular the Mesozoic) of the region remains relatively neglected. In this paper, the radiolarian paleobiogeography of the region is analyzed to identify the paleobiogeographic affinity and paleo-connectivity of the PSCS with the Pacific and Tethys oceans during the Mesozoic. Then the continent–ocean configuration and tectonic evolution of the PSCS and adjacent areas are discussed through the integration of paleobiogeographical results and associated paleomagnetic, stratigraphic, and petrologic data. The main conclusions are as follows: (1) During the Triassic, the PSCS was situated in the transition zone between the Pacific and Tethys oceans, and its paleobiogeography was influenced by both oceans. The PSCS was characterized by complex tectonic overprinting by the Pacific and Tethyan tectonic regimes. (2) In the Early–Middle Jurassic, the PSCS was well connected to the Pacific Ocean but poorly connected to the Tethys Ocean, consistent with the paleobiogeography of the PSCS being mainly constrained by the Pacific Ocean. The PSCS was part of the Paleo-Pacific slab. (3) During the Late Jurassic–Cretaceous, the PSCS was in a semi-closed environment. The Late Jurassic–early Late Cretaceous PSCS was part of a west-facing Andean-type subduction zone, and the late Late Cretaceous PSCS was situated in an extensional tectonic setting." @default.
- W2936624770 created "2019-04-25" @default.
- W2936624770 creator A5000586279 @default.
- W2936624770 creator A5016039392 @default.
- W2936624770 creator A5016061503 @default.
- W2936624770 creator A5020724652 @default.
- W2936624770 creator A5072055282 @default.
- W2936624770 date "2019-08-01" @default.
- W2936624770 modified "2023-09-23" @default.
- W2936624770 title "Mesozoic tectonic evolution of the Proto-South China Sea: A perspective from radiolarian paleobiogeography" @default.
- W2936624770 cites W1100243556 @default.
- W2936624770 cites W1441480832 @default.
- W2936624770 cites W1486347736 @default.
- W2936624770 cites W1505323387 @default.
- W2936624770 cites W1525258218 @default.
- W2936624770 cites W1552980575 @default.
- W2936624770 cites W1586275029 @default.
- W2936624770 cites W1592076167 @default.
- W2936624770 cites W1601210198 @default.
- W2936624770 cites W1618640913 @default.
- W2936624770 cites W1628621943 @default.
- W2936624770 cites W1781864697 @default.
- W2936624770 cites W1850129459 @default.
- W2936624770 cites W1953870425 @default.
- W2936624770 cites W1963903618 @default.
- W2936624770 cites W1963972264 @default.
- W2936624770 cites W1965325889 @default.
- W2936624770 cites W1965917434 @default.
- W2936624770 cites W1966310156 @default.
- W2936624770 cites W1973612594 @default.
- W2936624770 cites W1976033346 @default.
- W2936624770 cites W1977636777 @default.
- W2936624770 cites W1984638803 @default.
- W2936624770 cites W1986951585 @default.
- W2936624770 cites W1987845890 @default.
- W2936624770 cites W1989602494 @default.
- W2936624770 cites W1989816828 @default.
- W2936624770 cites W1992369722 @default.
- W2936624770 cites W1992680913 @default.
- W2936624770 cites W1997816021 @default.
- W2936624770 cites W1998671119 @default.
- W2936624770 cites W2001117061 @default.
- W2936624770 cites W2001239331 @default.
- W2936624770 cites W2003738035 @default.
- W2936624770 cites W2003954276 @default.
- W2936624770 cites W2005400568 @default.
- W2936624770 cites W2010967771 @default.
- W2936624770 cites W2012942615 @default.
- W2936624770 cites W2013013399 @default.
- W2936624770 cites W2013103945 @default.
- W2936624770 cites W2015590982 @default.
- W2936624770 cites W2017312495 @default.
- W2936624770 cites W2017836817 @default.
- W2936624770 cites W2018248405 @default.
- W2936624770 cites W2018660358 @default.
- W2936624770 cites W2019281111 @default.
- W2936624770 cites W2019751696 @default.
- W2936624770 cites W2021331774 @default.
- W2936624770 cites W2023273714 @default.
- W2936624770 cites W2024781959 @default.
- W2936624770 cites W2026225462 @default.
- W2936624770 cites W2026430737 @default.
- W2936624770 cites W2029180950 @default.
- W2936624770 cites W2032331952 @default.
- W2936624770 cites W2034397592 @default.
- W2936624770 cites W2034463147 @default.
- W2936624770 cites W2036484456 @default.
- W2936624770 cites W2036621031 @default.
- W2936624770 cites W2036810711 @default.
- W2936624770 cites W2036837579 @default.
- W2936624770 cites W2038544394 @default.
- W2936624770 cites W2039722155 @default.
- W2936624770 cites W2042634809 @default.
- W2936624770 cites W2045483810 @default.
- W2936624770 cites W2045778422 @default.
- W2936624770 cites W2045878430 @default.
- W2936624770 cites W2048068769 @default.
- W2936624770 cites W2048271710 @default.
- W2936624770 cites W2048833021 @default.
- W2936624770 cites W2049097219 @default.
- W2936624770 cites W2049621460 @default.
- W2936624770 cites W2053439268 @default.
- W2936624770 cites W2053922121 @default.
- W2936624770 cites W2055334012 @default.
- W2936624770 cites W2058150587 @default.
- W2936624770 cites W2058269792 @default.
- W2936624770 cites W2058314706 @default.
- W2936624770 cites W2060003735 @default.
- W2936624770 cites W2065616667 @default.
- W2936624770 cites W2066025065 @default.
- W2936624770 cites W2066711037 @default.
- W2936624770 cites W2067871313 @default.
- W2936624770 cites W2068365898 @default.
- W2936624770 cites W2072697389 @default.
- W2936624770 cites W2074440625 @default.
- W2936624770 cites W2075743454 @default.
- W2936624770 cites W2077232184 @default.
- W2936624770 cites W2079149334 @default.