2009
DOI: 10.1007/s12583-009-0001-8
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Tectonics and sedimentary basins of the South China Sea: Challenges and progresses

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Cited by 54 publications
(27 citation statements)
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“…They also feature wide areas of highly thinned, so-called hyperextended crust with a thickness of less than 10 km, where crust and mantle deformation appears to be tightly coupled Mohn et al, 2014]. Well-studied examples of magma-poor margins comprise the Iberia-Newfoundland conjugates [Hopper et al, 2004;Reston, 2007;Ranero and Perez-Gussinye, 2010;Sutra and Manatschal, 2012], the Central South Atlantic segment [Contrucci et al, 2004;Aslanian et al, 2009;Mohriak and Leroy, 2012], the Australian North West Shelf [Karner and Driscoll, 1999], the eastern Gulf of Aden and the South China Sea [Zhou and Yao, 2009;Franke, 2013].…”
Section: Magma-poor and Magma Rich End-membersmentioning
confidence: 99%
“…They also feature wide areas of highly thinned, so-called hyperextended crust with a thickness of less than 10 km, where crust and mantle deformation appears to be tightly coupled Mohn et al, 2014]. Well-studied examples of magma-poor margins comprise the Iberia-Newfoundland conjugates [Hopper et al, 2004;Reston, 2007;Ranero and Perez-Gussinye, 2010;Sutra and Manatschal, 2012], the Central South Atlantic segment [Contrucci et al, 2004;Aslanian et al, 2009;Mohriak and Leroy, 2012], the Australian North West Shelf [Karner and Driscoll, 1999], the eastern Gulf of Aden and the South China Sea [Zhou and Yao, 2009;Franke, 2013].…”
Section: Magma-poor and Magma Rich End-membersmentioning
confidence: 99%
“…It is characterized by a rhombic shape with an oceanic basin in the center surrounded by a passive margin to the north, convergent margins to the east and south, and a transform margin to the west (Hayes and Nissen, 2005;Yan et al, 2006;Zhou and Yao, 2009;Franke et al, 2011) as shown in Fig. 1.…”
Section: Introductionmentioning
confidence: 99%
“…The Taixinan basin is the name most used by Mainland Chinese researchers, based on its location off SW Taiwan (i.e. Zhou & Yao 2009). Recently, it has been described as a marine collision basin by Hsiung & Yu (2013), focusing on the collision process in the incipient collision zone north of the Manila subduction zone forming an ocean basin with distinct morphotectonic features such as prominent submarine canyons.…”
Section: Discussionmentioning
confidence: 99%