The continent‐ocean transition on the northwestern S outh C hina S ea

Rifted margins are created as a result of stretching and breakup of continental lithosphere that eventually leads to oceanic spreading and formation of a new oceanic basin. A cornerstone for understanding what processes control the final transition to seafloor spreading is the nature of the continen...

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Veröffentlicht in:	Basin research 2017-02, Vol.29 (S1), p.73-95
Hauptverfasser:	Cameselle, Alejandra L., Ranero, César R., Franke, Dieter, Barckhausen, Udo
Format:	Artikel
Sprache:	eng
Online-Zugang:	Volltext
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