Heat flow and flexure at subduction zones

It is often suggested that heat flow in the incoming plate at subduction zones is lower than expected for crust of that age due to increased hydrothermal circulation from flexure (extending about 300 km seaward of the trench) and faulting (observed starting about 50–75 seaward of the trench). Testin...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	Geophysical research letters 2003-12, Vol.30 (23), p.SDE4.1-n/a
1. Verfasser:	Stein, Carol A.
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth, ocean, space Exact sciences and technology Marine
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!