In situ thermal excursions detected in the Nankai Trough forearc slope sediment at IODP NanTroSEIZE Site C0008

At Integrated Ocean Drilling Program (IODP) Site C0008 in the Nankai Trough slope sediment, we discovered in situ temperature anomalies at 80 to 160 m below the seafloor, where pore fluid Cl and δ 18 O excursions were identified and interpreted as pore fluid refreshing due to hydrate dissociation. T...

Ausführliche Beschreibung

Bibliographische Detailangaben

Veröffentlicht in:	Earth, planets, and space planets, and space, 2015-12, Vol.67 (1), p.1-9
Hauptverfasser:	Kinoshita, Masataka, Fukase, Hiroaki, Goto, Shusaku, Toki, Tomohiro
Format:	Artikel
Sprache:	eng
Schlagworte:	Anomalies Computational fluid dynamics Earth and Environmental Science Earth Sciences Fluids Geology Geophysics/Geodesy Hydrates Letter Mathematical models Penetration Sediments Seismology Slopes
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!