X-ray fluorescence core scanning, magnetic signatures, and organic geochemistry analyses of Ryukyu Trench sediments: turbidites and hemipelagites

X-ray fluorescence core scanning, magnetic signatures, and organic geochemistry analyses of Ryukyu Trench sediments: turbidites and hemipelagites

Abstract The southwestern Ryukyu Trench represents the ultimate sink of sediments shed from Taiwan into the Philippine Sea, which are mainly transported to the trench by turbidity currents via submarine canyons. Here, we present trench turbidites intercalated with hemipelagites in a gravity pilot co...

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Bibliographic Details
Main Authors: Kan-Hsi Hsiung, Toshiya Kanamatsu, Ken Ikehara, Kazuko Usami, Chorng-Shern Horng, Naohiko Ohkouchi, Nanako O. Ogawa, Saneatsu Saito, Masafumi Murayama
Format: Article
Language:English
Published: SpringerOpen 2021-01-01
Series:Progress in Earth and Planetary Science
Subjects:
Distal turbidites
ITRAX
Pyrrhotite
Ryukyu Trench
Taiwan
Online Access:https://doi.org/10.1186/s40645-020-00396-2

Internet

https://doi.org/10.1186/s40645-020-00396-2

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