Friction experiments on saturated sediments and their implications for the stress state of the Nankai and Barbados subduction thrusts

Autor:	Achim J Kopf, Kevin M. Brown
Rok vydání:	2003
Předmět:	Décollement geography geography.geographical_feature_category Subduction Geology engineering.material Fault (geology) Oceanography Pore water pressure Plate tectonics Shear (geology) Geochemistry and Petrology Illite engineering Shear velocity Petrology Geomorphology
Zdroj:	Marine Geology. 202:193-210
ISSN:	0025-3227
Popis:	The Nankai and Barbados forearcs have low-stress subduction thrusts. The sediments entering the subduction zone, and namely the material in the decollement zones, have been well characterized by numerous deep-sea drilling legs and studies of the recovered cores. Nankai has high heat flow and significant amounts of illite, while Barbados is a smectite-dominated system. Based on results from ring shear (
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=doi_________::30f589ef5f43fd6b603951363217c63f https://doi.org/10.1016/s0025-3227(03)00286-x Zobrazit plný text záznamu Full Text from ScienceDirect