Evidence for mechanical decoupling of the upper plate at the Nankai subduction zone: Constraints from core-scale faults at NantroSEIZE Sites C0001 and C0002-Reference-Cited by-同舟云学术

Evidence for mechanical decoupling of the upper plate at the Nankai subduction zone: Constraints from core-scale faults at NantroSEIZE Sites C0001 and C0002

Published:2013-03 Issue:3 Volume:14 Page:620-633
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Lewis Jonathan C.¹,Byrne Timothy B.²,Kanagawa Kyuichi³

Affiliation:

1. Indiana University of Pennsylvania; Department of Geoscience; 114 Walsh Hall; Indiana; Pennsylvania; 15705; USA

2. University of Connecticut; Center for Integrative Geosciences; Storrs; Connecticut; USA

3. Chiba University; Department of Earth Sciences; Igage-ku; Chiba; Japan

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference35 articles.

1. NanTroSEIZE Stage 1A: NanTroSEIZE megasplay riser pilot;Ashi;IODP Prel. Rep.,2008

2. Broad, weak regions of the Nankai Megathrust and implications for shallow coseismic slip;Bangs;Earth Planet. Sci. Lett.,2009

3. Structural aspects of diapiric melange emplacement: the Duck Creek Diapir;Brown;J. Struct. Geol.,1993

4. Anelastic strain recovery reveals extension across SW Japan subduction zone;Byrne;Geophys. Res. Lett.,2009

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