Paleo-stress orientations and magnitudes from triaxial testing and stress inversion analysis in Nankai accretionary prism sediments-Reference-Cited by-同舟云学术

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Paleo-stress orientations and magnitudes from triaxial testing and stress inversion analysis in Nankai accretionary prism sediments

Published:2019-01-15 Issue:1 Volume:6 Page:
ISSN:2197-4284
Container-title:Progress in Earth and Planetary Science
language:en
Short-container-title:Prog Earth Planet Sci

Author:

Hashimoto Yoshitaka,Stipp Michael,Lewis Jonathan C.,Wuttke Frank

Funder

Japan Society for the Promotion of Science

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1186/s40645-018-0249-7.pdf

Reference28 articles.

1. Angelier J (1984) Tectonic analysis of fault slip data sets. J Geophys Res 89:5835–5848

2. Ashi J, Lallemant S, Masago H, the Expedition 315 Scientists (2009) Expedition 315 summary. In M. Kinoshita, et al. (Eds.), Proceedings of the Integrated Ocean Drilling Program, 314/315/316. Washington, DC: Integrated Ocean Drilling Program Management International, Inc. doi: https://doi.org/10.2204/iodp.proc.314315316.121 .2009

3. Byrne TB, Lin W, Tsutsumi A, Yamamoto Y, Lewis JC, Kanagawa K, Kimura G (2009) Anelastic strain recovery reveals extension across SW Japan subduction zone. Geophys res let 36(23). https://doi.org/10.1029/2009GL040749

4. Chang C, McNeill LC, Moore JC, Lin W, Conin M, Yamada Y (2010) In situ stress state in the Nankai accretionary wedge estimated from borehole wall failures. Geochem Geophys Geosys. 11:Q0AD04

5. Fukuchi R, Yamaguchi A, Yamamoto Y, Ashi J (2017) Paleothermal structure of the Nankai inner accretionary wedge estimated from vitrinite reflectance of cuttings. Geochem Geophys Geosys 18(8):3185–3196

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