Apparent overconsolidation of mudstones in the Kumano Basin of southwest Japan: Implications for fluid pressure and fluid flow within a forearc setting-Reference-Cited by-同舟云学术

Apparent overconsolidation of mudstones in the Kumano Basin of southwest Japan: Implications for fluid pressure and fluid flow within a forearc setting

Published:2013-04 Issue:4 Volume:14 Page:1023-1038
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Guo Junhua¹,Underwood Michael B.¹,Likos William J.²,Saffer Demian M.³

Affiliation:

1. Department of Geological Sciences; University of Missouri; Columbia MO 65211 USA

2. Department of Civil and Environmental Engineering; University of Missouri; Columbia MO 65211 USA

3. Department of Geosciences; The Pennsylvania State University; 534 Deike Building University Park PA USA

Funder

National Science Foundation

Consortium for Ocean Leadership

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference108 articles.

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3. Influence of mechanical compaction and clay mineral diagenesis on the microfabric and pore-scale properties of deep-water Gulf of Mexico mudstones;Aplin;Clays Clay Miner.,2006

4. ASTM International 2006 Standard test method for one-dimensional consolidation properties of saturated cohesive soils using controlled-strain loading (Standard D4186-06) Am. Soc. Testing and Mater West Conshohocken, PA

5. Compactional behavior of fine-grained sediments - examples from Deep Sea Drilling Project cores;Bayer;Geologische Rundschau,1989

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