Structural restoration of thrusts at the toe of the Nankai Trough accretionary prism off Shikoku Island, Japan: Implications for dewatering processes

Author:

Moore Gregory F.1,Saffer Demian2,Studer Melody1,Costa Pisani Patrizia1

Affiliation:

1. Department of Geology and Geophysics; University of Hawai'i at Mānoa; 1680 East-West Road,; Honolulu; Hawaii; 96822; USA

2. Department of Geosciences; Pennsylvania State University; 310 Deike Building,; University Park; Pennsylvania; 16802; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference55 articles.

1. Source mechanisms and tectonic significance of historical earthquakes along the Nankai Trough, Japan;Ando;Tectonophysics,1975

2. AAPG Mem.;Aoki,1982

3. Evidence of a low-velocity layer beneath the accretionary prism of the Nankai Trough: Inferences from a synthetic sonic log;Aoki;Initial Rep. Deep Sea Drill. Proj.,1986

4. Structure, seismic data, and orogenic evolution of the southern Canadian Rocky Mountains;Bally;Bull. Can. Pet. Geol.,1966

5. Evolution of the Nankai Trough décollement from the trench into the seismogenic zone: Inferences from three-dimensional seismic reflection imaging;Bangs;Geology,2004

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