The Ashigara Group: A regressive submarine fan-fan delta sequence in a Quaternary collision boundary, north of Izu Peninsula, central Honshu, Japan-Reference-Cited by-同舟云学术

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The Ashigara Group: A regressive submarine fan-fan delta sequence in a Quaternary collision boundary, north of Izu Peninsula, central Honshu, Japan

Published:1985-11 Issue:3-4 Volume:45 Page:261-292
ISSN:0037-0738
Container-title:Sedimentary Geology
language:en
Short-container-title:Sedimentary Geology

Author:

Ito Makoto

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference69 articles.

1. Seismo-tectonics of the 1923 Kanto earthquake;Ando;J. Phys. Earth,1974

2. Evolution of a strike-slip fault controlled basin, Upper Old Red Sandstone, Scotland;Bluck,1980

3. Multiple slump scars in the Tortonian type area (Piedmont Basin, northwestern Italy);Clari;Sedimentology,1979

4. Sedimentation along the San Andreas Fault, California;Crowell,1974

5. Pebbly mudstones;Crowell,1978

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1. Geological structure of the Izu collision zone, northern border of the Izu block, southern Kanto, Japan;The Journal of the Geological Society of Japan;2011-09-01

2. Double saloon door tectonics in the Japan Sea, Fossa Magna, and the Japanese Island Arc;Tectonophysics;2011-01

3. Collision and subduction structure of the Izu–Bonin arc, central Japan, revealed by refraction/wide-angle reflection analysis;Tectonophysics;2009-10

4. Temporal changes in the composition of Miocene sandstone related to collision between the Honshu and Izu Arcs, central Japan;Special Paper 436: Formation and Applications of the Sedimentary Record in Arc Collision Zones;2008

5. Shallow-marine fan delta slope deposits with large-scale cross-stratification: the Plio-Pleistocene Zaimokuzawa formation in the Ishikari Hills, northern Japan;Sedimentary Geology;2003-05

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