Backarc basin oceanic crust and uppermost mantle seismic velocity structure of the Shikoku Basin, south of Japan View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2011-02

AUTHORS

Azusa Nishizawa, Kentaro Kaneda, Mitsuhiro Oikawa

ABSTRACT

Seismic refraction and reflection measurements were made along three profiles across the Shikoku Basin, one of the three backarc basins on the Philippine Sea plate. The P-wave velocity models show the presence of a very large horizontal irregularity related to the seamounts on the extinct spreading center, transition zones from the Shikoku Basin to Kyushu-Palau Ridge, and from the Shikoku Basin to the Izu-Ogasawara Island arc. However, the other areas were found to have features similar to those of a normal oceanic crustal model composed of oceanic Layer 2 with a high velocity gradient and Layer 3 with a small velocity gradient. The Shikoku backarc basin oceanic crust was found to be characterized by a thinner igneous crust, especially in Layer 3, and the azimuthal anisotropy in the uppermost mantle expected from the seafloor spreading was not detected. More... »

PAGES

151-155

Journal

TITLE

Earth, Planets and Space

ISSUE

2

VOLUME

63

Identifiers

URI

http://scigraph.springernature.com/pub.10.5047/eps.2010.12.003

DOI

http://dx.doi.org/10.5047/eps.2010.12.003

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1027228401


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