eCite Digital Repository

Oceanic crust and Moho of the Pacific plate in the eastern Ogasawara Plateau region

Citation

Tsuji, T and Nakamura, Y and Tokuyama, H and Coffin, MF and Koda, K, Oceanic crust and Moho of the Pacific plate in the eastern Ogasawara Plateau region, The Island Arc, 16, (3) pp. 361-373. ISSN 1038-4871 (2007) [Refereed Article]


Preview
PDF
Restricted - Request a copy
1Mb
  

Copyright Statement

The definitive published version is available online at: http://onlinelibrary.wiley.com/

DOI: doi:10.1111/j.1440-1738.2007.00589.x

Abstract

To show the structure of oceanic crust and Moho around the eastern Ogasawara Plateau, we have analyzed industry-standard two-dimensional multichannel seismic reflection data. To obtain improved velocity models, phase information of seismic signals was used for velocity analysis and velocity models for oceanic crust above Moho were determined. We apply this velocity analysis technique to seismic reflection data around the eastern Ogasawara Plateau, with the result of clear images of structures within oceanic crust and Moho. South of the Ogasawara Plateau, Moho deepens proximal to the Plateau. Moho distal to the Plateau is ca 7 km below sea floor (bsf), whereas it is ca 10 km bsf near the Plateau. The characters of oceanic crust and Moho differ significantly north and south of the Plateau. To the north, the structure of oceanic crust is ambiguous, the sea floor is shallower and less smooth, and Moho is discontinuous. To the south, structures within oceanic crust and Moho are imaged clearly, and the sea floor is deeper. A strong Moho reflection south of the Plateau might represent a sharp boundary between layered gabbro and peridotite. However, discontinuous Moho reflections north of the Plateau might represent rough topography because of intensive magmatism or a gradual downward increase in velocity within a thick Moho transition zone. A fracture zone north of the Plateau also appears to separate oceanic crust and Moho of different characters, suggesting vigorous magmatism between the Plateau and the fracture zone, and that the Ogasawara Plateau and the fracture zone influenced the genesis of oceanic crust and upper mantle. Differences in acoustic characteristics to the north and south of the Plateau are apparent in profiles illuminated by seismic attributes.

Item Details

Item Type:Refereed Article
Keywords:magmatic activities;Moho;oceanic crust;Ogasawara Plateau;seismic attributes;seismic velocity
Research Division:Earth Sciences
Research Group:Geology
Research Field:Marine Geoscience
Objective Division:Expanding Knowledge
Objective Group:Expanding Knowledge
Objective Field:Expanding Knowledge in the Earth Sciences
Author:Coffin, MF (Professor Mike Coffin)
ID Code:73702
Year Published:2007
Web of Science® Times Cited:8
Deposited By:Research Division
Deposited On:2011-10-24
Last Modified:2011-11-10
Downloads:1 View Download Statistics

Repository Staff Only: item control page