eCite Digital Repository

Researchers Investigate Fate of Oceanic Plateaus at Subduction Zones

Citation

Mann, P and Coffin, M and Shipley, T and Cowley, E and Phinney, E and Teagan, A and Suyehiro, K and Takahashi, N and Araki, E and Shinohara, M and Miura, S and Collot, JY and Delteil, RH and Wood, R and Lewis, KB, Researchers Investigate Fate of Oceanic Plateaus at Subduction Zones, EOS, Transactions American Geophysical Union, USA, 77, 30, pp. 282-283. (1996) [Newspaper Article]

Abstract

During a 32-day marine geophysical expedition aboard the R/V Maurice Ewing, scientists investigated the fate of the Ontong Java oceanic plateau (OJP) at the Solomon island arc (Figure 1). The purpose of the cruise was to examine whether oceanic plateaus subduct, obduct, or partially obduct at subduction zones. With an area of 1.86106 km2 and a crustal thickness of 2543 km, the OJP is the largest and thickest oceanic plateau on Earth and one of the few Pacific oceanic plateaus that is actively converging on an island arc. Obducted remnants of the OJP may occur in a Neogene accretionary prism, the Malaita anticlinorium, which separates the Solomon Island volcanic arc from the OJP (Figure 1).

Item Details

Item Type:Newspaper Article
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
ID Code:75390
Year Published:1996
Deposited By:IMAS - Directorate
Deposited On:2012-01-30
Last Modified:2012-01-30
Downloads:0

Repository Staff Only: item control page