2003 Seattle Annual Meeting (November 2–5, 2003)
Paper No. 169-6
Presentation Time: 2:45 PM-3:00 PM

SEAFLOOR DEFORMATION ACROSS THE MINDORO COLLISION ZONE (MCZ) AND VERDE ISLAND PASSAGE FAULT ZONE (VIPFZ), PHILIPPINES

HOGAN, Phillip J., URS Corporation, 130 Robin Hill Road, Suite 100, Santa Barbara, CA 93117, phillip_hogan@urscorp.com and MOLINARI, Mark P., URS Corporation, 1501 4th Avenue, Suite 1400, Seattle, WA 98101-1616

Marine geohazard surveys conducted for an offshore gas pipeline route crossed two major, active fault zones offshore Mindoro Island. Bathymetric charts and computer renderings of seafloor data provide a detailed image of associated seafloor deformation. The MCZ is the southern extension of the Manila Trench, where continental crust of the South China Sea is subducted beneath continental crust of Mindoro Island. The active collision zone off the southern end of Mindoro Island is 25 km west of the previously inferred trace. At this location the subducted plate is being arched, and tension fractures and extensional faults are present. Transpressional folding and thrust faulting are evident in the overriding plate, reflecting oblique convergence. The VIPFZ is a major left-lateral fault zone between Luzon and Mindoro Island. Numerous pull-aparts, pressure ridges, volcanic vents, and volcanic islands (including Verde Island itself) occur along the VIPFZ. The VIPFZ appears to be offset by the historically active Aglubang fault west of Verde Island.

2003 Seattle Annual Meeting (November 2–5, 2003)
Session No. 169
Tectonics III: Tectonics of the Circum-Pacific Rim in Space and Time: Focus on Alaska, Central and South America, and the Western Pacific
Washington State Convention and Trade Center: 611/612
1:30 PM-5:30 PM, Tuesday, November 4, 2003

Geological Society of America Abstracts with Programs, Vol. 35, No. 6, September 2003, p. 429

© Copyright 2003 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.