|2009 Portland GSA Annual Meeting (18-21 October 2009)|
|Paper No. 110-4|
|Presentation Time: 9:00 AM-6:00 PM|
GEOCHEMISTRY OF THE LATE EOCENE GRAYS RIVER VOLCANICS, SOUTHWESTERN WASHINGTON AND NORTHWESTERN OREGON: EVIDENCE FOR A SLAB WINDOW IN THE CASCADIA FOREARC
CHAN, Christine F.1, TEPPER, Jeffery H.1, and NELSON, Bruce2, (1) Geology Department, University of Puget Sound, 1500 N. Warner #1048, Tacoma, WA 98416, firstname.lastname@example.org, (2) Department of Earth and Space Sciences, University of Washington, 4000 15th Avenue NE, Seattle, WA 98195|
The Grays River Volcanics (GRV) is one of several Late Eocene to Early Oligocene volcanic units that erupted within the Cascadia forearc basin. Consisting of >2000 m of submarine and subaerial flows and volcaniclastics, the GRV (~42-37 Ma) extend from NW Oregon into SW Washington and show a younger-to-the-north age progression. These lavas are chemically similar to, but younger than, the 44 Ma Tillamook Volcanics (TV) of the Oregon Coast Range. Previous genetic explanations for the GRV and TV include forearc rifting, a hot spot, or passage of a slab window. The goals of our investigation are to characterize the chemical and Sr-Nd isotope signature of the GRV and better constrain the tectonic setting in which they formed.
The GRV postdate the more voluminous 53-45 Ma Crescent Basalts (CB) and show greater enrichment in Ti, K, and P. Although this could be attributed to smaller degrees of melting, differences in incompatible trace element ratios indicate different mantle sources for the GRV and CB. For example, the GRV have higher average La/YbN (7.4 vs. 2.7) and Zr/Hf (40.4 vs. 35.6) and lower Zr/Nb (6.95 vs. 11.5) than the CB. Ongoing Sr-Nd isotope analyses will further characterize these mantle sources. Based on the lack of an arc signature and the likelihood that mantle rocks above the subducting plate would be too cool to yield GRV basalts, we suggest that the GRV source was below the subducting plate. This evidence for an asthenospheric source, combined with northward age progression of volcanism, support a slab-window setting. A similar setting may also explain younger forearc basaltic centers in Oregon if left-stepping offsets in the subducting Kula-Farallon ridge caused southward jumps of the ridge-trench triple junction.
2009 Portland GSA Annual Meeting (18-21 October 2009)
General Information for this Meeting
|Session No. 110--Booth# 285|
Multidisciplinary Studies of Cascade Volcanism and its Tectonic Setting (Posters)
Oregon Convention Center: Hall A
9:00 AM-6:00 PM, Monday, 19 October 2009
Geological Society of America Abstracts with Programs, Vol. 41, No. 7, p. 309
© Copyright 2009 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.