Geophysical constraints on Washington convergent margin structure
Journal of Geophysical Research
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Abstract
Gravity and magnetic maps of western Washington reveal the lateral structure and fabric of the Washington Coast Range, Puget Basin, and southern Washington Cascade Range. Two-dimensional gravity and magnetic modeling constrained with geological and other geophysical data indicate that the Coast Range Province rocks are about 1 km thick at the coast, thickening to as much as 30 km near their postulated eastern edge. A composition largely of basalt and gabbro with little interbedded sediments is suggested. Under these rocks may be mantle or a subduction complex composed of dense mafic, ultramafic, and sedimentary rocks like that proposed to underlie Vancouver Island. The Washington model requires that the proposed subduction complex be more dense than the trench sediments and, therefore, that material denser than sediments be incorporated within it. The absence of continental mantle and the modeled wedge shape of the Coast Range Province upper crust suggest that erosion of the bottom of the overriding plate by subduction processes may have occurred. -from Author
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Geophysical constraints on Washington convergent margin structure |
| Series title | Journal of Geophysical Research |
| DOI | 10.1029/JB095iB12p19533 |
| Volume | 95 |
| Issue | B12 |
| Year Published | 1990 |
| Language | English |
| Publisher | American Geophysical Union |
| Description | 14 p. |
| First page | 19533 |
| Last page | 19546 |
| Country | United States |
| State | Washington |
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