Nature, Structure and Evolution of the Ocean-Continent Boundary: The Lesson of the West Galicia Margin (Spain) View Full Text


Ontology type: schema:Chapter     


Chapter Info

DATE

1995

AUTHORS

G. Boillot , M. O. Beslier , J. Girardeau

ABSTRACT

The available geological data on the West Galicia Ocean-Continent boundary are briefly reviewed. Four parallel belts of basement terranes were sampled from the oceanic domain to the passive margin: basaltic seafloor, sheared and serpentinized mantle rocks cropping out on the “peridotite ridge”, mylonitized underplated gabbro, and upper continental crust resting on a strong seismic reflector considered to be a detachment. The geological and geophysical data support a simple shear model, according to which the lithosphere stretching and thinning were accommodated by two sets of conjugate shear zones. In conclusion we advocate a “basement strategy” in passive margin and Ocean-Continent Boundary studies, the basement rocks providing better evidence of the rifting processes than sediments. More... »

PAGES

219-229

Book

TITLE

Rifted Ocean-Continent Boundaries

ISBN

978-94-010-4024-2
978-94-011-0043-4

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/978-94-011-0043-4_12

DOI

http://dx.doi.org/10.1007/978-94-011-0043-4_12

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1025191215


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