Thrust fault separating serpentinized peridotites from metamorphosed sedimentary rocks

Steeply-inclined sedimentary strata the left side of the image are juxtaposed with serpentinized peridotites of the Bay of Islands complex by a thrust fault. That fault was later folded and this view is nearly along the original slip direction. The peridotites to the right of the image have been dis...

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Bibliographic Details
Other Authors: Wojtal, Steven F.
Format: Other/Unknown Material
Language:unknown
Published: Oberlin College Library 1983
Subjects:
Online Access:http://server15963.contentdm.oclc.org/u?/p15963coll1,1633