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