Peridotites cut by serpentine-filled veins

Massive serpentinized peridotites more than 25 m from the thrust in image 40 weather into rounded blocks. The borders of these blocks are serpentine-coated veins and/or slip surfaces.

Bibliographic Details
Other Authors: Wojtal, Steven F.
Format: Other/Unknown Material
Language:unknown
Published: Oberlin College Library 1983
Subjects:
Geology
Structural
Thrust faults (Geology)
Newfoundland
Table Mountain
Online Access:http://server15963.contentdm.oclc.org/u?/p15963coll1,1634
id ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/1634
record_format openpolar
spelling ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/1634 2023-05-15T17:17:02+02:00 Peridotites cut by serpentine-filled veins Wojtal, Steven F. Zone: 21 Easting: 429480, Northing: 5484905 49.51267 -57.97419 Table Mountain Newfoundland and Labrador Newfoundland Cambrian 1983-08 jpeg2000 http://server15963.contentdm.oclc.org/u?/p15963coll1,1634 unknown Oberlin College Library wojtals_pcd_041 http://server15963.contentdm.oclc.org/u?/p15963coll1,1634 For research and educational use only. For all other uses please contact the Oberlin College. Geology Department 35 mm Kodachrome slide. Oberlin College. Geology Department. Geology Structural Thrust faults (Geology) Bay of Islands Complex. 1983 ftohiocolleges 2022-05-18T11:55:36Z Massive serpentinized peridotites more than 25 m from the thrust in image 40 weather into rounded blocks. The borders of these blocks are serpentine-coated veins and/or slip surfaces. Other/Unknown Material Newfoundland Five Colleges of Ohio Digital Collections Newfoundland Table Mountain ENVELOPE(69.031,69.031,-48.668,-48.668)
institution Open Polar
collection Five Colleges of Ohio Digital Collections
op_collection_id ftohiocolleges
language unknown
topic Geology
Structural
Thrust faults (Geology)
spellingShingle Geology
Structural
Thrust faults (Geology)
Peridotites cut by serpentine-filled veins
topic_facet Geology
Structural
Thrust faults (Geology)
description Massive serpentinized peridotites more than 25 m from the thrust in image 40 weather into rounded blocks. The borders of these blocks are serpentine-coated veins and/or slip surfaces.
author2 Wojtal, Steven F.
format Other/Unknown Material
title Peridotites cut by serpentine-filled veins
title_short Peridotites cut by serpentine-filled veins
title_full Peridotites cut by serpentine-filled veins
title_fullStr Peridotites cut by serpentine-filled veins
title_full_unstemmed Peridotites cut by serpentine-filled veins
title_sort peridotites cut by serpentine-filled veins
publisher Oberlin College Library
publishDate 1983
url http://server15963.contentdm.oclc.org/u?/p15963coll1,1634
op_coverage Zone: 21 Easting: 429480, Northing: 5484905
49.51267
-57.97419
Table Mountain
Newfoundland and Labrador
Newfoundland
Cambrian
long_lat ENVELOPE(69.031,69.031,-48.668,-48.668)
geographic Newfoundland
Table Mountain
geographic_facet Newfoundland
Table Mountain
genre Newfoundland
genre_facet Newfoundland
op_source 35 mm Kodachrome slide. Oberlin College. Geology Department.
op_relation wojtals_pcd_041
http://server15963.contentdm.oclc.org/u?/p15963coll1,1634
op_rights For research and educational use only. For all other uses please contact the Oberlin College. Geology Department
_version_ 1766082849560068096

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