Gabbro sills intruded into peridotite

The gray rocks are a series of gabbroic sills interlayered with cumulate gabbros and peridotites. These sills occur along the boundary between underlying peridotites and overlying gabbros in the the Bay of Islands ophiolite. This is, then, an exposure of a fossil "Moho" separating Cambrian...

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Bibliographic Details
Other Authors: Wojtal, Steven F.
Format: Other/Unknown Material
Language:unknown
Published: Oberlin College Library 1987
Subjects:
Geology
Structural
Peridotite
Newfoundland
Online Access:http://server15963.contentdm.oclc.org/u?/p15963coll1,1632
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record_format openpolar
spelling ftohiocolleges:oai:server15963.contentdm.oclc.org:p15963coll1/1632 2023-05-15T17:18:03+02:00 Gabbro sills intruded into peridotite Wojtal, Steven F. Zone: 21 Easting: 403816, Northing: 5431947 49.0329 -58.31591 Bay of Islands Newfoundland and Labrador Newfoundland Cambrian 1987-09 jpeg2000 http://server15963.contentdm.oclc.org/u?/p15963coll1,1632 unknown Oberlin College Library wojtals_pcd_039 http://server15963.contentdm.oclc.org/u?/p15963coll1,1632 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 Peridotite Bay of Islands Complex. 1987 ftohiocolleges 2022-05-18T11:55:36Z The gray rocks are a series of gabbroic sills interlayered with cumulate gabbros and peridotites. These sills occur along the boundary between underlying peridotites and overlying gabbros in the the Bay of Islands ophiolite. This is, then, an exposure of a fossil "Moho" separating Cambrian oceanic crust from the underlying mantle. Other/Unknown Material Newfoundland Five Colleges of Ohio Digital Collections Newfoundland
institution Open Polar
collection Five Colleges of Ohio Digital Collections
op_collection_id ftohiocolleges
language unknown
topic Geology
Structural
Peridotite
spellingShingle Geology
Structural
Peridotite
Gabbro sills intruded into peridotite
topic_facet Geology
Structural
Peridotite
description The gray rocks are a series of gabbroic sills interlayered with cumulate gabbros and peridotites. These sills occur along the boundary between underlying peridotites and overlying gabbros in the the Bay of Islands ophiolite. This is, then, an exposure of a fossil "Moho" separating Cambrian oceanic crust from the underlying mantle.
author2 Wojtal, Steven F.
format Other/Unknown Material
title Gabbro sills intruded into peridotite
title_short Gabbro sills intruded into peridotite
title_full Gabbro sills intruded into peridotite
title_fullStr Gabbro sills intruded into peridotite
title_full_unstemmed Gabbro sills intruded into peridotite
title_sort gabbro sills intruded into peridotite
publisher Oberlin College Library
publishDate 1987
url http://server15963.contentdm.oclc.org/u?/p15963coll1,1632
op_coverage Zone: 21 Easting: 403816, Northing: 5431947
49.0329
-58.31591
Bay of Islands
Newfoundland and Labrador
Newfoundland
Cambrian
geographic Newfoundland
geographic_facet Newfoundland
genre Newfoundland
genre_facet Newfoundland
op_source 35 mm Kodachrome slide. Oberlin College. Geology Department.
op_relation wojtals_pcd_039
http://server15963.contentdm.oclc.org/u?/p15963coll1,1632
op_rights For research and educational use only. For all other uses please contact the Oberlin College. Geology Department
_version_ 1766086214431014912

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