Skaergaard Intrusion, East Greenland: contact metamorphism and deformation on Mellemø
Contact metamorphism and deformation are described from part of the Skaergaard intrusion. Rapid C5 heating of the envelope was followed by relatively slow cooling. Deformation occurred in the contact zone after crystallization of the Chilled Marginal Gabbro; pelitic rocks are strongly deformed, fold...
Main Author: | |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1978
|
Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.527.8820 http://2dgf.dk/xpdf/bull28-01-02-1-4.pdf |
id |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.527.8820 |
---|---|
record_format |
openpolar |
spelling |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.527.8820 2023-05-15T16:03:35+02:00 Skaergaard Intrusion, East Greenland: contact metamorphism and deformation on Mellemø John S. Myers The Pennsylvania State University CiteSeerX Archives 1978 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.527.8820 http://2dgf.dk/xpdf/bull28-01-02-1-4.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.527.8820 http://2dgf.dk/xpdf/bull28-01-02-1-4.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://2dgf.dk/xpdf/bull28-01-02-1-4.pdf text 1978 ftciteseerx 2016-01-08T10:26:25Z Contact metamorphism and deformation are described from part of the Skaergaard intrusion. Rapid C5 heating of the envelope was followed by relatively slow cooling. Deformation occurred in the contact zone after crystallization of the Chilled Marginal Gabbro; pelitic rocks are strongly deformed, folded and brecciated, and psammitic rocks are injected as partial melts into fracture zones in the gabbro. Text East Greenland Greenland Unknown Greenland Mellemø ENVELOPE(-73.087,-73.087,76.718,76.718) |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
Contact metamorphism and deformation are described from part of the Skaergaard intrusion. Rapid C5 heating of the envelope was followed by relatively slow cooling. Deformation occurred in the contact zone after crystallization of the Chilled Marginal Gabbro; pelitic rocks are strongly deformed, folded and brecciated, and psammitic rocks are injected as partial melts into fracture zones in the gabbro. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
John S. Myers |
spellingShingle |
John S. Myers Skaergaard Intrusion, East Greenland: contact metamorphism and deformation on Mellemø |
author_facet |
John S. Myers |
author_sort |
John S. Myers |
title |
Skaergaard Intrusion, East Greenland: contact metamorphism and deformation on Mellemø |
title_short |
Skaergaard Intrusion, East Greenland: contact metamorphism and deformation on Mellemø |
title_full |
Skaergaard Intrusion, East Greenland: contact metamorphism and deformation on Mellemø |
title_fullStr |
Skaergaard Intrusion, East Greenland: contact metamorphism and deformation on Mellemø |
title_full_unstemmed |
Skaergaard Intrusion, East Greenland: contact metamorphism and deformation on Mellemø |
title_sort |
skaergaard intrusion, east greenland: contact metamorphism and deformation on mellemø |
publishDate |
1978 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.527.8820 http://2dgf.dk/xpdf/bull28-01-02-1-4.pdf |
long_lat |
ENVELOPE(-73.087,-73.087,76.718,76.718) |
geographic |
Greenland Mellemø |
geographic_facet |
Greenland Mellemø |
genre |
East Greenland Greenland |
genre_facet |
East Greenland Greenland |
op_source |
http://2dgf.dk/xpdf/bull28-01-02-1-4.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.527.8820 http://2dgf.dk/xpdf/bull28-01-02-1-4.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766399271477706752 |