AN EARLY PRECAMBRIAN SUPPOSED CONGLOMERATE IN THE FISKENÆSSET AREA
gossan zone was discovered in the Fiskenæsset area, West Greenland. Blasting showed a rock composed of well rounded rock fragments (mainly gneiss and ultrabasic rocks) in a matrix consisting mainly of pyrrhotite and pyrite. The zone can be traced for more than 30 km with a width of only 1.5 m, and a...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.545.1890 2023-05-15T16:17:23+02:00 AN EARLY PRECAMBRIAN SUPPOSED CONGLOMERATE IN THE FISKENÆSSET AREA Peter Uitterdijk Appel The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.545.1890 http://2dgf.dk/xpdf/bull21-01-11-17.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.545.1890 http://2dgf.dk/xpdf/bull21-01-11-17.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://2dgf.dk/xpdf/bull21-01-11-17.pdf text ftciteseerx 2016-01-08T11:15:12Z gossan zone was discovered in the Fiskenæsset area, West Greenland. Blasting showed a rock composed of well rounded rock fragments (mainly gneiss and ultrabasic rocks) in a matrix consisting mainly of pyrrhotite and pyrite. The zone can be traced for more than 30 km with a width of only 1.5 m, and all observations so far indicate a conform-able position within the surrounding rocks on a major scale. Local variations in width are believed to be due strong folding. An origin as an intrusive breccia cannot be rejected, but a sedimentary origin seems most probable to the author. Text Fiskenæsset Greenland Unknown Greenland |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
gossan zone was discovered in the Fiskenæsset area, West Greenland. Blasting showed a rock composed of well rounded rock fragments (mainly gneiss and ultrabasic rocks) in a matrix consisting mainly of pyrrhotite and pyrite. The zone can be traced for more than 30 km with a width of only 1.5 m, and all observations so far indicate a conform-able position within the surrounding rocks on a major scale. Local variations in width are believed to be due strong folding. An origin as an intrusive breccia cannot be rejected, but a sedimentary origin seems most probable to the author. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Peter Uitterdijk Appel |
spellingShingle |
Peter Uitterdijk Appel AN EARLY PRECAMBRIAN SUPPOSED CONGLOMERATE IN THE FISKENÆSSET AREA |
author_facet |
Peter Uitterdijk Appel |
author_sort |
Peter Uitterdijk Appel |
title |
AN EARLY PRECAMBRIAN SUPPOSED CONGLOMERATE IN THE FISKENÆSSET AREA |
title_short |
AN EARLY PRECAMBRIAN SUPPOSED CONGLOMERATE IN THE FISKENÆSSET AREA |
title_full |
AN EARLY PRECAMBRIAN SUPPOSED CONGLOMERATE IN THE FISKENÆSSET AREA |
title_fullStr |
AN EARLY PRECAMBRIAN SUPPOSED CONGLOMERATE IN THE FISKENÆSSET AREA |
title_full_unstemmed |
AN EARLY PRECAMBRIAN SUPPOSED CONGLOMERATE IN THE FISKENÆSSET AREA |
title_sort |
early precambrian supposed conglomerate in the fiskenæsset area |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.545.1890 http://2dgf.dk/xpdf/bull21-01-11-17.pdf |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Fiskenæsset Greenland |
genre_facet |
Fiskenæsset Greenland |
op_source |
http://2dgf.dk/xpdf/bull21-01-11-17.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.545.1890 http://2dgf.dk/xpdf/bull21-01-11-17.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766003232050511872 |