RECONNAISSANCE GEOCHRONOLOGY OF THE INFRACRUSTAL ROCKS OF FLYVERFJORD

A Rb-Sr whole rock isochron has yielded an age of 3000 m.y. for the infracrustal rocks occurring in Flyverfjord, East Greenland. This age is further evidence for the presence of Precambrian basement rocks occurring in the East Greenland Caledonian fold belt.

Bibliographic Details
Main Authors: Scoresby Sund, East Greenland, David C. Rex, Andrew Gledhill, Department Of Earth Sciences
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Flyverfjord
Greenland
East Greenland
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.626.2560
http://2dgf.dk/xpdf/bull23-01-02-49-54.pdf
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record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.626.2560 2023-05-15T16:03:12+02:00 RECONNAISSANCE GEOCHRONOLOGY OF THE INFRACRUSTAL ROCKS OF FLYVERFJORD Scoresby Sund East Greenland David C. Rex Andrew Gledhill Department Of Earth Sciences The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.626.2560 http://2dgf.dk/xpdf/bull23-01-02-49-54.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.626.2560 http://2dgf.dk/xpdf/bull23-01-02-49-54.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://2dgf.dk/xpdf/bull23-01-02-49-54.pdf text ftciteseerx 2016-01-08T15:14:11Z A Rb-Sr whole rock isochron has yielded an age of 3000 m.y. for the infracrustal rocks occurring in Flyverfjord, East Greenland. This age is further evidence for the presence of Precambrian basement rocks occurring in the East Greenland Caledonian fold belt. Text East Greenland Greenland Unknown Flyverfjord ENVELOPE(-27.917,-27.917,71.567,71.567) Greenland
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description A Rb-Sr whole rock isochron has yielded an age of 3000 m.y. for the infracrustal rocks occurring in Flyverfjord, East Greenland. This age is further evidence for the presence of Precambrian basement rocks occurring in the East Greenland Caledonian fold belt.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Scoresby Sund
East Greenland
David C. Rex
Andrew Gledhill
Department Of Earth Sciences
spellingShingle Scoresby Sund
East Greenland
David C. Rex
Andrew Gledhill
Department Of Earth Sciences
RECONNAISSANCE GEOCHRONOLOGY OF THE INFRACRUSTAL ROCKS OF FLYVERFJORD
author_facet Scoresby Sund
East Greenland
David C. Rex
Andrew Gledhill
Department Of Earth Sciences
author_sort Scoresby Sund
title RECONNAISSANCE GEOCHRONOLOGY OF THE INFRACRUSTAL ROCKS OF FLYVERFJORD
title_short RECONNAISSANCE GEOCHRONOLOGY OF THE INFRACRUSTAL ROCKS OF FLYVERFJORD
title_full RECONNAISSANCE GEOCHRONOLOGY OF THE INFRACRUSTAL ROCKS OF FLYVERFJORD
title_fullStr RECONNAISSANCE GEOCHRONOLOGY OF THE INFRACRUSTAL ROCKS OF FLYVERFJORD
title_full_unstemmed RECONNAISSANCE GEOCHRONOLOGY OF THE INFRACRUSTAL ROCKS OF FLYVERFJORD
title_sort reconnaissance geochronology of the infracrustal rocks of flyverfjord
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.626.2560
http://2dgf.dk/xpdf/bull23-01-02-49-54.pdf
long_lat ENVELOPE(-27.917,-27.917,71.567,71.567)
geographic Flyverfjord
Greenland
geographic_facet Flyverfjord
Greenland
genre East Greenland
Greenland
genre_facet East Greenland
Greenland
op_source http://2dgf.dk/xpdf/bull23-01-02-49-54.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.626.2560
http://2dgf.dk/xpdf/bull23-01-02-49-54.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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