Thermotectonic evolution of a rifted continental margin: fission track evidence from the Kangerlussuaq area, SE Greenland
ABSTRACT Fission track analyses of apatites from sediments, Precambrian gneisses and Caledonian to Tertiary intrusive rocks from the Kangerlussuaq region reveal its postāCaledonian thermotectonic history. Inland the history involves cooling to temperatures within the high temperature part of the apa...
Published in: | Terra Nova |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Wiley
1996
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Online Access: | http://dx.doi.org/10.1111/j.1365-3121.1996.tb00771.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-3121.1996.tb00771.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-3121.1996.tb00771.x |