GREENLAND: GEOCHRONOLOGY AND PETROLOGY

A group of dyke rocks from the Frederick E. Hyde Fjord area form the southern termination of a prominent dyke-swarm in Peary Land, northernmost Greenland. The melanocratic dykes are NS- to NW–SE-trending, vertically dipping, ≤10–12 m wide, and have narrow chilled margins. Whole-rock 40Ar/39Ar dating...

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Bibliographic Details
Main Authors: Cretaceous Mafic, Dyke Swarm, Peary Land, Daniel J. Kontak, Sven M. Jensen, Douglas A. Archibald, T. Kurtis Kyser
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.2392
http://rruff.info/doclib/cm/vol39/CM39_997.pdf