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...
Main Authors: | , , , , , , |
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.556.2392 http://rruff.info/doclib/cm/vol39/CM39_997.pdf |