Abstract
Igneous layering is developed in the Proterozoic rapakivi granite suite of South Greenland in an area on the south-easternmost coast of the island of Angnikitsoq. The layering at this locality is unusual in that it is defined by interstitial phases. We suggest that large-scale hydrothermal alteration has converted a fine-grained pyroxene cumulate, in which original cumulate pyroxenes occurred in the interstices between larger feldspars, to interstitial biotite and green amphibole.
Original language | English |
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Pages (from-to) | 739-742 |
Number of pages | 4 |
Journal | Journal of the Geological Society |
Volume | 147 |
Publication status | Published - Sept 1990 |