Generation of nordmarkitic melts by melting of basement gneisses: the Astrophyllite Bay complex

Acid-basic net-veined or pillowed dykes and intrusive bodies are small but important components in the felsic complexes of the Tertiary magmatic province in East Greenland. In Astrophyllite bay in the Snout Series syenite intrusion at the margin of the Kangerdlugssuaq syenite intrusion basic trachya...

Full description

Bibliographic Details
Main Authors: Troels F. D. Nielsen, C. Kent Brooks
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.519.6629
http://2dgf.dk/xpdf/bull38-03-04-161-164.pdf
Description
Summary:Acid-basic net-veined or pillowed dykes and intrusive bodies are small but important components in the felsic complexes of the Tertiary magmatic province in East Greenland. In Astrophyllite bay in the Snout Series syenite intrusion at the margin of the Kangerdlugssuaq syenite intrusion basic trachyandesite melts invade and melt the host of Archaean granitic gneisses. Pillows of trachyandesite are chilled to the surrounding felsic anatectic melt. The felsic melt is not granitic but syenitic in composition. Element distributions between the chilled basic and felsic melts suggest that the anatectic melt was transformed to a syenitic composition by diffusion between the two contacting melts.