West Greenland Glass in Picrite – Low-pressure Cotectic Differentiates or Independent Compositions?
J. Natland
West Greenland was hot – how else can you make 22,000 km3 of picrites?
Eruptive Temperatures of the Paleogene Picrites of West Greenland and Baffin Bay
J.H. Natland
Why olivine control arguments cannot be used to infer high temperature at Samoa
last updated 8th March, 2009