Publication Date:
1969-10-01
Description:
SUMMARYThe field of composition and the geochemical trend of the lower portion of the stratiform Stillwater igneous complex correlate well with the field and trend for alpine-type ultrabasic masses in the nearby gneissic basement of the Beartooth Mountains. This is consistent with a derivation of some alpine-type masses by the tectonic disruption and metamorphism of stratiform complexes.
Print ISSN:
0016-7568
Electronic ISSN:
1469-5081
Topics:
Geosciences