Publication Date
1980
Document Type
Dissertation/Thesis
First Advisor
Berg, Jonathan H.
Degree Name
M.S. (Master of Science)
Legacy Department
Department of Geology
LCSH
Mineralogy--Newfoundland--Labrador; Mineralogical chemistry; Rocks--Thermal properties; Petrology--Newfoundland--Labrador
Abstract
Mafic granulites surrounding the Kiglapait layered intrusion Labrador, were previously thought to represent a contaminated chilled margin (Outer Border Zone) of the intrusion. Mineral chemistry data combined with petrographic observations and bulk chemical analyses suggest that the OBZ mafic granulites were meta metamorphosed by the emplacement of the intrusion and are probably petrogenetically unrelated to it. Petrographic study suggests that systematic appearances and disappearances of various minerals occur in the mafic granulites as the intrusion is approached. These are: 1) actinolite out 2 ) sphene out 3) epidote - calcite out 4) chlorite out 5) clinopyroxene in 6 ) quartz out 7) orthopyroxene in 8 ) olivine in 9) magnetite in 10) hornblende - ilmenite out
Recommended Citation
Docka, Janet Anne, "Mineral chemistry and thermometry of metamorphosed mafic rocks in the contact aureole of the Kiglapait intrusion" (1980). Graduate Research Theses & Dissertations. 3972.
https://huskiecommons.lib.niu.edu/allgraduate-thesesdissertations/3972
Extent
ix, 155 pages
Language
eng
Publisher
Northern Illinois University
Rights Statement
In Copyright
Rights Statement 2
NIU theses are protected by copyright. They may be viewed from Huskie Commons for any purpose, but reproduction or distribution in any format is prohibited without the written permission of the authors.
Media Type
Text
Comments
Includes bibliographical references.||Includes illustrations.