Geological Development of the Proterozoic Basement of East Antarctica in the Prydz Bay-Prince Charles Mountains RegionEntry ID: ASAC_51
Abstract: The structural and metamorphic history of the Proterozoic of the northern Prince Charles Mountains will be determined and compared with the geological history of the Prydz Bay region. The nature of the 1000 Ma granulite facies metamorphism, and its regional variability will be assessed. The role of fluids in this metamorphism will also be evaluated.
For more details see the full report at the url below.
Temporal coverage is only approximate.
Start Date: 1988-11-30Stop Date: 1989-01-15
Access Constraints The field report is publicly available for download from the URL given below.
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Role: TECHNICAL CONTACT
Role: DIF AUTHOR
Phone: +61 2 6220 2477
Fax: +61 2 6220 2186
Australian National University R'SRCH SCHOOL OF EARTH SCIENCES
Province or State: Australian Capital Territory
Postal Code: 2600
Fitzsimons, I.C.W. and Thost, D.E. (1992), Geological relationships in high-grade basement gneiss of the northern Prince Charles Mountains, East Antarctica., Australian Journal of Earth Sciences, 39, 173-193
Nichols, G.T. and Berry, R.F. (1991), A decompressional P-T path, Reinbolt Hills, East Antarctica., Journal of Metamorphic Geology, 9, 257-266
Tait, R. and Harley, S. ( (1988), The role of mafic granulites in the generation of calc-alkaline magmas: a study of granulite migmatites, Transactions of the Royal Society of Edinburgh, 79, 209
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Creation and Review Dates
DIF Creation Date: 2000-07-18
Last DIF Revision Date: 2014-01-10