Geology of the Elisenheim area, Windhoek district, South West Africa, with special reference to the Matchless amphibolite belt

dc.contributor.advisor	Jacob RE	en_US
dc.contributor.author	Finnemore Stephen Horace	en_US
dc.date.accessioned	2013-07-02T14:12:38Z
dc.date.available	2013-07-02T14:12:38Z
dc.date.issued	19750600	en_US
dc.identifier.uri	http://hdl.handle.net/11070.1/5399
dc.description.abstract	Abstract provided by author:	en_US
dc.description.abstract	Petrochemical evidence indicates that the Matchless amphibolites are igneous in origin and genetically related to the ultrabasic talc schists. They are similar in composition to oceanic tholeiites and are thought to have been extruded subaqueously	en_US
dc.description.abstract	Medium grade regional metamorphism accompanied F1, F2 and F3 and outlasted the latter. Mineral assemblages throughout the area are those of the amphibolite facies and P, T conditions prevailing during metamorphism are estimated to have been at least 5 kb at ~ 55O°C	en_US
dc.format.extent	75 p	en_US
dc.language.iso	eng	en_US
dc.subject	Matchless mine	en_US
dc.subject	Windhoek region, geology	en_US
dc.subject	Regional geology	en_US
dc.subject	Elisenheim	en_US
dc.subject	Amphibolites	en_US
dc.title	Geology of the Elisenheim area, Windhoek district, South West Africa, with special reference to the Matchless amphibolite belt	en_US
dc.type	thesis	en_US
dc.identifier.isis	F099-199502130000427	en_US
dc.description.degree	Grahamstown	en_US
dc.description.degree	South Africa	en_US
dc.description.degree	Rhodes University	en_US
dc.description.degree	M Sc	en_US
dc.masterFileNumber	426	en_US

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