Title

Author; Kent, L.E.; Gribnitz, K.H.

dc.contributor.advisor	SAJAR	en_ZA
dc.contributor.author	Author	en_ZA
dc.contributor.author	Kent, L.E.
dc.contributor.author	Gribnitz, K.H.
dc.coverage.spatial	Antarctica	en_ZA
dc.coverage.spatial	Gough Island
dc.date.accessioned	2018-08-23T07:58:05Z
dc.date.available	2018-08-23T07:58:05Z
dc.date.created	1971	en_ZA
dc.date.created	1983
dc.date.issued	1971	en_ZA
dc.date.issued	1983
dc.identifier.uri	http://hdl.handle.net/123456789/7502
dc.description.abstract	abstract	en_ZA
dc.description.abstract	The successions in the cliffs at Macaroni Bay and Ship’s Cove, regarded by a previous worker as glacigenic, with tills of three different ages, are on geological, petrographical and mineralogical evidence considered here to be volcanogenic. Tuff breccias predominate. They are thought to be sub-aqueously deposited debris flows originating from terrestrial volcanoes.	en_ZA
dc.description.sponsorship	Sponsored by the National Research Foundation (South Africa)	en_ZA
dc.description.sponsorship	Sponsored by the National Research Foundation (South Africa)
dc.description.statementofresponsibility	Antarctic Legacy of South Africa	en_ZA
dc.description.statementofresponsibility	Antarctic Legacy Project
dc.language	en_ZA	en_ZA
dc.language	en_ZA
dc.publisher	South African Journal of Antarctic Research	en_ZA
dc.publisher	South African Journal of Antarctic Research Vol 13
dc.relation.ispartof	Vol 4	en_ZA
dc.rights	Copyright	en_ZA
dc.rights	Copyright
dc.subject	Antarctica	en_ZA
dc.subject	Marion Island
dc.subject	Geology
dc.title	Title	en_ZA
dc.title	Problematical Quaternary successions on Marion Island: volcanogenic or glacigenic?
dc.type	Articles	en_ZA
dc.type	Articles
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iso19115.mdformat.name	PDF	en_za
iso19115.mdidentification.deliverypoint	Antarctic Legacy of South Africa, Faculty of Science, Stellenbosch University. Private Bag X1, Matieland. Stellenbosch. South Africa.	en_za
iso19115.mdidentification.electronicmailaddress	antarcticlegacy@sun.ac.za	en-za