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Article: A chronological framework for colluviation during the last 110 kyr in KwaZulu/Natal

TitleA chronological framework for colluviation during the last 110 kyr in KwaZulu/Natal
Authors
Issue Date1995
PublisherAcademy of Science of South Africa. The Journal's web site is located at http://www.sajs.co.za
Citation
South African Journal Of Science, 1995, v. 91 n. 3, p. 134-139 How to Cite?
AbstractLuminescence dating techniques have been applied to colluvial sediments of the Masotcheni Formation. The ages obtained suggest that colluvial deposition occurred during late Oxygen Isotope Stage 5, after the peak of the Last Interglacial (Sub-stage 5e). Further colluvial deposition seems to have commenced early in Stage 3, following a period of donga erosion. A soil was then formed during Stage 3 in the top of this deposit at two of the sites, and this was covered by more colluvial deposits before Stage 3 ended. Evidence for late Holocene colluviation is also presented. -from Authors
Persistent Identifierhttp://hdl.handle.net/10722/90475
ISSN
2015 Impact Factor: 0.902
2015 SCImago Journal Rankings: 0.341

 

DC FieldValueLanguage
dc.contributor.authorWintle, AGen_HK
dc.contributor.authorBotha, GAen_HK
dc.contributor.authorLi, SHen_HK
dc.contributor.authorVogel, JCen_HK
dc.date.accessioned2010-09-06T10:11:06Z-
dc.date.available2010-09-06T10:11:06Z-
dc.date.issued1995en_HK
dc.identifier.citationSouth African Journal Of Science, 1995, v. 91 n. 3, p. 134-139en_HK
dc.identifier.issn0038-2353en_HK
dc.identifier.urihttp://hdl.handle.net/10722/90475-
dc.description.abstractLuminescence dating techniques have been applied to colluvial sediments of the Masotcheni Formation. The ages obtained suggest that colluvial deposition occurred during late Oxygen Isotope Stage 5, after the peak of the Last Interglacial (Sub-stage 5e). Further colluvial deposition seems to have commenced early in Stage 3, following a period of donga erosion. A soil was then formed during Stage 3 in the top of this deposit at two of the sites, and this was covered by more colluvial deposits before Stage 3 ended. Evidence for late Holocene colluviation is also presented. -from Authorsen_HK
dc.languageengen_HK
dc.publisherAcademy of Science of South Africa. The Journal's web site is located at http://www.sajs.co.zaen_HK
dc.relation.ispartofSouth African Journal of Scienceen_HK
dc.rightsCreative Commons: Attribution 3.0 Hong Kong License-
dc.titleA chronological framework for colluviation during the last 110 kyr in KwaZulu/Natalen_HK
dc.typeArticleen_HK
dc.identifier.openurlhttp://library.hku.hk:4550/resserv?sid=HKU:IR&issn=1027-202X&volume=91&spage=134&epage=139&date=1995&atitle=A+chronological+framework+for+colluviation+during+the+last+110+kyr+in+KwaZulu/Natalen_HK
dc.identifier.emailLi, SH:shli@hku.hken_HK
dc.identifier.authorityLi, SH=rp00740en_HK
dc.description.naturepublished_or_final_version-
dc.identifier.scopuseid_2-s2.0-0028882987en_HK
dc.identifier.hkuros13652en_HK
dc.identifier.volume91en_HK
dc.identifier.issue3en_HK
dc.identifier.spage134en_HK
dc.identifier.epage139en_HK
dc.publisher.placeSouth Africaen_HK
dc.identifier.scopusauthoridWintle, AG=7005930050en_HK
dc.identifier.scopusauthoridBotha, GA=7003928560en_HK
dc.identifier.scopusauthoridLi, SH=24438103700en_HK
dc.identifier.scopusauthoridVogel, JC=7403035000en_HK

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