Corrigendum to "A ca. 200 Ma hiatus between the Lower and Upper Transvaal Groups of southern Africa: SHRIMP U-Pb detrital zircon evidence from the Segwagwa Group, Botswana: Implications for Palaeoproterozoic glaciations" [Earth Planet. Sci. Lett. 244 (2006) 113-132] (DOI:10.1016/j.epsl.2006.02.008);A ca. 200 Ma hiatus between the Lower and Upper Transvaal Groups of southern Africa: SHRIMP U-Pb detrital zircon evidence from the Segwagwa Group, Botswana: Implications for Palaeoproterozoic glaciations

Earth and Planetary Science Letters

Volumn 244, Issue 1-2, 2006, Pages 113-132

  Mapeo, R B M ^a   Armstrong, R A ^b   Kampunzu, A B ^a   Modisi, M P ^a   Ramokate, L V ^c   Modie, B N J ^c  

^a UNIVERSITY OF BOTSWANA   (Botswana)

^b AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

^c Department of Geological Survey ^*  (Botswana)

Author keywords

Botswana; Detrital zircon geochronology; Glacial implications; Segwagwa Pretoria Group; Southern Africa; Transvaal Supergroup

Indexed keywords

BASALT; CARBONATES; DEPOSITION; GEOCHRONOLOGY; IGNEOUS ROCKS; SANDSTONE; SEDIMENTARY ROCKS; STRATIGRAPHY; ZIRCON;

DETRITAL ZIRCON GEOCHRONOLOGY; GLACIAL IMPLICATIONS; PALAEOPROTEROZOIC GLACIATIONS; SEGWAGWA/PRETORIA GROUP; TRANSVAAL SUPERGROUP;

GLACIAL GEOLOGY;

GLACIATION; PALEOCLIMATE; PROTEROZOIC; SHRIMP DATING;

AFRICA; BOTSWANA; SOUTHERN AFRICA; SUB-SAHARAN AFRICA;

EID: 33645504255     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2006.05.014     Document Type: Erratum

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