Zobrazeno 1 - 10
of 46
pro vyhledávání: '"A.B. Moyes"'
Publikováno v:
Journal of African Earth Sciences. 30:641-650
Biotite separates from Archaean granitoid lithologies on the Kaapvaal Craton north of the roterozoic Namaqua-Natal Belt in south eastern South Africa exhibit RbSr model dates of 967 ± 24 Ma for samples from within 25 km of the present northern li
Autor:
P.B. Groenewald, A.B. Moyes
Publikováno v:
Chemical Geology. 129:247-256
Garnet SmNd isotopic data are presented for selected samples from the metamorphic terrane of the H.U. Sverdrupfjella, western Dronning Maud Land, and yield Pan-African ages ranging from 680 to 415 Ma. Reproducibility of the garnet data is outside
East Antarctic crustal evolution: geological constraints and modelling in western Dronning Maud Land
Publikováno v:
Precambrian Research. 75:231-250
Two geological provinces of western Dronning Maud Land provide constraints which allow preliminary modelling of crustal evolution in this part of East Antarctica. The Grunehogna province comprises a 3000 Ma granitic basement overlain by a 1000 Ma seq
Autor:
P.D. Harris, G. H. Grantham, A.B. Moyes, P.B. Groenewald, C. Jackson, J.R. Krynauw, G. Ferrar
Publikováno v:
Precambrian Research. 75:209-229
Three episodes of deformation spanning a period of ∼900 Ma are recognised. The first deformation at ∼ 1000 Ma involved progressive, yet distinct stages within a protracted, composite event involving recumbent folding, low-angle thrust faulting an
Publikováno v:
Antarctic Science. 7:87-97
The Ahlmannryggen-Borgmassivet area of western Dronning Maud Land comprises a relatively undeformed, unmetamorphosed sequence of sedimentary-volcanogenic rocks, the Ritscherflya Supergroup, intruded by a suite of continental tholeiites, the Borgmassi
Publikováno v:
Journal of the Geological Society. 150:833-842
The Mid-Proterozoic-Early Palaeozoic tectonic development of western Dronning Maud Land is examined in the light of recent proposals that suggest geological continuity between Laurentia and Gondwana during the Middle Proterozoic (the SWEAT hypothesis
Publikováno v:
Chemical Geology. 106:453-466
The alkali granitoids of the Brattskarvet intrusive suite constitute the largest intrusion (∼ 100 km2) post-dating Middle Proterozoic orogeny in the Sverdrupfjella region of the Maudheim tectonic province, western Dronning Maud Land. RbSr whole-
Autor:
A.B. Moyes, L.A.G. Antoine
Publikováno v:
Tectonophysics. 212:33-44
A new processing procedure is implemented on Magsat data over the southern African region and surrounding oceans. The oceanic region of the ensuing map is interpreted in this study. The anomaly map is image processed and a composite image of Magsat w
Publikováno v:
Antarctic Science. 3:197-204
The ∼470 Ma Dalmatian Granite forms sheet-like bodies intruded discordantly into orthogneisses, paragneisses and calcareous rocks belonging to the ∼1000 Ma Jutulrora, Sveabreen and Fuglefjellet formations respectively. The Dalmatian Granite is mu
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