Zobrazeno 1 - 10
of 25
pro vyhledávání: '"M. S. Huber"'
Publikováno v:
Meteoritics & Planetary Science. 55:2320-2337
The Vredefort granophyre dikes have long been recognized as being derived from the now-eroded Vredefort melt sheet. One dike, in particular, the Daskop granophyre dike, is notable for a high abundance of lithic clasts derived from various stratigraph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::89c3518520b7da8103763d48e0a2ec57
https://doi.org/10.1130/2021.2550(10)
https://doi.org/10.1130/2021.2550(10)
The Bon Accord nickel body has been known since the 1920s to contain rocks with up to 50 wt% NiO. Numerous nickel-rich minerals have been described from this deposit. However, none of these minerals contains significant Cu or S, making the deposit ch
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a090a42846e8ea28a86033381a69cc2a
https://doi.org/10.1130/2021.2550(13)
https://doi.org/10.1130/2021.2550(13)
Publikováno v:
Meteoritics & Planetary Science. 54:1579-1593
Publikováno v:
Meteoritics & Planetary Science. 54:2254-2272
Publikováno v:
South African Journal of Geology. 122:109-115
Publikováno v:
Geosciences
Geosciences, Vol 11, Iss 96, p 96 (2021)
Volume 11
Issue 2
Geosciences, Vol 11, Iss 96, p 96 (2021)
Volume 11
Issue 2
Better characterization features borne from long-term crustal modification processes is essential for understanding the dynamics of large basin-forming impact structures on Earth. Within the deeply eroded 2.02 Ga Vredefort Impact Structure in South A
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a37d2aa67a43083e8a588c527d5955fd
http://hdl.handle.net/11427/35267
http://hdl.handle.net/11427/35267
Publikováno v:
South African Journal of Geology. 121:403-420
While the formation of tectonic PTs is widely accepted as related to friction melting for all rock types, the mechanism of formation of impact-related pseudotachylites (PTs) is strongly debated. Moreover, the influence of the target lithology on the
Publikováno v:
South African Journal of Geology. 121:383-402
Vredefort Granophyre dykes are generally considered to be a part of impact melt, which intruded downward from the melt sheet of the Vredefort impact structure (South Africa). This work reports enigmatic textural inhomogeneities found within the Dasko
Autor:
M. S. Huber, Gary R. Byerly
Publikováno v:
South African Journal of Geology. 121:463-486
The Saw Mill Complex (SMC) is a 1 275 m thick layered komatiitic sequence in the 3.3 Ga Weltevreden Formation, uppermost stratigraphic unit of the Onverwacht Group in the northern part of the Barberton Greenstone Belt, South Africa. A series of ultra