The formation of the Vredefort Dome, a structure in excess of 100 km in diameter and located in the approximate center of the Witwatersrand basin, is still the subject of lively geological controversy. It is widely accepted that its formation seems to have taken place in a single sudden event, herein referred to as the Vredefort event, accompanied by the release of gigantic amounts of energy. It is debated, however, whether this central event was an internal one, i.e., a cryptoexplosion triggered by volcanic or tectonic processes, or the impact of an extraterrestrial body. The results of this debate are presented
Fault-generated pseudotachylytes are the product of frictional melting during high-velocity slip ass...
The Schurwedraai alkali granite is one of a number of prominent ultramafic-mafic and felsic intrusio...
© 2017 Elsevier Ltd 40 Ar/ 39 Ar dating of specimens of moldavite, the formation of which is linked ...
Since the discovery of the Ir enrichment in Cretaceous-Tertiary boundary clays in 1980, the effects ...
The Vredefort Dome is located within and almost central to the Witwatersrand basin in its presently ...
The Vredefort structure located in the center of the Witwatersrand basin in South Africa and the Sud...
The unique 2.05-Ga Bushveld and Vredefort complexes cover 100,000 sq km (diameter 400 km) on the oth...
U-Pb geochronology on baddeleyite is a powerful technique that can be applied effectively to chronos...
(IF 3,082)International audienceWe have carried out paleomagnetic sampling of a similar to 750 m seq...
Fault-generated pseudotachylytes are the product of frictional melting during high-velocity slip ass...
Studies of meteorites are based mostly on samples that fell to Earth in the recent past (i.e., a few...
Studies of meteorites are based mostly on samples that fell to Earth in the recent past (i.e., a few...
Impact cratering was a fundamental geological process in the early Solar System and, thus, constrain...
Impact cratering was a fundamental geological process in the early Solar System and, thus, constrain...
The ~70 km-diameter Yarrabubba impact structure in Western Australia is regarded as among Earth’s ol...
Fault-generated pseudotachylytes are the product of frictional melting during high-velocity slip ass...
The Schurwedraai alkali granite is one of a number of prominent ultramafic-mafic and felsic intrusio...
© 2017 Elsevier Ltd 40 Ar/ 39 Ar dating of specimens of moldavite, the formation of which is linked ...
Since the discovery of the Ir enrichment in Cretaceous-Tertiary boundary clays in 1980, the effects ...
The Vredefort Dome is located within and almost central to the Witwatersrand basin in its presently ...
The Vredefort structure located in the center of the Witwatersrand basin in South Africa and the Sud...
The unique 2.05-Ga Bushveld and Vredefort complexes cover 100,000 sq km (diameter 400 km) on the oth...
U-Pb geochronology on baddeleyite is a powerful technique that can be applied effectively to chronos...
(IF 3,082)International audienceWe have carried out paleomagnetic sampling of a similar to 750 m seq...
Fault-generated pseudotachylytes are the product of frictional melting during high-velocity slip ass...
Studies of meteorites are based mostly on samples that fell to Earth in the recent past (i.e., a few...
Studies of meteorites are based mostly on samples that fell to Earth in the recent past (i.e., a few...
Impact cratering was a fundamental geological process in the early Solar System and, thus, constrain...
Impact cratering was a fundamental geological process in the early Solar System and, thus, constrain...
The ~70 km-diameter Yarrabubba impact structure in Western Australia is regarded as among Earth’s ol...
Fault-generated pseudotachylytes are the product of frictional melting during high-velocity slip ass...
The Schurwedraai alkali granite is one of a number of prominent ultramafic-mafic and felsic intrusio...
© 2017 Elsevier Ltd 40 Ar/ 39 Ar dating of specimens of moldavite, the formation of which is linked ...