A palaeoseismic trench investigation of early Holocene neotectonic faulting along the Kango Fault, southern Cape Fold Belt, South Africa - Part I: stratigraphic and structural features

Goedhart M. L.; Booth P. W. K.

首页> 外文期刊>South African Journal of Geology: Being the Transaction of the Geological Society of South African: Syndie die Verhandelinge van die Geologiese Vereniging van Suid-Afrika >A palaeoseismic trench investigation of early Holocene neotectonic faulting along the Kango Fault, southern Cape Fold Belt, South Africa - Part I: stratigraphic and structural features

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A palaeoseismic trench investigation of early Holocene neotectonic faulting along the Kango Fault, southern Cape Fold Belt, South Africa - Part I: stratigraphic and structural features

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Who would have thought that the southern part of 'stable, old South Africa' was in fact 'not-so-stable', and that there has been spectacular tectonic activity in the Cape Fold Belt as recent as the early Holocene, about 10,327 +/- 755 years ago?

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《South African Journal of Geology: Being the Transaction of the Geological Society of South African: Syndie die Verhandelinge van die Geologiese Vereniging van Suid-Afrika》 |2016年第3期|545-568|共24页
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Goedhart M. L.; Booth P. W. K.;
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Kainos South Africa, POB 15501,Emerald Hill, ZA-6011 Port Elizabeth, South Africa;

Nelson Manclela Metropolitan Univ, Dept Geosci, POB 77000, ZA-6031 Port Elizabeth, South Africa;

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正文语种英语
中图分类地质学;
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A palaeoseismic trench investigation of early Holocene neotectonic faulting along the Kango Fault, southern Cape Fold Belt, South Africa - Part I: stratigraphic and structural features

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