Structural evolution of carbonate-hosted cataclastic bands adjacent to a major neotectonic fault, Sellicks Beach, South Australia

Deformation bands are common fault-related strain features found in upper crustal granular highly porous sedimentary rocks. However, the majority of research has focused on siliciclastic-related case studies, resulting in a knowledge gap surrounding the nomenclature and implications of carbonate-hos...

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Detaylı Bibliyografya

Yayımlandı:	https://doi.org/10.1016/j.jsg.2019.05.004
Yazar:	Lubiniecki, D.C.
Diğer Yazarlar:	White, S.R.S., King, R.C., Holford, S.P., Bunch, M.A., Hill, S.M.
Materyal Türü:	Makale
Dil:	İngilizce
Baskı/Yayın Bilgisi:	Elsevier 2019
Konular:	Willunga Fault; St. Vincent Basin; cataclasis intensity; fault history; Mount Lofty Ranges
Online Erişim:	http://hdl.handle.net/2440/121543
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