MARBLE STRIPE KARST OF THE SCANDINAVIAN CALEDONIDES: AN END-MEMBER IN THE CONTACT KARST SPECTRUM MARMORNAT PASASTI KRAS SKANDINAVSKIH KALEDONIDOV: SKRAJNI PRIMER KONTAKTNEGA KRASA

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Publication Date

January 2001

Abstract

Stripe karst is an extreme case of contact karst, where the allogenic contact perimeter is very large relative to the area of the karst outcrop. This is the dominant karst found in metamorphic marble outcrops of the Scandinavian Caledonides, and is named the Norwegian karst type, as it was first described here by the Norwegian geologist Gunnar Horn. Analysis of the geometric properties of a stripe suggests that stripe karst can be defined as a narrow karst outcrop with length to width ratio (g) greater than 3 and is fully developed when g =30. Stripe karst contacts are either sub-vertical, or inclined with confined or perched contacts.

Keywords

Conact Karst, Marble Stripe Kaerst, Scandanavia Caledonides

Document Type

Article

Notes

Acta Carsologica, Vol. 30, no. 2 (2001).

Identifier

SFS0072261_00001

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