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THE RISE OF SOLID-STATE DIAPIRS
Uppsala University.
Uppsala University.
1995 (English)In: JOURNAL OF STRUCTURAL GEOLOGY, ISSN 0191-8141, Vol. 17, no 8, 1183-1195 p.Article in journal (Other scientific) Published
Abstract [en]

When magma inside a diapir solidifies it increases in density and becomes a stiff power-law fluid. If the diapir is still positively (or negatively) buoyant after solidification, it will continue to rise (or start to sink). The results presented here sugg

Place, publisher, year, edition, pages
PERGAMON-ELSEVIER SCIENCE LTD , 1995. Vol. 17, no 8, 1183-1195 p.
Keyword [en]
CONTINENTAL-CRUST; FLOW PROPERTIES; EMPLACEMENT; DEFORMATION; GRANITE; PLUTON; RHEOLOGY; ASCENT; ROCKS; SPHERE
Identifiers
URN: urn:nbn:se:uu:diva-27972OAI: oai:DiVA.org:uu-27972DiVA: diva2:55868
Note
Addresses: UPPSALA UNIV, INST EARTH SCI, HANS RAMBERG TECTON LAB, S-75236 UPPSALA, SWEDEN. VRIJE UNIV AMSTERDAM, INST EARTH SCI, 1081 HV AMSTERDAM, NETHERLANDS. RUSSIAN ACAD SCI, INST EXPTL MINERAL, CHERNOGOLOVKA 142432, RUSSIA.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-16

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