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CO2 sequestration and extreme Mg depletion in serpentinized peridotite clasts from the Devonian Solund basin,
 

Summary: CO2 sequestration and extreme Mg depletion in
serpentinized peridotite clasts from the Devonian Solund basin,
SW-Norway
Andreas Beinlich a,b,
, Ha°kon Austrheim a,b
, Johannes Glodny c
, Muriel Erambert a,b
,
Torgeir B. Andersen a,b
a
Physics of Geological Processes (PGP), University of Oslo, P.O. Box 1048, Blindern, 0316 Oslo, Norway
b
Department of Geosciences, University of Oslo, P.O. Box 1047, Blindern, 0316 Oslo, Norway
c
Deutsches GeoForschungsZentrum (GFZ), Telegrafenberg, 14473 Potsdam, Germany
Received 22 February 2010; accepted in revised form 22 July 2010; available online 12 August 2010
Abstract
The conglomerates of the Solund Devonian basin of SW-Norway contain numerous (locally up to 20 vol.%) peridotitic
clasts with concentric mm- to 10-cm thick zones of varying red to black color. The peridotite clasts show a clear, alter-
ation-related textural evolution. The least-altered rocks are partly serpentinized peridotites, showing a typical mesh texture

  

Source: Andersen, Torgeir Bjørge - Centre for Physics of Geological Processes & Department of Geosciences, Universitetet i Oslo

 

Collections: Geosciences