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LocalitiesLapanouse-de-Sévérac slag locality, Sévérac-d'Aveyron, Rodez, Aveyron, Occitanie, France
6th Jan 2017 12:43 UTCŁukasz Kruszewski Expert
6th Jan 2017 13:47 UTCUwe Kolitsch Manager
The products of combustion metamorphism have received different names in the past, for example, thermantide, thermantide porcellanite, fused shale, porcellanite, porcelain jasper. However, most of these names have also been used for the products of contact metamorphism in volcanic or near-surface settings. Thus the SG decided to find a general name for all rocks generated by combustion metamorphism and an agreement was found for the term burned (or burnt) rock, which has been defined as follows: Burned rock: General term for a compact, vesicular or clinkery, glassy to holocrystalline metamorphic rock of various colours, produced by the combustion metamorphism of pre-existing sedimentary rocks. In the fused varieties the glass coexists with refractory grains and/or newly formed minerals (e.g.melilite, wollastonite, mullite, cristobalite, spinel), whose nature reflects both the very high temperature metamorphic conditions and the variable chemical composition of the original rock. The term burned rock supersedes such old names as thermantide, thermantide porcellanite, fused shale, porcellanite, porcelain jasper. The glassy or glass-bearing varieties of burned rocks are called buchite (coal-fire buchite) or fritted rock respectively. The term burned rocks also includes some typical ash deposits of refractory material remaining after he combustion of coal seams, giving rise to soft, clay-like rocks resembling volcanic cinerites, and for which the SG proposes the name of coal-fire ashto distinguish it from ash deposits of volcanic origin.
http://www.bgs.ac.uk/SCMR/docs/papers/paper_10.pdf
See also
Grapes, R. (2006): Pyrometamorphism. Springer, Berlin, 276 pp.
7th Jan 2017 11:47 UTCŁukasz Kruszewski Expert
I often find a convertive use of various rock-type names used for the same lithologies; buchites are usually vesicular (but may resemble obsidiane, too), formed from sandstones and similar rocks, may be rounded, pumice-like, and their colour is quite characteristic, as it is often slighly violet-black to violet gray (although the burning heap samples are often orange, sometimes with green internal parts, resembling the "fake" bricks), but I've also seen yellow, light gray and white examples; slags are exclusively formed from the carbonate rocks (and thus don't fit to most "industrial slags"); parabasalts in the heaps are actually quite scarce.
7th Jan 2017 15:43 UTCUwe Kolitsch Manager
Thanks for your observations.
22nd Jan 2017 16:31 UTCPhilip Bluemner Expert
which locality is this about?
Philip
22nd Jan 2017 16:43 UTCUwe Kolitsch Manager
22nd Jan 2017 16:49 UTCJolyon Ralph Founder
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