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- Fiamme abstract "Fiamme are lens-shapes, usually millimetres to centimetres in size, seen on surfaces of some volcaniclastic rocks. They can occur in welded pyroclastic fall deposits and in ignimbrites, which are the deposits of pumiceous pyroclastic density currents. The name fiamme comes from the Italian word for flames, describing their shape. The term is descriptive and non-genetic.Fiamme are most typical of welded lapilli-tuffs and are commonly found in association with eutaxitic textures, best seen under the microscope.Some fiamme represent fragments of volcanic ejecta, often pumice lapilli that have been flattened by compaction and/or shear. Some fiamme are formed from flattened hot, relatively low viscosity, high porosity fragments of volcanic glass or pumice. But this is not the only way they can form: they can also form when pumice lapilli are altered to clay and compact during diagenesis; and fiamme are also widely reported in viscous lavas (andesites to rhyolites) where they form by shear-induced autobrecciation of pumiceous or obsidian zones, followed by shear and annealing of the fragments. Fiamme can also result from patchy alteration and recrystalisation of volcanic rocks, or by patchy revesiculation of welded tuff matrix (especially in rheomorphic peralkaline tuffs).".
- Fiamme thumbnail FiammeRestingSpringTuff031811.jpg?width=300.
- Fiamme wikiPageID "3495345".
- Fiamme wikiPageLength "2166".
- Fiamme wikiPageOutDegree "29".
- Fiamme wikiPageRevisionID "666456013".
- Fiamme wikiPageWikiLink Agglomerate.
- Fiamme wikiPageWikiLink Andesite.
- Fiamme wikiPageWikiLink Breccia.
- Fiamme wikiPageWikiLink Category:Petrology.
- Fiamme wikiPageWikiLink Category:Tephra.
- Fiamme wikiPageWikiLink Clay_minerals.
- Fiamme wikiPageWikiLink Diagenesis.
- Fiamme wikiPageWikiLink Eutaxitic_texture.
- Fiamme wikiPageWikiLink Ignimbrite.
- Fiamme wikiPageWikiLink Lapilli.
- Fiamme wikiPageWikiLink Matrix_(geology).
- Fiamme wikiPageWikiLink Obsidian.
- Fiamme wikiPageWikiLink Peralkaline.
- Fiamme wikiPageWikiLink Peralkaline_rock.
- Fiamme wikiPageWikiLink Porosity.
- Fiamme wikiPageWikiLink Pumice.
- Fiamme wikiPageWikiLink Pyroclastic_flow.
- Fiamme wikiPageWikiLink Revesiculation.
- Fiamme wikiPageWikiLink Rhyolite.
- Fiamme wikiPageWikiLink Rock_microstructure.
- Fiamme wikiPageWikiLink Shear_(geology).
- Fiamme wikiPageWikiLink Tuff.
- Fiamme wikiPageWikiLink Vesicular_texture.
- Fiamme wikiPageWikiLink Viscosity.
- Fiamme wikiPageWikiLink Volcanic.
- Fiamme wikiPageWikiLink Volcanic_glass.
- Fiamme wikiPageWikiLink Volcano.
- Fiamme wikiPageWikiLink Welded_tuff.
- Fiamme wikiPageWikiLink File:BishopTuff.jpg.
- Fiamme wikiPageWikiLink File:FiammeRestingSpringTuff031811.jpg.
- Fiamme wikiPageWikiLinkText "Fiamme".
- Fiamme wikiPageWikiLinkText "fiamme".
- Fiamme hasPhotoCollection Fiamme.
- Fiamme wikiPageUsesTemplate Template:Reflist.
- Fiamme wikiPageUsesTemplate Template:Volcanology-stub.
- Fiamme subject Category:Petrology.
- Fiamme subject Category:Tephra.
- Fiamme type Subfield.
- Fiamme comment "Fiamme are lens-shapes, usually millimetres to centimetres in size, seen on surfaces of some volcaniclastic rocks. They can occur in welded pyroclastic fall deposits and in ignimbrites, which are the deposits of pumiceous pyroclastic density currents. The name fiamme comes from the Italian word for flames, describing their shape.".
- Fiamme label "Fiamme".
- Fiamme sameAs m.09gmf5.
- Fiamme sameAs Фьямме.
- Fiamme sameAs Q4493802.
- Fiamme sameAs Q4493802.
- Fiamme wasDerivedFrom Fiamme?oldid=666456013.
- Fiamme depiction FiammeRestingSpringTuff031811.jpg.
- Fiamme isPrimaryTopicOf Fiamme.