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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…
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volcanic welded fragments pumice also pumiceous lapilli shear seen rocks flattened ignimbrites viscosity porosity clay diagenesis andesites rhyolites autobrecciation obsidian
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