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Sedimentary rock made of large grains, usually of calcium carbonate
Pisoids in the Conococheague limestone (Upper Cambrian) of eastern Pennsylvania
Pisolitic limestone; Itaboraí , Rio de Janeiro , Brazil; pisolith diameters average 1.0 cm
QEMSCAN mineral map of bauxite forming pisoids
A pisolite (from Ancient Greek πίσον (píson) 'pea ') is a sedimentary rock made of pisoids , which are concretionary grains – typically of calcium carbonate which resemble ooids , but are more than 2 mm in diameter. These grains are approximately spherical and have concentric layers reaching 10 mm in diameter.
Bauxites , limonites , and siderites often have a pisolitic structure.
See also
References
Mindat - Pisolite
Further reading
Manutchehr-Danai, Mohsen (2009). Dictionary of gems and gemology (3rd ed.). Springer. ISBN 978-3-540-72795-8 .
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