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A Chemical Classification of Volcanic Rocks Based on the Total Alkali-Silica Diagram

Bibliographic Data

ID23326366
AuthorsM J L BAS, M J Le Bas (University of Leicester), R W Le Maitre (The University of Melbourne), R W L MAITRE, A STRECKEISEN, Bruno Zanettin (University of Padua), IUGS Subcommission on the Systematics of Igneous Rocks
Year1986
Volume27
Issue3
Pages745-750
Publication date1986-06-01
Peer ReviewedYes
Open AccessNo
TypeARTICLE
VenueJournal of Petrology (JOURNAL)
Journal identifiersISSN: 0022-3530 • E-ISSN: 1460-2415
PublisherOxford University Press (OUP) (PUBLISHER)
DOI10.1093/petrology/27.3.745
OpenAlexW2157099954
LanguageEN
Citations received150

This contribution summarizes and brings up to date the recommendations made by the IUGS Subcommission on the Systematics of Igneous Rocks for the classification of volcanic rocks when modal analyses are lacking. The classification is on a non-genetic basis using the total alkali-silica (TAS) diagram, and is as nearly consistent as possible with the QAPF modal classification. The diagram is divided into 15 fields, two of which contain two root names which are separated according to other chemical criteria, giving the following 17 root names: basalt, basaltic andesite, andesite, dacite, rhyolite, trachybasalt, basaltic trachyandesite, trachyandesite, trachyte, trachydacite, picrobasalt, basanite, tephrite, phonotephrite, tephriphonolite, phonolite and foidite. Using Na-K criteria, trachybasalt may be further divided into the sub-root names hawaiite and potassic trachybasalt, basaltic trachyandesite into the sub-root names mugearite and shoshonite, and trachyandesite into the sub-root names benmoreite and latite.

Andesite · Basalt · Geochemistry · Rhyolite · Trachyte · Volcanic rock · Volcano · Clay minerals and soil interactions · Geochemistry and Geologic Mapping · Geological and Geochemical Analysis · Geology

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Unique citing works150
Citations per year4,55
Citation span1993 - 2026 (34)
Citation velocitycurrent
Highly citedYes
Citation typesNeutral: 126

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