experimental

Entry: pegmatite

URI: http://inspire.ec.europa.eu/codelist/MineralDepositGroupValue/pegmatite

Pegmatites tend to occur in the aureoles of granites in most cases, and are usually granitic in character, often closely matching the compositions of nearby granites. Pegmatites should thus represent exsolved granitic material which crystallises in the country rocks. However, an origin of pegmatite fluids by devolatilisation (dewatering) of metamorphic rocks is also envisaged. Pegmatites are coarse-grained rocks, mainly composed of quartz, feldspar and mica and are important because they often contain rare earth minerals and gemstones, such as aquamarine, tourmaline, topaz, fluorite, apatite and corundum, often along with tin and tungsten minerals, among others.

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is a Concept
submitted bySophie Chaduteau
accepted on 16 Jul 2026 11:52:37.280

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date accepted 16 Jul 2026 11:52:37.280
date submitted 16 Jul 2026 09:20:11.014
definition
entity pegmatite
source graph graph

item class Concept
label pegmatite
notation 05627144-5915-4388-bc34-1a5f43d9063e
register mineral deposit group value
status status experimental
submitter
account name s.chaduteau@brgm.fr
name Sophie Chaduteau

type register item
version info 2
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Definition

definition Pegmatites tend to occur in the aureoles of granites in most cases, and are usually granitic in character, often closely matching the compositions of nearby granites. Pegmatites should thus represent exsolved granitic material which crystallises in the country rocks. However, an origin of pegmatite fluids by devolatilisation (dewatering) of metamorphic rocks is also envisaged. Pegmatites are coarse-grained rocks, mainly composed of quartz, feldspar and mica and are important because they often contain rare earth minerals and gemstones, such as aquamarine, tourmaline, topaz, fluorite, apatite and corundum, often along with tin and tungsten minerals, among others.
in scheme Mineral Deposit Group Value
notation pegmatite
pref label pegmatite
type Concept

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