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- Feldspathoid abstract "The feldspathoids are a group of tectosilicate minerals which resemble feldspars but have a different structure and much lower silica content. They occur in rare and unusual types of igneous rocks.Foid, contraction of the term feldspathoid, is applied to any igneous rock containing up to 60% modal feldspathoid minerals. For example, a syenite with significant nepheline present can be termed a ‘(nepheline)-bearing syenite’, or a ‘(nepheline)-syenite’, with the term (nepheline) replaceable by any 'foid' mineral. Such terminology is used in the Streckeisen (QAPF) classification of igneous rocks.".
- Feldspathoid wikiPageID "305429".
- Feldspathoid wikiPageRevisionID "600170838".
- Feldspathoid hasPhotoCollection Feldspathoid.
- Feldspathoid subject Category:Tectosilicates.
- Feldspathoid comment "The feldspathoids are a group of tectosilicate minerals which resemble feldspars but have a different structure and much lower silica content. They occur in rare and unusual types of igneous rocks.Foid, contraction of the term feldspathoid, is applied to any igneous rock containing up to 60% modal feldspathoid minerals.".
- Feldspathoid label "Feldespatoide".
- Feldspathoid label "Feldspathoid".
- Feldspathoid label "Feldspatoide".
- Feldspathoid label "Feldspatoide".
- Feldspathoid label "Foidit".
- Feldspathoid label "Foïdite".
- Feldspathoid label "Skaleniowce".
- Feldspathoid label "Veldspaatvervanger".
- Feldspathoid label "Фельдшпатоиды".
- Feldspathoid label "準長石".
- Feldspathoid sameAs Foidy.
- Feldspathoid sameAs Foidit.
- Feldspathoid sameAs Αστριοειδή.
- Feldspathoid sameAs Feldespatoide.
- Feldspathoid sameAs Foïdite.
- Feldspathoid sameAs Feldspatoide.
- Feldspathoid sameAs 準長石.
- Feldspathoid sameAs Veldspaatvervanger.
- Feldspathoid sameAs Skaleniowce.
- Feldspathoid sameAs Feldspatoide.
- Feldspathoid sameAs m.01sg2d.
- Feldspathoid sameAs Q1322038.
- Feldspathoid sameAs Q1322038.
- Feldspathoid wasDerivedFrom Feldspathoid?oldid=600170838.
- Feldspathoid isPrimaryTopicOf Feldspathoid.