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- Q567788 subject Q6431951.
- Q567788 subject Q7348574.
- Q567788 subject Q8767031.
- Q567788 abstract "Anorthosite /ænˈɔːrθəsaɪt/ is a phaneritic, intrusive igneous rock characterized by a predominance of plagioclase feldspar (90–100%), and a minimal mafic component (0–10%). Pyroxene, ilmenite, magnetite, and olivine are the mafic minerals most commonly present.Anorthosite on Earth can be divided into two types: Proterozoic anorthosite (also known as massif or massif-type anorthosite) and Archean anorthosite. These two types of anorthosite have different modes of occurrence, appear to be restricted to different periods in Earth's history, and are thought to have had different origins.Lunar anorthosites constitute the light-coloured areas of the Moon's surface and have been the subject of much research.".
- Q567788 thumbnail Anorthosit_of_Salem_Tamil_Nadu.jpg?width=300.
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- Q567788 wikiPageExternalLink abstract_51333.htm.
- Q567788 wikiPageExternalLink Anorthosite.htm.
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- Q567788 type Thing.
- Q567788 comment "Anorthosite /ænˈɔːrθəsaɪt/ is a phaneritic, intrusive igneous rock characterized by a predominance of plagioclase feldspar (90–100%), and a minimal mafic component (0–10%). Pyroxene, ilmenite, magnetite, and olivine are the mafic minerals most commonly present.Anorthosite on Earth can be divided into two types: Proterozoic anorthosite (also known as massif or massif-type anorthosite) and Archean anorthosite.".
- Q567788 label "Anorthosite".
- Q567788 differentFrom Q244994.
- Q567788 depiction Anorthosit_of_Salem_Tamil_Nadu.jpg.
