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- Q46947 subject Q8532081.
- Q46947 subject Q8594046.
- Q46947 subject Q8767031.
- Q46947 abstract "Gabbro /ˈɡæbroʊ/ refers to a large group of dark, often phaneritic (coarse-grained), mafic intrusive igneous rocks chemically equivalent to basalt. It forms when molten magma is trapped beneath the Earth's surface and slowly cools into a holocrystalline mass.Much of the Earth's oceanic crust is made of gabbro, formed at mid-ocean ridges. Gabbro is also found as plutons associated with continental volcanism. Due to its variant nature, the term "gabbro" may be applied loosely to a wide range of intrusive rocks, many of which are merely "gabbroic".".
- Q46947 thumbnail GabbroRockCreek1.jpg?width=300.
- Q46947 wikiPageExternalLink 176IGNE.HTML.
- Q46947 wikiPageExternalLink 060420_earth_drill.html.
- Q46947 wikiPageWikiLink Q1018732.
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- Q46947 wikiPageWikiLink Q8532081.
- Q46947 wikiPageWikiLink Q8594046.
- Q46947 wikiPageWikiLink Q8767031.
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- Q46947 comment "Gabbro /ˈɡæbroʊ/ refers to a large group of dark, often phaneritic (coarse-grained), mafic intrusive igneous rocks chemically equivalent to basalt. It forms when molten magma is trapped beneath the Earth's surface and slowly cools into a holocrystalline mass.Much of the Earth's oceanic crust is made of gabbro, formed at mid-ocean ridges. Gabbro is also found as plutons associated with continental volcanism.".
- Q46947 label "Gabbro".
- Q46947 depiction GabbroRockCreek1.jpg.