Gabbro
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| Did you know | Long belts of gabbro intrusions are typically formed at proto-rift zones and around ancient rift zone margins. |
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| Address | Vişnezade, Acısu Sokaği No:19, 34357 Beşiktaş/İstanbul |
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| ID | 1354248 |
About Gabbro
Gabbro is a phaneritic, mafic intrusive igneous rock formed from the slow cooling of magnesium-rich and iron-rich magma into a holocrystalline mass deep beneath the Earth's surface. Slow-cooling, coarse-grained gabbro is chemically equivalent to rapid-cooling, fine-grained basalt.
Where is the Gabbro
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Gabbro Photos
