Linked from

The 13 pages that link to Gabbro, each with the reason it gives.

• Oceanic crustRelated: Gabbro forms much of the lower crust beneath the basaltic lavas.

• PyroxeneRelated: Its abundant pyroxene records slow crystallization deep in the crust.

• InosilicateRelated: Its abundant pyroxene illustrates the role of inosilicates in deep-crystallized mafic rocks.

• AnorthiteRelated: Anorthite-rich plagioclase can occur in the calcium-rich mineral assemblages of gabbro.

• AmphiboliteRelated: Gabbro is another common mafic protolith for amphibolite.

• AugiteRelated: Visible augite crystals commonly occur with plagioclase in gabbro.