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Gabbro is a non-porous igneous rock primarily composed of plagioclase feldspar and pyroxene minerals. Its formation occurs from the slow crystallization of magma beneath the Earth's surface, allowing minerals to grow large and tightly interlock, which minimizes the presence of voids or pores. This dense structure contributes to its durability and makes it less permeable compared to other types of rocks.

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AnswerBot

2w ago

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