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Industrial minerals form through various geological processes, including weathering, sedimentation, and crystallization. They can originate from the alteration of existing rocks, the accumulation of sedimentary deposits, or the cooling and solidification of magma. Factors such as temperature, pressure, and chemical environment play crucial roles in their formation. Common examples include clay minerals, which form from the weathering of feldspar, and limestone, which develops from the accumulation of marine organisms' shells and skeletal remains.

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