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In addition to the minerals shown in the Graph of Changes in Mineral Composition Within the Palisades Sill, two other minerals commonly found in diabase samples are olivine and biotite. Olivine can be present in some mafic igneous rocks, while biotite is often associated with the presence of other ferromagnesian minerals. The specific composition of diabase can vary, leading to the potential for these minerals to be included in certain samples.

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