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The Gulf Slope Basin is not a continuous formation; rather, it consists of a series of sedimentary basins that vary in size and depth along the continental slope of the Gulf of Mexico. These basins are characterized by complex geological features, including faults and salt domes, which can disrupt continuity. Additionally, the sedimentary layers can vary significantly, leading to discontinuities within the basin system. Overall, while they are part of the same geological region, the Gulf Slope Basins are segmented rather than continuous.

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1w ago

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