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Under the binocular microscope, mm and cm-scale sedimentary features, textures, color and HCleffervescence were described and logged. The cores were then laid out and photographed in their coreboxes, and as individual samples. It should be noted that the water that was used to help increase thecontrast as well as clean the core occasionally caused the core to break up, so in areas that were veryfissile, isopropyl alcohol was used lessen the damage to the cores.
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