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Impact ejecta from the Albion Formation are exposed in northern Belize. The ejecta come from the outer portion of the continuous ejecta blanket of the Chicxulub crater, which is located 360 km to the northwest. The basal unit of the Albion Formation is a ¾1-m-thick clay and dolomite spheroid bed composed of up to four discrete flows. The clay spheroids are(More)
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