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Chicxulub impact ejecta from Albion Island, Belize
Authors:Kevin O Pope  Adriana C Ocampo  Alfred G Fischer  Walter Alvarez  Bruce W Fouke  Clyde L Webster  Francisco J Vega  Jan Smit  AEugene Fritsche  Philippe Claeys
Institution:

a Geo Eco Arc Research, 3220 N Street NW, Suite 132, Washington, DC 20007, USA

b Jet Propulsion Laboratory, California Institute of Technology, MS 183-601, 4800 Oak Grove Drive, Pasadena, CA 91109, USA

c Department of Earth Sciences, University of Southern California, University Park, Los Angeles, CA 90089, USA

d Department of Geology and Geophysics, University of California, Berkeley, CA 94720, USA

e Department of Geology, University of Illinois at Urbana-Champaign, Urbana, IL 61801, USA

f Geoscience Research Institute, Loma Linda University, Loma Linda, CA 92350, USA

g Instituto de Geologia, Universidad Nacional Autonoma de Mexico, Ciudad Universitaria, Mexico D.F., Mexico

h Institute of Earth Sciences, Vrije Universiteit, de Boelelaan 1085, 1081 HV Amsterdam, Netherlands

i Department of Geological Sciences, California State University, Northridge, CA 91330, USA

j Museum für Naturkunde, Institut für Mineralogie, D-10115 Berlin, Germany

Abstract: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 not, vert, similar1-m-thick clay and dolomite spheroid bed composed of up to four discrete flows. The clay spheroids are altered impact glass, and the dolomite spheroids are accretionary lapilli. The upper unit is a not, vert, similar15-m-thick coarse diamictite bed containing altered glass, large accretionary blocks, striated, polished, and impacted cobbles, and rare shocked quartz. The abundance of accretionary clasts, evidence for atmospheric drag sorting, and the presence of multiple flows in the Albion Formation indicate that atmospheres play an important role in the formation of the outer portions of continuous ejecta blankets of large craters.
Keywords:ejecta  impact features  Chicxulub Crater  Belize
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