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Science 11 July 1986:
Vol. 233. no. 4760, pp. 200 - 203
DOI: 10.1126/science.233.4760.200

Articles

The Acraman Impact Structure: Source of Ejecta in Late Precambrian Shales, South Australia

GEORGE E. WILLIAMS 1

1 The Broken Hill Proprietary Co. Ltd., Minerals Exploration Department, PO Box 860, Norwood, South Australia 5067, Australia, and Department of Planetary Sciences, Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721.

A major probable impact structure occurs in middle Proterozoic dacitic volcanics in the Gawler Ranges, central South Australia. The structure has an inner depressed area about 30 kilometers in diameter that contains the Lake Acraman salina, an intermediate depression or ring about 90 kilometers in diameter, and a possible outer ring approximately 160 kilometers in diameter. Outcrops of dacite in Lake Acraman are intensely shattered and contain shatter cones and multiple sets of shock lamellac in quartz grains. The Acraman structure is the largest probable impact structure known in Australia and is the likely source of dacitic ejecta found in late Precambrian marine shales some 300 kilometers to the east.

Submitted on December 2, 1985
Accepted on April 8, 1986


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