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Economic Geology; October 1961; v. 56; no. 6; p. 1088-1102
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The stratigraphic succession and structure in the Zinc Corporation Ltd. and New Broken Hill Consolidated Ltd., Broken Hill, New South Wales

D. S. Carruthers, and R. D. Pratten

Data from diamond drilling have demonstrated repetition of certain distinctive rock types (granitic gneiss, amphibolite, bedded iron formation, and so-called Potosi gneiss) formerly thought to occur at only one horizon in the Broken Hill succession. As a result, the structure which contains the lead and zinc lodes, once considered anticlinal, is now interpreted as a drag fold on the steeply dipping eastern limb of a major syncline (the Hanging Wall Basin).

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