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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
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The Balcones and Mexia fault zones are groups of tension fractures curving about the eastern and southern sides of the Llano uplift. This paper describes experiments which show that the subsidence of the coastal plain region, resisted by the support of the Llano positive element, would cause tension fractures curving about the eastern and southern sides of the Llano uplift. A bibliography accompanies the paper.
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