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<br /> <br />(,:;. <br />(.:J <br />o <br />(.:;l <br />-..1 <br />CO <br /> <br />2. deep-basin deposits which range in depth from <br />200 to 5,000 feet, and are mined solely by in <br />situ recovery methods. <br /> <br />The principal deposits of near-surface lignite occur in the <br />Wilcox Group and are classified by Kaiser according to origin <br />as iluvial, deltaic, or lagoonal. Fluvial lignites are associated <br />with overbank deposits of stream systems and have a high percentage <br />of woody material but low sulfur ~ontent. Deltaic deposits <br />of lignite occur in association with delta-front sequences, <br />interdistributary deposits, and meanderbeltdeposits. The most <br />commercially significant deposits are associated with the delta <br />plain. Primarily nonwoody, deltaie lignite results from a <br />marsh environment. Lagoonal lignite has a high sulfur and ash <br />content, possibly reflecting a salt marsh environment (Kaiser, <br />1974).1' , <br /> <br />Deep-basin lignite resources have not been extensively studied <br />but apparently are related to fluVial systems in the Wilcox <br />Group. <br /> <br />Surface and subsurface coal deposits occur in the Pennsylvanian <br />rocks of North-Central Texas. The coal deposits are associated <br />with fluvial-deltaic facies tracts in the Straw~ Canyon and <br />Cisco Groups. As defined by T.J. Evans (1974)_/bituminous c,oa1 <br />contains approximately 86% fixed carbon (dry basis) and has <br />heating values of 11,000 btu/lb, In the late 1800's, a coal mine <br />was producing from the Cisco Group :!.n'Montague County; 'however, <br />abundant oil and gas undercut the coal market and most mines were <br />closed by 1928. <br /> <br />At present, there are two active or recently active uranium mines <br />in the region. These deposits are small, off..urring in the <br />Triassic redbeds. According to F1awn, (1967)_the uranium was most <br />probably deposited by precipitation from circulating ground <br />water in conglomeratic sandstone. <br /> <br />The petroleum and natural gas p~oduction in the Arkansas-White-Red <br />region comprises 5% and 18% respectively of the State's total <br />production. During 1972, several deep gas fields, 18,000 to <br />21,000 feet in depth, were discovered in the Anadarko Basin, <br />Wheeler County. The majority of the petroleum production <br />is in the Levelland-Slaughter_San Andres trend in Cochran and <br />Hockley Counties ~exas Gulf Region), and' in the Anadarko' Basi,n <br />along the Red River, , , <br /> <br />11 <br /> <br />Kaiser, W, R" 1974, Texas Li~nite: Near-Surfaee and <br />Deep Basin Resourc~s, Bureau of Economic Geology, University <br />of Texas at Austin, Report of Investigations, 76. <br /> <br />Evans, T. J" 1974, Bituminous Coal in Texas, Bureau of <br />Economic Geology, University of Texas at Austin, Handbook 4. <br /> <br />F1awn, P. T., 1967, Uranium in,Texas-1967, Bureau of <br />Economic Geology, University of Texas at Austin, Geological <br />Circular 67-1. 136 <br /> <br />]j <br /> <br />]..1 <br /> <br />. <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />