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TABLE 8.-Average mineral composition, in percent, of sand. <br /> stones from the Salt Wash Member of the Morrison Formation <br /> - IBaed on model ppooint counts tt200 points) and model estimate of thin sections. <br /> TABLE 5.-Comparison of average mineral tompoeilion of ean� "Minor'gw=India"la.than 0.25 percent) <br /> stones from the Salt Wash ember, Slick Rock district, with <br /> that of eandetonee from the Salt Wash Member throughout the Component iwa, MidaIImi <br /> Colorado Plateau uninit i <br /> Slim Rock district Quartz grains and overgrowtha----_ 78 77.5 75' <br /> Colorado Chert_-- 7 2 0.5 <br /> Component Orthoclase----------------------- 10 3.5 4. 5 <br /> Point Modal Average Plateau r counts etaaae Microcliae----------------------- 1 .5 .5 <br /> Plagioclace----------------------- I 1 1 <br /> uartz_____.----- <br /> 72.3 71. 7 72.0 71.4 Rock fragments and mineral aggre- <br /> Q gates-------------------------- 2 Minor Minor <br /> Quarts oveegrowtha____._. 4.3 4.3 4.3 4 Clay (mineral clay and clay-sited <br /> Chert-------------------- 4.8 8.4 5.8 5.8 detritus)----------------------- Minor 1 2 <br /> K-feldspar--------------- 2. 7 5.3 4.0 l 5.8 Calcite and dolomite-------------- 2 13 9 <br /> Plagioclase--------------- .8 .9 Ba rite----------_---------------- Minor -------- Minor <br /> Calcite------------------ 8.2 S. 5 8. 3 13 Chlorite------------------------- Minor Minor Minor <br /> Clay____________________ 2. 1 29 2.5 -------- Hematite and other black opaque <br /> Other- 5.0 -------- 2.5 -------- minerals_______________________ Minor .5 Minor <br /> Biotite__________________________________ Minor Minor <br /> Number of samples------- 19 19 38 202 Muscovite_______________________________________ Minor <br /> Leucozene and anatsse------------ Minor Minor Minor <br /> Limonite----------------------------- ----- --_ Minor <br /> Analyzed b7 B. A. Cadillac,olgilatsd fines dataof Craig and oxen, (IOU Pyrite____________________ <br /> p.lna.z). -'----------'-- Minor -------- <br /> Number of samples--------------- 1 3 14 <br /> TABLr, 7.Average mineral composition in percent, of silGtones <br /> from the Salt Wash Member of the korruon Formation TABLE Salt innash al composit <br /> _of the,in per , <br /> F rmaiion�from the <br /> [Based on modal point wants (2m points) and modal estimates of thin sections. <br /> "Minor'generally indicates lea than om pa all (Bawd an modal etimates of thin section."Minor^ generally Indicates Im than <br /> 0.25 perwati <br /> Component Lower Middle u <br /> unit unit cat Component Iowa Middle <br /> unit unit <br /> Quartz grains and overgrowths_____ 50 45 52.5 <br /> Chert---_________________ _ 5 5 3.5 Quartz grains and overgrowths------------- 28 30 <br /> Orthoclase----- 5 5 3 Chert----------------------------------- 3 4 <br /> Microcline 1 2 .5 Orthoclase --------------- 2 3 <br /> Plagioclase 3 2 .5 Microcline--------------------------------------- I <br /> Clay (mineral clay and clay-sized Plagioclase------------------------------- I I <br /> detritus)----------------------- 25 30 12 Clay------------------------------------ 85 15 <br /> Calcite-------------------------- 10 10 27 Calcite and dolomite---------------------- 2 45 <br /> Chlorite_________________________ Minor Minor Minor Hematite and other black opaque minerals----------- 1 <br /> Hematite 'and other black opaque Blotite------------------------------- Minor --- <br /> minerals----------------------- Minor Minor ------- Muscovite------------------------------- Minor Minor <br /> Biotite----'-------------------------- ------- Minor Leucozene Minor Minor <br /> Muscovite_______________________ Minor -------- Minor Pyrite-.--------------------------------- Minor --______ <br /> Leucozene Minor Minor Minor Carbonaceous material-------------------- 1 -----'-- <br /> Limonite________________________________________ Minor <br /> Number of samples----------------------- 1 1 <br /> Number of eamples________________ 1 1 2 <br /> Mineral Composition of Salt wash rocks in the Slick Rock District <br /> (from Shawe, 1968) . <br />