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subsurface geology and coal resources of the pennsylvanian system ...

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ILLIATOIS BASIN COAL RESO URCES<br />

GARTER OIL COMPANY CARTER OIL COMPANY SOHlO PRODUCING COMPANY<br />

GALLATIN COUNTY NO. 20L<br />

GALLATIN COUNTY NO 246<br />

CRAWFORD,J.L .NO.3 CRAWFORD,J.L.,ND.4<br />

SEG.II,T.BS .R.IOE.<br />

SEC.II,T.IS.,R.IOE.<br />

POTENTIAL RESISTIVITY<br />

GALLATIN COUNTY NO 215<br />

CRAWFORD-WRIGHT-NATURAL RESOURCES<br />

SEC. lZ.TBS..R IOE.<br />

WEST FRANKLIN LIMESTONE<br />

tOP PALZO SANDSTD<br />

p DAVIS SANDSTONE<br />

;GP CURLEW SANDSTONE<br />

MURRAY BLUFF SANDSTONE<br />

lop PAL20 SANDSTONE<br />

ISV OELWOOD SANDSTONE<br />

~ J MURRAY V<br />

BLUFF SANDSTONE<br />

POUNDS SANDSTONE<br />

101 DELWDOD SANDSTONE<br />

aATTERY ROCK SANDSTONE ---<br />

fop PDUNOS SANDSTONE<br />

BATTERY ROCK SANDSTONE<br />

R iOE<br />

FIG. 13.-Graphic<br />

logs <strong>of</strong> three drill holes adjacent to <strong>the</strong> Inman East fault in Gallatin County,<br />

showing extent <strong>and</strong> nature <strong>of</strong> displacement.<br />

Bankston Fork <strong>and</strong> Jamestown<br />

lime-<br />

stones <strong>and</strong> A nail Rock s<strong>and</strong>stone.-The<br />

Bankston Fork <strong>and</strong> Jamestown limestones<br />

lie between <strong>the</strong> "No. 7" <strong>coal</strong> bed <strong>and</strong> <strong>the</strong><br />

Herrin limestone over wide areas in sou<strong>the</strong>rn<br />

Illinois. The Jamestown limestone,<br />

not over I feet thick <strong>and</strong> usually less, resembles<br />

<strong>and</strong> lies a few feet above <strong>the</strong> Herrin<br />

limestone. The two limestones are sepa-<br />

rated by <strong>the</strong> thin Jamestown <strong>coal</strong> bed which<br />

is usually only a few inches thick <strong>and</strong> accompanied<br />

by not more than a few inches<br />

<strong>of</strong> overlying dark gray shale <strong>and</strong> underlying<br />

clay.<br />

The two limestones are so nearly alike<br />

<strong>and</strong> so closely associated that <strong>the</strong>ir differentiation<br />

in electric logs is impossible. The<br />

Bankston Fork limestone is more definitely

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