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

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68 ILLINOIS BASIlV COAL RESOURCES<br />

<strong>the</strong> heavier portions <strong>of</strong> <strong>the</strong> <strong>coal</strong> are likely<br />

to concentrate in <strong>the</strong> samples <strong>and</strong> thus may<br />

have a higher sulfur content than <strong>the</strong> <strong>coal</strong><br />

as a whole. The fairly high sulfur content<br />

<strong>of</strong> <strong>the</strong>se samples probably indicates a relatively<br />

high sulfur content in <strong>the</strong> bed.<br />

OIL AND GAS RESOURCES<br />

Although <strong>the</strong> structure maps accompanying<br />

this report provide a general picture <strong>of</strong><br />

<strong>the</strong> "lay" <strong>of</strong> <strong>the</strong> <strong>coal</strong>-bearing strata in Edwards<br />

County, <strong>the</strong>y are not designed to delineate<br />

oil <strong>and</strong> gas structures. In <strong>the</strong> first<br />

place, not all available data were used, <strong>and</strong><br />

in <strong>the</strong> second place, <strong>the</strong> structure has been<br />

delineated according to engineering methods,<br />

without <strong>the</strong> liberties in interpretation that<br />

usually characterize oil <strong>and</strong> gas structure<br />

mapi. Consequently <strong>the</strong> structural irregularities<br />

shown, although <strong>the</strong>y may correspond<br />

in some places with <strong>the</strong> position <strong>of</strong><br />

oil <strong>and</strong> gas pools, can scarcely be expected<br />

to do so consistently, <strong>and</strong> <strong>the</strong> maps are not<br />

regarded as particularly suitable for forecasting<br />

<strong>the</strong> position <strong>of</strong> undiscovered oil <strong>and</strong><br />

gas accumulations.<br />

CONCLUSION<br />

In this study <strong>of</strong> <strong>the</strong> Pennsylvanian beds<br />

<strong>of</strong> Edwards County emphasis has been<br />

placed upon <strong>the</strong> <strong>coal</strong> beds <strong>and</strong> limestones<br />

in <strong>the</strong> McLeansboro <strong>and</strong> Carbondale groups.<br />

The stratigraphic logs compiled from cuttings<br />

carefully collected from control wells<br />

at close intervals <strong>and</strong> drilling time records<br />

<strong>of</strong> <strong>the</strong> same drill holes have been <strong>the</strong> principal<br />

source <strong>of</strong> information. They have provided<br />

a means <strong>of</strong> interpreting electric logs<br />

<strong>of</strong> adjacent drill holes. Study has been<br />

made <strong>of</strong> about 330 such electric logs <strong>and</strong> <strong>of</strong><br />

<strong>the</strong> logs <strong>and</strong> cuttings from two cable-tool<br />

holes. Much more detailed information in<br />

regard to <strong>the</strong> stratigraphic succession in <strong>the</strong><br />

McLeansboro <strong>and</strong> Carbondale groups is<br />

available in <strong>the</strong> cuttings that have been collected<br />

from <strong>the</strong> control wells than was<br />

possible or necessary to assemble for <strong>the</strong><br />

purposes <strong>of</strong> <strong>the</strong> present report. This is<br />

particularly true <strong>of</strong> <strong>the</strong> beds above <strong>the</strong> West<br />

Franklin limestone <strong>and</strong> those below <strong>the</strong><br />

Palzo s<strong>and</strong>stone.

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