DCNR_20027572 - Pennsylvania Department of Conservation and ...
DCNR_20027572 - Pennsylvania Department of Conservation and ...
DCNR_20027572 - Pennsylvania Department of Conservation and ...
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KENN ET H HASSON <strong>and</strong> JOHN DENNISON, East T ennessee State Universi ty.<br />
Stratigraphy <strong>of</strong> Harrell Shale <strong>and</strong> Millboro. Harrell Shale <strong>of</strong> <strong>Pennsylvania</strong> is a<br />
tongue <strong>of</strong> the Millboro Shale black sha ly f acies <strong>of</strong> Virginia. The Tully Limestone<br />
forms a marker horizon associated w ith the Harrell <strong>and</strong> Millboro.<br />
JAM ES W. HEAD, Lunar Exploration <strong>Department</strong>, Bellcomm, Inc. Late<br />
Cayugan (Upper Silurian) <strong>and</strong> Helderbergian (Lower Devonian) Paleoenvironmental<br />
Stratigraphy <strong>and</strong> Basin Evolution.<br />
LOUIS HEYMAN, <strong>Pennsylvania</strong> Geological Survey. Subsurface Correlation<br />
Sections, Tully (M. Devon.) - Queenston (U. Ordov.). Establish stratigraphic<br />
framework for subsurface sedimentary petrology studies <strong>of</strong> various producing<br />
<strong>and</strong> potent ial oil <strong>and</strong> gas reservoirs in this part <strong>of</strong> the geologic section. T hese<br />
reservoir rocks are also potential waste disposal zones. Other zones <strong>of</strong> potential<br />
value (brine production, evaporites) will be indicated.<br />
WAYNE C. MARTIN <strong>and</strong> B. R. HENN ING ER, Miami University (Ohio) <strong>and</strong><br />
West Virginia University. The Mather <strong>and</strong> Hockingport s<strong>and</strong>stone lentils (<strong>Pennsylvania</strong>n<br />
<strong>and</strong> Permian) <strong>of</strong> t he Dunkard Basin, Pennsylvan ia, West Virginia, <strong>and</strong><br />
Ohio.<br />
W. C. MARTIN <strong>and</strong> D. M. LOREN, Miam i University (Oh io). Integrated Facies<br />
Analysis <strong>of</strong> the Dunkard Group.<br />
C. E. PROUTY, Michigan State University. Revision <strong>of</strong> the Chazy <strong>of</strong> <strong>Pennsylvania</strong>.<br />
The stratigraphy <strong>of</strong> the Chazy rocks is bei ng studied in regard to their<br />
lateral relationship between eastern <strong>and</strong> central Pennsy lvania; between eastern<br />
<strong>Pennsylvania</strong> <strong>and</strong> the Maryl<strong>and</strong> <strong>and</strong> Virginia ou tcrop; <strong>and</strong> to their subsurface<br />
extensions into western <strong>Pennsylvania</strong> <strong>and</strong> West Virginia. Measured sections <strong>and</strong><br />
most fossil collections have been made f rom the Pennsylvan ia outcrop.<br />
JOHN B. ROEN, U. S. Geological Survey. Stratigraphy <strong>of</strong> the Coal-bearing<br />
Rocks <strong>of</strong> the Monongahela <strong>and</strong> Dunkard Groups in t he Northern Part <strong>of</strong> the<br />
Dunkard Basi n. Fifteen regional stratigraphic cross sections have been constructed<br />
showing the correlation <strong>and</strong> facies t re nds <strong>of</strong> the coal-bearing rocks <strong>of</strong><br />
the Monongahela <strong>and</strong> Dunkard Groups in Ohio, <strong>Pennsylvania</strong>, <strong>and</strong> West V irginia.<br />
HARO LD B. ROLLINS, JACK DONAHUE, NORMAN FLINT, <strong>and</strong> RI CHA RD<br />
LUND, University <strong>of</strong> Pittsbu rgh . Depositional Environment <strong>of</strong> the Conemaugh<br />
in t he Appalachian Basin.<br />
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