About This Item
- Full text of this item is not available.
- Abstract PDFAbstract PDF(no subscription required)
Share This Item
The AAPG/Datapages Combined Publications Database
Fort Worth Geological Society
Abstract
ABSTRACT: Ichnology and Sedimentology of Shallow Marine Sandstone Reservoirs: Sequence
Stratigraphy, Depositional Environments and Effects of Bioturbation Upon
Reservoir
Performance and
Properties
Reservoir
Performance and
Properties
By
Pacheron Group, McKinney,
TX
Adjunct Assistant Professor, TCU
Professor of Geology, Texas Christian University
This one day course is designed to provide participants with a working knowledge of the physical and biological processes operating in shallow-marine depositional-systems.
Taken together, current-produced sedimentary structures and trace fossils permit a more
refined interpretation of depositional setting (and likely
reservoir
behavior) than is
possible when either sedimentology or ichnology are considered separately. The course
combines lecture and hands-on work with core, with an emphasis on the application of
ichnology to
petroleum
exploration and
reservoir
evaluation. Modern examples include
the mesotidal barrier islands and inlets of the Carolinas and Georgia, the macrotidal
embayments in Alaska, Canada and Scotland, and the Mississippi Delta.
Reservoir
studies will be presented in montages for all participants to review and will include the
Frio Formation of the Gulf Coast, the Sag River Sandstone of North Slope, and the
Bridgeport Sandstone of Wytch Farm, England. Core and data sets from the Ferron Sandstone of the Western Interior, the Sag River
Sandstone, the St Petersburg Sandstone from the Michigan Basin, and the SubClarksville
sandstone from the East Texas Basin will be available for participants to study. Case
histories will explain the sequence stratigraphy and depositional setting of these
sandstones, and also demonstrate the nature of the flow units in the reservoirs. The effects
of bioturbation on
reservoir
properties
and production performance can be demonstrated
and quantified for each sandstone.