BEGIN:VCALENDAR VERSION:2.0 METHOD:PUBLISH PRODID:-//Tendenci - The Open Source AMS for Associations//Tendenci Codeba se MIMEDIR//EN BEGIN:VEVENT DESCRIPTION:--- This iCal file does *NOT* confirm registration.\nEvent det ails subject to change. ---\nhttps://www.swsaapg.org/events/24/\n\nEvent T itle: 2012 Bill Hailey Memorial Short Course\nStart Date / Time: Jan 10, 2 012 02:00 AM US/Central\nLocation: TCU Brown-Lupton University Union Audit orium\nSpeaker: Dr. Peter A. Scholle\nGoogle\nhttp://maps.google.com/maps? q=2901+Stadium+Drive,Ft. Worth,TX\n\nForecast\nhttp://www.weather.com/weat her/monthly/\n\n\n \n \n \n \n Southwest Section\n \n Ame rican Association of Petroleum Geologists\n \n Presents the 2012 Bi ll Hailey Memorial Short Course\n \n \n \n Studies of Late Paleozoic outcrops and modern sediments \n \n relevant to Penn-Perm hydrocarbon exploration\n \n by Dr. Peter A. Scholle\n \n \ n \n REGISTRATION\n \n \n \n \n \n Monday, Janua ry 9, 2012 \n \n Hardin-Simmons University \n \n Johnson Building Multipurpose Rm.\n \n Am bler &\; Hickory Streets, north Abilene\n \n \n \n Tuesd ay, January 10, 2012\n \n Texas Christian University\n \n Au ditorium, Brown-Lupton University Union\n \n 2901 Stadium Drive, Ft . Worth, TX\n \n \n \n \n \n \n \n \n Registration is now open. Please complete the bottom part of the Registration Form\; then follow the "\;Payable to"\; and &quo t\;Mail to"\; instructions corresponding to the date and location you wish to attend.\n \n \n \n \n \n \n \n \n \n \n \n \n Persian Gulf tidal flat - analog of the Per mian of West Texas.\n \n \n \n Studies of Late Paleozoic outcro ps and modern sediments relevant to Penn-Permhydrocarbon exploration\n \ n \n \n Understanding carbonate reservoirs of different ages is c omplicated by evolutionary trends of organisms (especially as punctuated b y major extinctions events) and by changes in climate and tectonic regimes . The Upper Paleozoic of Texas and New Mexico is a fine example of such i nterpretive complexities. The Late Devonian extinction event decimated r eef-building faunas, so Mississippian strata have no barrier reefs and har dly any reefal deposits of any sort. In the absence of barriers, open she lf and slope deposits predominate and range from crinoidal grainstones to organic-rich mudstones that are interspersed with small, muddy bryozoan/mi crobe buildups. By Pennsylvanian time, phylloid algae and fusulinid foram infers had evolved and combined with corals, red algae and other organisms to produce widespread mounds and buildups. These, however, were generall y small in overall size and thus rarely formed restrictions to open shelf water circulation. Active tectonics and repeated glacioeustatic sea-level changes in the Late Pennsylvanian led to extensive meteoric alteration of these rocks, with locally extensive secondary porosity development . By Mid-Permian time, continued faunal evolution led to the development of maj or reef complexes, including the sponge/algal/microbial/cement barriers of the Permian Basin. Coupled with waning southern hemisphere glaciations a nd cessation of collisional tectonics, this led to widespread restricted s helves with thick evaporates, associated dolomites and spectacular reservo irs.\n \n \n \n Modern analogs are typically used to gain an un derstanding of the processes and environments of carbonate sediment format ion. But these three &ldquo\;different worlds&rdquo\; of Paleozoic sedime ntation require judicious selection and &ldquo\;blending&rdquo\; of modern analogs from a wide range of locations, coupled with outcrop studies of M ississippian to Permian strata, to make real sense of the depositional and diagenetic patterns found in the diverse Late Paleozoic reservoirs of the southwest. No single analog can suffice to model these complex strata, a nd there can be no simple model for understanding the porosity distributio n in those reservoirs. But modern and ancient analog studies at least all ow an understanding of the processes involved in both deposition and diage nesis and that knowledge can significantly improve exploration modeling.\n \n \n\n\n\n\n\n--- This iCal file does *NOT* confirm registration.Event details subject to change. ---\n\n--- By Tendenci - The Open Source AMS fo r Associations ---\n UID:uid24@swsaapg.org SUMMARY:2012 Bill Hailey Memorial Short Course DTSTART:20120110T080000Z DTEND:20120110T170000Z CLASS:PUBLIC PRIORITY:5 DTSTAMP:20260405T175654Z TRANSP:OPAQUE SEQUENCE:0 LOCATION:TCU Brown-Lupton University Union Auditorium X-ALT-DESC;FMTTYPE=text/html:
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Event Title: 2012 Bill Hailey Memorial Short Course

https://www.swsaapg.org/events /24/

When: Jan 10, 2012 02:00 AM US/Central
Spea ker: Dr. Peter A. Scholle

TCU Brown-Lupton University Union Aud itorium
2901 Stadium Drive
Ft. Worth, TX
http://maps.g oogle.com/maps?q=2901+Stadium+Drive,Ft. Worth,TX

Forecast: http://www.weather.com/weather/monthly/


Southwest Section
American Association of Petroleum Geologists
Presents the 2012 Bill Hailey Memorial Short Course
 \;
Studies of Late Paleozoic outcrops and modern sediments
relevant to Penn-Permhydrocarbon explorati on
by < strong>Dr. Peter A. Scholle
& nbsp\;
 \;
Monday, January 9, 2012 \; \; \; \; \;&n bsp\; \; \; \; \; \; \; \;
Hardin-Simmons University \;  \; \; \;  \; \; \; \; \; \; \; \; \; \;&nbs p\; \; \; \; \;  \; \; \; \;
Johnson Building Multipurpose Rm.
Ambler &\; Hickory Streets, north Abilene
 \;
Tuesday, Janu ary 10, 2012
Texas Christian Univers ity
Auditorium, Brown-Lupton Univers ity Union
2901 Stadium Drive, Ft. Wo rth, TX
 \;
 \;
 \; \;
 \;< /div>
Persian Gulf tidal flat - analog of the Permian of West Texas.
 \;
Studies of Late Paleozoic outcrops and mo dern sediments relevant to Penn-Permhydrocarbon explorati on
 \;
Understanding carbonate reservoirs of different ages is complicated by evolutionary trends of organisms (especially as pu nctuated by major extinctions events) and by changes in climate and tecton ic regimes. \; The Upper Paleozoic of Texas and New Mexico is a fine e xample of such interpretive complexities. \; \; The Late Devonian extinction event decimated reef-building faunas, so Mississippian strata h ave no barrier reefs and hardly any reefal deposits of any sort. \; In the absence of barriers, open shelf and slope deposits predominate and ra nge from crinoidal grainstones to organic-rich mudstones that are interspe rsed with small, muddy bryozoan/microbe buildups. \; By Pennsylvanian time, phylloid algae and fusulinid foraminfers had evolved and combined wi th corals, red algae and other organisms to produce widespread mounds and buildups. \; These, however, were generally small in overall size and thus rarely formed restrictions to open shelf water circulation. \; Ac tive tectonics and repeated glacioeustatic sea-level changes in the Late P ennsylvanian led to extensive meteoric alteration of these rocks, with loc ally extensive secondary porosity development .  \;By Mid-Permian time , continued faunal evolution led to the development of major reef complexe s, including the sponge/algal/microbial/cement barriers of the Permian Bas in. \; Coupled with waning southern hemisphere glaciations and cessati on of collisional tectonics, this led to widespread restricted shelves wit h thick evaporates, associated dolomites and spectacular reservoirs.
 \;
Moder n analogs are typically used to gain an understanding of the processes and environments of carbonate sediment formation. \; But these three &ldq uo\;different worlds&rdquo\; of Paleozoic sedimentation require judicious selection and &ldquo\;blending&rdquo\; of modern analogs from a wide range of locations, coupled with outcrop studies of Mississippian to Permian st rata, to make real sense of the depositional and diagenetic patterns found in the diverse Late Paleozoic reservoirs of the southwest. \; No sing le analog can suffice to model these complex strata, and there can be no s imple model for understanding the porosity distribution in those reservoir s. \; But modern and ancient analog studies at least allow an understa nding of the processes involved in both deposition and diagenesis and that knowledge can significantly improve exploration modeling.
--- This iCal file does *NOT* confi rm registration.Event details subject to change. ---
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