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Title: Structural and depositional evolution of the East

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5905728
 [1];  [2];  [3]
  1. Savannah River Group, Westinghouse, Aiken, SC (United States)
  2. Univ. of Texas, Dallas, TX (United States)
  3. Univ. of South Carolina, Columbia, SC (United States)

The East Slovakian Basin, eastern Czechoslovakia, is a Neogene back-arc extensional and transtensional basin that formed during east and northeast shortening across the Outer Carpathian fold and thrust belt. Analysis of seismic, well log and outcrop data indicate three principal phases of structural evolution: (1) Early transtension, (2) Basin-wide downwarping, and, (3) Late compression and transpression. Initial clastic deposition occurred in the northwest corner of the present-day basin during Egerian/Eggenburgian time. Sedimentation accompanied increasing subsidence through the Karpatian, Badenian and into the Lower Sarmatian. Following Sarmatian time the rate of sedimentation slowed, and deposition was restricted to the southeastern part of the basin. Deposition occurred in a shallow marine to transitional environment, becoming more terrestrial through time. Early deposition occurred along an east to southeast axis with the depocenter axis rotating through time in a clockwise direction. The East Slovakian Basin has been heavily explored and is currently producing predominantly dry gas from five different fields. Wet gas is produced only from the Ptruksa anticline, a phase one structure while dry gas is produced from phase three structural traps. This implies that late-forming hydrocarbon traps combined with high heat flow may preclude the entrapment of liquid phase hydrocarbons.

OSTI ID:
5905728
Report Number(s):
CONF-921058-; CODEN: GAAPBC
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Vol. 24:7; Conference: 1992 annual meeting of the Geological Society of America (GSA), Cincinnati, OH (United States), 26-29 Oct 1992; ISSN 0016-7592
Country of Publication:
United States
Language:
English