Thrust faults that violate classic thrust belt rules: Marathon basin, Texas

Conference · Sun Apr 01 00:00:00 EST 1984 · Am. Assoc. Pet. Geol., Bull.; (United States)

OSTI ID:6871994

Demis, W D

One generally accepted rule of thrust belt geometry is that folding does not occur before thrust faulting; thrust do not cut across folds in cross-section view. Original mapping in the Marathon basin documents that the Hell's Half Acre thrust sheet was emplaced after an episode of large-scale folding. The Hell's Half Acre thrust fault is a shallow, low-angle fault which separates the northeasterly trending, broad (4-km or 2.5-mi wavelength), open folds on the north from the imbricately thrust faulted and overturned, tightly folded (1-km or 0.6-mi wavelength) Paleozoic rocks of the thrust sheet. The thrust fault trends east and truncates the structures on the north. Within the thrust sheet, folds plunge into and are truncated by thrust faults. The Tesnus Formation (Mississippian) is the principal formation of the sheet, but large blocks of younger Dimple Limestone (Morrowan) and Haymond Formation (Atokan) are lodged within fault planes bounded by Tesnus, thereby documenting folding thrust faulting. This nonclassic geometry is due to lithology. Classic thrust belt style was developed for a miogeoclinal sequence. The Ouachita stratigraphy is a eugeoclinal sequence composed of lower and middle Paleozoic, thin limestones and cherts with numerous shale interbeds and an upper Paleozoic flysch sequence with a low sand/shale ratio and numerous thick shale horizons. The many thick, incompetent horizons allowed the thrust fault to cut across preexisting structures.

• Research Organization: Pennzoil Exploration and Production Co., Denver, CO
• OSTI ID: 6871994
• Report Number(s): CONF-8405216-
• Journal Information: Am. Assoc. Pet. Geol., Bull.; (United States), Vol. 68:4; Conference: AAPG annual convention, San Antonio, TX, USA, 20 May 1984
• Country of Publication: United States
• Language: English

Related Subjects

02 PETROLEUM
03 NATURAL GAS
SEDIMENTARY BASINS
GEOLOGIC FAULTS
TEXAS
GEOLOGIC FORMATIONS
LIMESTONE
LITHOLOGY
MISSISSIPPIAN PERIOD
SHALES
CARBONATE ROCKS
FEDERAL REGION VI
GEOLOGIC AGES
GEOLOGIC FRACTURES
GEOLOGIC STRUCTURES
NORTH AMERICA
PALEOZOIC ERA
ROCKS
SEDIMENTARY ROCKS
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