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Title: Basement-influenced deformation in the Marathon fold-thrust belt, West Texas

Journal Article · · J. Geol.; (United States)
DOI:https://doi.org/10.1086/629253· OSTI ID:6860428

The Marathon Basin of West Texas is a window into the southwestern end of the Ouachita system and formed as a response to north-to-northwest-directed late Paleozoic thrust faulting. Folds in the basin are elongate, trend northeast, and are highly non-cylindrical. Thickness and facies changes within the flysch sediments of the basin are coincident with the plunge of major anticlinoria. These features are superimposed on a pre-existing structural framework inherited from earlier deformation and modified by pre-, syn-, and post-tectonic sedimentation. Field, seismic, aeromagnetic, and deep well data indicate the presence of both northeast-trending frontal ramps and northwest-trending transverse ramps beneath the allochthonous rocks of the Marathon Basin. Evidence for reactivated northwest-trending features includes: (1) changes in plunge of first- and second-order folds; (2) large offsets in Devonian carbonate/top of basement seismic reflectors; (3) structure contours on Cretaceous rocks surrounding the basin; (4) dramatic changes in elevation of top of Ellenburger along strike; (5) variable tectonic stratigraphy and flysch thickness along strike; (6) a northwest-trending magnetic low through the middle of the basin; and (7) outcrop and well data for large-scale vertical movements along colinear northwest-trending features both north and south of the basin proper. These basement structural features (high-angle faults.) were inherited from Late Precambrian rifting and reactivated during Ouachita, Laramide, and Basin and Range events. Basement-influenced transverse structures affect the sedimentological and subsequent deformational histories of this and other fold-thrust belts around the world.

Research Organization:
Univ. of Texas, Austin (USA)
OSTI ID:
6860428
Journal Information:
J. Geol.; (United States), Vol. 96:5
Country of Publication:
United States
Language:
English