Late Paleozoic Evolution of the Anadarko Basin: Implications for Laurentian Tectonics and the Assembly of Pangea

Journal Article · Fri Oct 21 00:00:00 EDT 2022 · Tectonics

DOI:https://doi.org/10.1029/2021TC007197· OSTI ID:1894372

Hobbs, Noah. F. ^[1]; van Wijk, Jolante W. ^[2]; Leary, Ryan ^[1]; Axen, Gary J. ^[1]

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1. Department of Earth and Environmental Science New Mexico Institute of Mining and Technology Socorro NM USA
2. Department of Earth and Environmental Science New Mexico Institute of Mining and Technology Socorro NM USA, Los Alamos National Laboratory, Computational Earth Science Los Alamos NM USA

Abstract

Interplay between marginal and intraplate late Paleozoic tectonics in southeastern Laurentia is a subject of debate. In southern Laurentia, intraplate deformation has been attributed to combinations of compressive forces from orogenic belts in the west, southwest, and southeast. While left‐lateral transpression is generally an accepted mechanism for formation of uplifts in the Southern Oklahoma Aulacogen (SOA), to date no studies have explained the driving mechanisms of these kinematics. Here, we analyze the Southern Oklahoma Transpressional System (SOTS), a ∼500 km long ∼50 km wide fault zone that extends from the southeastern Laurentian margin into the plate interior along Cambrian lithospheric weaknesses inherited from the SOA. We use a compilation of published studies to present detailed, time‐integrated sedimentary thickness maps of SOTS‐related basins. We combine these maps with a new interpretation of three 2D seismic reflection lines to constrain timing and kinematics of all major late Paleozoic SOTS fault zones. We show that the SOTS kinematics evolved from contraction to left‐lateral strike‐slip during Mississippian‐Pennsylvanian time. Tectonic activity and fault kinematics in the SOTS are explained by a model in which a remnant ocean basin closed diachronously from northeast to southwest along the Southern Appalachian and Ouachita‐Marathon orogens. Left‐lateral transpression during diachronous closure of the Rheic oceanic basin along the Ouachita‐Marathon margin is related to rotation of the stress field due to changes in slab‐pull and eastward drift of Laurentia toward Gondwana. We speculate that the SOTS acted in part as a STEP (subduction‐transfer edge propagator) fault that followed the pre‐existing SOA.

• Sponsoring Organization: USDOE
• Grant/Contract Number: NONE; FE0031684
• OSTI ID: 1894372
• Journal Information: Tectonics, Journal Name: Tectonics Journal Issue: 10 Vol. 41; ISSN 0278-7407
• Publisher: American Geophysical Union (AGU)
• Country of Publication: United States
• Language: English