43 NETectonics: New Advances in Structural Geology and Tectonics in the Appalachians

Monday, 20 March 2017
1:30 PM - 5:30 PM
Lawrence Welk Room, Mezzanine Level

REFINING BALANCED CROSS SECTION KINEMATIC SEQUENCES WITH FLEXURAL AND EROSIONAL FORWARD MODELING

Paper number: 43-13
Program: Theme Sessions
Time: 5:10 PM – 5:30 PM

Authors

Abstract

Creating forward modeled, balanced cross sections, while accounting for both flexural loading and erosional unloading have the potential to verify and refine the kinematic sequence of deformation in fold and thrust belts. Insight into the relative order of events is particularly apparent for out-of-sequence faults that have the ability to either vertically exhume deeper strata in the case of thrusts, or normal faults which create basins that may or may not be preserved in the mapped geology. Strata exhumed by thrusts (either in- or out-of-sequence) may leave a distinct provenance or detrital age signature in the foreland basin. A predicted foreland basin and foreland basin stratigraphy develops as a result of the isostatic model, allowing correlation between modeled and measured stratigraphic sections in the vicinity of the cross section. Incremental modeling in short displacement steps (~10 km) creates “pseudostratigraphy” in the foreland which predicts the location and magnitude of preserved sediment, and identifies the location and amount of material eroded in the incremental thrust event, i.e. the provenance of the sediments within the pseudostratigraphy. We present a case study for this method from the Himalayas in Western Nepal and demonstrate examples for how it may be used for cross sections in the Appalachians and other mountain belts.

Geological Society of America Abstracts with Programs. Vol. 49, No. 2

doi: 10.1130/abs/2017NE-290467

© Copyright 2017 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.