| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4733207 | Journal of Structural Geology | 2013 | 12 Pages |
Abstract
⺠We present a model for the structural architecture for the Marathon fold and thrust belt. ⺠New subsurface data is incorporated with surface exposures. ⺠A bed-parallel detachment in the lower Tesnus Formation separates structural lithic units. ⺠A perched décollement in the foreland was later reactivated as a roof thrust to duplex systems. ⺠The structural model we present may be applicable to much of the Ouachita orogenic system.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
James B. Chapman, Reid S. McCarty,