January 6, 2020
By Philip S. Prince, Virginia Tech Active Tectonics and Geomorphology Lab
Understanding thrust fault geometries beneath active compressional mountain ranges is vital to evaluating seismic hazard as well as understanding the overall evolution of the mountain belt. In particular, trying to identify ramp step-ups between lower angle fault segments is important to understanding fault rupture potential. Gaining information about faults kilometers beneath the land surface is difficult, and geoscientists have to use creative approaches to gather this important information. Because fault segments of interest may be 10-15 km deep beneath extreme mountain topography (see scale on figure below), studying them can be quite a challenge.
A particularly interesting method of attempting to understanding deep fault geometry is using patterns of surface landscape evolution to identify the moving zone of uplift above a deep fault ramp.
A useful analogy for this concept is to visualize sliding a spatula underneath a cooking egg. Even though you can’t see the edge of the spatula, you can tell where it is because the thin, flat egg steps up onto the spatula from the base of the pan. The edge of the spatula is like a ramp, and as the spatula is pushed further under the egg, the bulge in the overlying egg moves along with it. In the case of a real mountain range, the dimensions of the edge of the spatula (the ramp) would be at the scale of kilometers, but the idea is essentially the same.
The basic concept of uplift above a deeper ramp can be visualized in an analog model using strong, cohesive layers separated by very weak layers of microbeads. This setup creates ramp-flat-ramp faults, and surface uplift can be seen in the growing tectonic wedge as it warps over a ramp. Uplift occurs at the structural front, or leading edge of the deformed area, as well as above the deeper ramp that is underneath the interior of the deformed area.
The model ramp can be compared to the spatula edge (see below), and it produces a comparable effect in the overlying wedge, which is of course proportionally thicker than an egg. These models aren’t really set up to have precise lithotectonic analogies in a real system; they are simply intended to show the surface effects of ramp-flat fault geometries. The overarching pattern to look for, as mentioned above, is minor uplift at the structural front, and a zone of uplift above the much thicker part of the wedge well away from the structural front. Between these two areas, there is a zone where little or no surface uplift occurs despite ongoing movement in the model.
In a real mountain belt, this uplift above a deep ramp would force accelerated river incision, which could be identified by large-scale studies of channel steepness and topographic relief or the identification of an older landscape into which rivers have recently incised (check out this paper). The models shown here greatly exaggerate the scale of the bulge and contain many other simplifications and assumptions, but the general spatula-under-egg concept is the same.
The amount of uplift depends on the height of the ramp and the structures within the overlying wedge, but in the models linked in the video below, you can see it happen (it is admittedly subtle in the third model).
This pattern is fairly easily reproduced in a model with appropriate materials; check out 00:38 in this video. While the papers linked here address mid-crustal ramps beneath orogenic interiors, I presume this concept might be observed in thinner, external sedimentary fold-thrust belts. The third model in the video might have more analogy to such settings. The second model in the video (see gif below) was constructed for the Bane Dome post here; I think the dome would have generated focused surface uplift during its formation, but no one was around in the Permian to take a look.
I think the concept of using landscape patterns to look at fault geometries kilometers below rugged mountains is a really cool practical application of geomorphology concepts. It also demonstrates the integration of geomorphology with other branches of solid earth geoscience. It requires understanding of “background” stream morphologies so that patterns of accelerated incision can be identified, and it also makes extensive use of processing digital topography to apply techniques to large and very rugged areas.
Links to papers:
This post was originally published on The Geo Models blog.