My background is economic geology, specifically mineral exploration/mining work in the precious metals industry. That's where I started out and I later went back for a Master's when the price of gold took a dive in the late 90s (when many geos were laid off).
The paper you linked discusses regional structural trends/shear zones in Colorado that are probably related to arc accretion in the Proterozoic.
One of my projects is an intrusion located in southern Wyoming about 15 km south of the Archean-Proterzoic suture. In the past, I was unaware of the presence of those two thrusts located up north as they are not present on any of the maps I have.
The second project is located in the vicinity of the Black Canyon. I've been mapping pediment surfaces (and structure when I can find it) out there in an attempt to reconstruct the geomorphic and erosional history of the area, basically paleolandscape reconstruction. The pediment surfaces, which are comprised of unconsolidated gravels up to boulder size, occur at different elevations similar to river terraces, and probably represent different pulses of stream formation/deposition at the end of at least two glacial periods.
The pediment project is only one portion of a larger project involving studying rocks deposited in the Western Interior Seaway. We recently recovered 500+ feet of core drilled into Cretaceous rocks (located near the Black Canyon) that were deposited in the seaway and I am logging that right now.
The paper you linked specifically discusses structure in the Black Canyon area. Just based on a quick perusal of the paper, the authors appear to have re-interpreted some of the major structures, so it will be interesting to see why.
This message has been edited by roxrkool, 03-17-2006 09:40 AM