Tectonic History of the Western United States
GEOL 5690, Spring 2024
Meet: Wednesdays and Fridays 11:30-12:45, BESC 440E.
Instructor: Craig
Jones, ESCI 440C, cjones@colorado.edu
Text: Turcotte and Schubert, Geodynamics, 2nd or 3rd edition.
Baldridge, Geology of the American
Southwest is optional
Stüwe, Geodynamics of the Lithosphere:
An Introduction can be helpful
News:
- Class projects (written version) wil be due May 7 by 5 pm. (Earlier would be nice).
- Oral presentations (15 minutes apiece, ideally a bit less) on final class May 1.
Syllabus
(mostly updated for 2024)
Friday, 4/19: Shatsky Conjugate, Alternative models. How do we know there was a Shatsky conjugate? How can we decide where it was? How do we determine its effect on the surface? What should alternative models predict? What options are there?
- Please read and be ready to discuss: Liu, L., Gurnis, M., Seton, M., Saleeby, J., Müller, R. D., and Jackson, J. M., 2010, The role of oceanic plateau subduction in the Laramide orogeny: Nature Geoscience, v. 3, no. 4, p. 1-5, doi: 10.1038/ngeo829. Note there is a supplement that can be of some use.
- If you are curious, a recent paper with some challenges for the Shatsky story: Schwartz, J. J., Lackey, J. S., Miranda, E. A., Klepeis, K. A., Mora-Klepeis, G., Robles, F., and Bixler, J. D., 2023, Magmatic surge requires two-stage model for the Laramide orogeny: Nature Communications, v. 14, no. 1, 3841, doi: 10.1038/s41467-023-39473-7.
- Another resource. How much should we believe a specific seismic tomographic model? One thing you can do is compare a bunch of models...which would be daunting except that there are tools at IRIS that allow one to make these plots fairly easily. You might want to fist identify models relevant for your concerns (hit the "Earth Models" link, where models are listed by extent) and then, armed with the shorthand ID of the models of interest, you can make arbitrary cross sections, stacked sections, stacks of map views at different depths, etc.
Wednesday, 4/24: Paleoelevation. What approaches work for getting ancient elevations? What are the assumptions? What are the weaknesses? Focus will be on "Nevadaplano"; consider the differences in interpretations of these two papers and why they do differ:
- Lechler, A. R., Niemi, N. A., Hren, M. T., & Lohmann, K. C. (2013). Paleoelevation estimates for the northern and central proto-Basin and Range from carbonate clumped isotope thermometry. Tectonics, 32(3), 295–316.
- Snell, K. E., Koch, P. L., Druschke, P., Foreman, B. Z., & Eiler, J. M. (2014). High elevation of the “Nevadaplano” during the Late Cretaceous. Earth and Planetary Science Letters, 386(C), 52–63.
- This week's colloquium touches on related issues, so for instance Kelson, J. R., Petersen, S. V., Niemi, N. A., Passey, B. H., and Curley, A. N., 2022, Looking upstream with clumped and triple oxygen isotopes of estuarine oyster shells in the early Eocene of California, USA: Geology, v. 50, no. 7, p. 755-759, doi: 10.1130/G49634.1 uses datasets based on work of the speaker this week, like Wostbrock, J. A. G., Cano, E. J., and Sharp, Z. D., 2020, An internally consistent triple oxygen isotope calibration of standards for silicates, carbonates and air relative to VSMOW2 and SLAP2: Chemical Geology, v. 533, 119432, doi: 10.1016/j.chemgeo.2019.119432.
- Images used in class
- Paleoelevation handout
Friday, 4/26: Gravitational potential energy, Basin and Range extension and Core Complexes. What are the sources of stress necessary to drive deformation? How does lithospheric structure affect those stresses? What is a core complex, and how might they form? What is the relationship between Basin and Range extension and the evolution of magmatism?
- Forces acting on the lithosphere (handout) (might note new paleoelevation handout covering some of Wednesday's class material)
- Turcotte and Schubert, pp. 226-229 (section 6-1, 6-2); (Baldridge sec. 8.4)
- Buck, W.
R., Modes of continental lithospheric extension, J. Geophys. Res., 96,
20,161-20,178, doi: 10.1029/91JB01485,1991.
- Images used in class
Wednesday, 5/1: Term project presentations. Please send whatever PowerPoint/Keynote you intend to show prior to class so they can all be on one computer. Everybody gets 15 minutes, but aim for less so there can be some Q and A and discussion.
Homeworks:
Handouts: (subject to updating)
Final project 2021: Plateau Subduction and the Laramide Orogeny
Please send mail to cjones@colorado.edu
if you encounter any problems or have suggestions.
GEOL5690 home | C.
H. Jones | CIRES
| Dept. of Geological
Sciences | Univ. of Colorado
at Boulder
Last modified at
April 26, 2024 5:38 PM