The Cenozoic history of the western US

Goals of the project:
The underplating and subsequent sinking or removal of the Farallon slab must have been the crucial event that has influenced tectonics in the Western US since the early Tertiary.
Yet there is no agreement on the fate of the subducting Farallon beneath North America and various models exist (e.g. Coney and Reynolds, 1977; Bird, 1988; Severinghaus and Atwater, 1990; Humphreys, 1995; Van der Lee and Nolet, 1997).
Models are based on limited datasets, and it is not clear which model, if any, would satisfy the totality of what is known. In addition, seismological data sets have greatly increased recently in California/Nevada, and very soon USArray will provide a quantum leap in station coverage for the rest of our region of interest, the western part of North America.

It is important to integrate data sets and to develop models that satisfy all available data - seismological as well as geological.
In more detail, we plan to:

* Modify existing data processing software to allow different types of data and other constraints to be input into one, general purpose (linear) inversion strategy. Data include seismic and non-seismic observations.

* Develop or modify flexible (non-uniform) parameterization schemes for the joint modeling of these data sets. Model parameters include seismic velocities, anisotropy, attenuation, and density which are interpretable in terms of constraints on composition, temperature and crystal or crack orientation.

* Test-drive the joint inversion approach on currently available data, in anticipation of EarthScope, and provide a starting model for future efforts that will rely heavily on the data produced by the EarthScope observatory,

* Test current hypotheses on Rocky Mountain contraction, western US uplift, the post-Laramide igmembritic flareup, and the present-day magmatic and tectonic activity against the starting model,

* Discover at an early stage where the station coverage of USArray leaves crucial gaps in information needed to understand the tectonic and magmatic history, to enable us to design effective deployments of the Flexible Array component.



Collaborators:

Gene Humphreys, Doug Toomey (U. Oregon)
Suzan van der Lee (Northwestern)
Alan Levander (Rice)

Postdocs:
Raffaella Montelli

Graduate students:
Karin Sigloch
Paul McGee

Funding:
NSF EarthScope Program


Return to Guust Nolet's home page