Robert B. Herrmann - US grants

Affiliations:

Saint Louis University, St. Louis, MO, United States

Area:

Geophysics

Website:

http://www.eas.slu.edu/People/RBHerrmann/

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High-probability grants

According to our matching algorithm, Robert B. Herrmann is the likely recipient of the following grants.

Years	Recipients	Code	Title / Keywords	Matching score
1977 — 1979	Herrmann, Robert	N/AActivity Code Description: No activity code was retrieved: click on the grant title for more information	Earthquake Ground Motion Modeling For the Central U.S. @ Saint Louis University	0.915
1979 — 1982	Herrmann, Robert	N/AActivity Code Description: No activity code was retrieved: click on the grant title for more information	Earthquake Ground Motion Scaling For the Central United States @ Saint Louis University	0.915
1982 — 1984	Herrmann, Robert Nuttli, Otto (co-PI) [⬀]	N/AActivity Code Description: No activity code was retrieved: click on the grant title for more information	Strong Ground Motion Scaling For the Central United States (Earthquake Engineering) @ Saint Louis University	0.915
1984 — 1987	Herrmann, Robert Nuttli, Otto (co-PI) [⬀]	N/AActivity Code Description: No activity code was retrieved: click on the grant title for more information	Strong Ground Motion Scaling With Application to the Centralunited States @ Saint Louis University	0.915
2002 — 2005	Zhu, Lupei (co-PI) [⬀] Herrmann, Robert Kusky, Timothy (co-PI) [⬀] Mitchell, Brian (co-PI) [⬀] Koper, Keith [⬀]	N/AActivity Code Description: No activity code was retrieved: click on the grant title for more information	Upgrade of Computer Facilities For the Seismology Research Group At Saint Louis University @ Saint Louis University 0214259 Koper This grant provides partial support for an upgrade of the high-performance computing environment for geophysicists at Saint Louis University. Research carried out by the group is wide-ranging and includes Earth structure studies, seismic source studies, seismic hazard analysis, application of space-based remote sensing data to tectonic problems, and development of freely distributed software. The grant will especially benefit three recently hired assistant professors (Koper, Kusky and Zhu) in establishing research programs. *** Show summary Hide summary	0.915
2011 — 2017	Herrmann, Robert	N/AActivity Code Description: No activity code was retrieved: click on the grant title for more information	Collaborative Research: Northern Embayment Lithosphere Experiment (Nele) @ Saint Louis University Passage of the EarthScope Transportable Array across the Mississippi Embayment is providing an opportunity to investigate lithospheric structure associated with active deformation and an ancient, intracratonic rift. The Mississippi Embayment is a first-order geological structure of the North American continent with a long and complex geological history affected by at least two periods of continental breakup. The reason for geologically recent basin subsidence is enigmatic since subsidence began about 100 million years ago and is not linked to a major tectonic episode. In addition, the active New Madrid seismic zone (NMSZ) is located in the upper crust within the northern Mississippi Embayment. Lithospheric seismic velocity heterogeneity and anisotropy are likely indicators of the dynamic processes associated with basin subsidence and earthquake genesis in the region. The seismic experiment incorporates stations of EarthScope's Transportable Array and a higher density FlexArray deployment to provide an overall framework of lithospheric velocity and anisotropy structure to depths exceeding the upper mantle transition zone. Detailed variations in deep structure perpendicular and parallel to the embayment axis are imaged using three dense lines of FlexArray stations that extend within and outside of the Mississippi Embayment. Major issues that are addressed include 1) the primary differences in lithospheric structure between the embayment and the surrounding region, 2) the nature of early Cambrian rifting and relationship to pre-existing structure, 3) the dynamic processes responsible for basin subsidence, and 4) the relationship of the NMSZ to large scale lithospheric structure. This is accomplished through joint interpretation of seismic velocity tomography, potential fields, transfer/receiver functions, and depth-dependent anisotropy images generated using traditional and new geophysical techniques. Show summary Hide summary	0.915