Detailseite
Projekt
Ein Abbild der tiefen Strukturen der San Andreas Fault Zone in Parkfield, Kalifornien mit Magnetotellurikmessungen
Antragsteller
Professor Dr. Oliver Ritter
Fachliche Zuordnung
Physik des Erdkörpers
Förderung
Förderung von 2004 bis 2011
Projektkennung
Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 5423681
Magnetotelluric (MT) studies have always played an important role in the investigation of the San Andreas Fault. Due to short profile lengths, they have generally focused on the geometry and nature of the upper crustal fault. Geophysical imaging of the ductile roots is essential, however, to address the dynamics of interplate transform faulting. We propose a high resolution MT survey in the vicinity of the SAFOD site near Parkfield, California following a 50 km reflection/refraction seismic profile [Hole and Ryberg, 2003]. New and existing MT data sets [Unsworth et al., 2000; Park et al., 1991] will be modeled jointly using 2D inversion procedures. Acquisition of additional spatially distributed sites will help separate off-profile features from structure at depth. Accompanying 2D anisotropic and 3D forward modeling studies will be carried out to examine more complicated conductivity structures. Acquiring seismic and magnetotelluric data along a coincident profile is an unprecedented opportunity to utilize the combined imaging power of the two methods. The project will be coordinated and carried out in close cooperation with scientists and partner institutions in the United States.
DFG-Verfahren
Infrastruktur-Schwerpunktprogramme
Beteiligte Person
Professor Dr. Michael Weber
