Oligocene stratigraphy, tectonics, and paleogeography southwest of the San Andreas Fault, Santa Cruz Mountains and Gabilan Range, California coast ranges

The Loma Prieta, California, earthquake of October 17, 1989: Aftershocks and postseismic effects

“…Third, we used bathymetric contour maps for approximating the ocean floor topography. Finally, we used surface geologic information (Clark and Rietman, 1973) for setting the very near surface resistivity information. We show one a priori model for profile A in figure 5.…”

Geohydrology and mathematical simulation of the Pajaro Valley aquifer system, Santa Cruz and Monterey Counties, California

“…The regional geology of the Pajaro Valley area has been mapped and described by Greene (1970Greene ( , 1977, Muir (1972), Clark and Rietman (1973), Dupre (1974Dupre ( , 1975, and Dupre" and Tinsley (1980). The central part of the Pajaro Valley is basically an erosional and structural depression surrounded by areas of uplift and folding.…”

Fault zone structure determined through the analysis of earthquake arrival times

“…Cruz mountains (SCM) by Clark and Rietman (1973). In the study area, northeast of the Sargent fault (SF), the Franciscan sequence contains limestone lenses and horneblende-glaucophane-bearing metamorphic rocks.…”

“…This narrowed LVZ is bounded on its southwest side by the Zayante-Vergeles tectonic line and by the SAF to the northeast. Other evidence for this fault bounded LVZ comes from gravity modeling (Clark and Rietman, 1973), deep wells northeast and southwest of the Zayante-Vergeles line (see Clark and Rietman, 1973, for a discussion) and by Mooney and Colburn (1985) in the interpretation of a refraction seismic line across the SCM from Watsonville to Gilroy (i.e., approximately the vertical cross-section at y = -20, in our model). The interpretation is that the Salinian basement has downdropped between the two faults by approximately 2 to 3 km (Clark and Rietman, 1973) or by about 1.5 km (Mooney and Colburn, 1985).…”