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Quaternary Geology of the Monterey Bay Region, California
The central Monterey Bay region (Figure 1) has been a stable to subsiding depocenter and the locus of fluvial, alluvialfan, and eollan activity throughout the Quaternary. It and adjacent tectonically uplifting areas provide an opportunity to study the development of marine and non-marine depositional systems as a function of fluctuating sea level and tectonic setting.
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