Two independent methods are used in this study to estimate the age of the aquifer rocks and sediments. Samples from cores will be examined for fossil dinoflagellate cysts, pollen, mollusks, foraminifers, and ostracodes, and their age determined by correlation to other distant sites that have been dated isotopically. Age also will be estimated by the isotopic composition of strontium in unaltered shells. The ratio of the stable isotopes of strontium in the oceans has varied over geologic time such that, in the last 40 million years, there has been a unique relation between age and isotopic composition. Marine invertebrates incorporate the strontium isotopic ratio of the ocean into their shells as they grow, thereby preserving evidence of their age.
Geophysical logs provide a continuous downhole record of the properties of the rocks that form the aquifer. They are especially valuable in providing physical and chemical properties of the corehole where particular intervals of core recovery are poor. Also, they allow extension of hydrologic test data from discrete samples to the rest of the core. Geophysical logs, combined with aquifer water properties and flow measurements, will be used to relate large-scale ground-water circulation to the distribution of hydrologic properties of the aquifer. For example, flowmeter logs can confirm that the most permeable intervals, as inferred from core measurements, coincide with the intervals that conduct the most flow in the vicinity of test wells. Geophysical logs also will indicate which confining units act to separate the aquifer system into discrete aquifers having different water quality and hydraulic head.
Cunningham, Kevin J.
Weedman, S. D.; Simmons, K. R.; Scott, T. M.; Brewster-Wingard, G. L.; Ishman, S. E.; Carlin, N. M.
Paillet, F. L; Edwards, L. E.; Simmons. K. R.; Scott, T. M.; Wardlaw, B. R.; Reese, R. S.; Blair, J. L.
Paillet, F. L.; Means, G. H.; Scott, T. M.
Cores have been examined for mineralogy, texture, sedimentary structures, and fossils to determine rock type, age, mineralization, and porosity and to differentiate the zones that form aquifers from the confining units that separate them.
Stratigraphic units have been identified and correlated between coreholes and their properties estimated where core data are absent.
Aquifer tests were being performed on selected coreholes to measure permeability of the aquifer system.
U.S. Department of the Interior, U.S. Geological Survey, Center for
Coastal Geology
Comments and suggestions? Contact: Heather
Henkel - Webmaster
Generated by mp version 2.8.18 on Wed Feb 21 09:13:19 2007