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ATTACHMENT F:MAPS AND CROSS SECTIONS OF GEOLOGIC STRUCTURE OF AREA <br /> Physical Extent <br /> The Domengine Formation isopach map (Figure F-9), developed for the original permit by <br /> examination and correlation of DOGGR well records and geophysical logs (Table F-1),is <br /> based on 22 thickness values. The thickness of the injection unit is 831 feet and is not less <br /> than 780 feet thick within the AOR. The Domengine thins toward both the Lodi Airport to <br /> the east and the East Islands Gas Fields to the northwest. <br /> The Domengine Formation structure contour map (Figure F-10) is based on 23 wells that <br /> penetrated the top of the formation. The formation dips about 2 degrees uniformly to the <br /> southwest. A structural nose 2 to 3 miles to the east of the facility occurs below and, <br /> coincidentally,is generally aligned with the railroad line that runs northwest-southeast. A <br /> second less prominent structural nose occurs 1 to 2 miles west of the facility,and is oriented <br /> to the northeast-southwest. Gas fields appear to be associated with these structural features. <br /> The structure contour map does not indicate any closed structural features in the area. <br /> Description <br /> The Domengine Formation consists of two to three sand intervals separated by siltstone or <br /> shale. It is a coarse-grained, gray to brown marine quartz sandstone with feldspar and <br /> occasional glauconite. It is exposed to the west in the Mount Diablo area. <br /> Physical Properties <br /> The hydraulic conductivity and permeability of the injection zone within the Domengine <br /> Formation has been measured several times during routine testing since the well was <br /> installed in 1994. The averages of these measurements was used to calculate the AOR and <br /> are summarized in Tables A-2 and A-3. The hydraulic conductivity of the injection zone is <br /> estimated to be 0.591 feet/day and the permeability to be 142 millidarcys. <br /> Confining Zones <br /> The upper confining zone is the Nortonville Formation. The lower confining zone is the <br /> Capay Formation. They are shown in the two cross sections (Figures F-2 and F-3). <br /> Nortonville Shale <br /> The Nortonville shale is a dark gray marine shale and siltstone that is the upper confining <br /> unit for the injection zone. In some areas, minor sandstone,coal,and glauconitic sandstone <br /> can also occur within it. In parts of the state,it produces gas. <br /> The Nortonville shale isopach map (Figure F-11) has thickness estimates from 24 local wells. <br /> The thickness of the Nortonville Shale ranges from 100 to more than 200 feet within the area <br /> contoured. This includes a thickness of 117 feet at the STIG-1 well. Overall,the unit thickens <br /> to the southeast. <br /> Capay Formation <br /> The Capay Formation is the lower confining shale unit for the injection zone. It is a marine <br /> shale to silty shale with occasional sand stringers. The Capay Formation is being considered <br /> and studied for a possible carbon-sequestration project within the sand stringers in the <br /> F-4 SAC/371322/082550021(ATTACHMENT-F.DOC) <br />