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2.0 Overview of Region 2.1 Introduction: The Rio Grande Rift Basin is a prominent geologic feature that stretches from South Central Colorado into Mexico (See Figure 2). The formation of the Rift Basin began approximately 30 MYA and has continued until the present (Morgan et al., 1986). The basin of interest for this enhanced geothermal system (EGS) feasibility study is the Albuquerque Basin. This section of the report will focus on the geology, stratigraphy, structures, and geothermal resources within the basin that are relevant to the study area that is presented on figure 3. The target formations are the Precambrian basement rocks (See Figure 4). Relevant citations are provided for the other non-target formations. 2.2 Geology and Stratigraphy: The formations within the Albuquerque Basin can be divided into Precambrian crystalline basement rocks, pre-rifting Paleozoic and Mesozoic Sedimentary rocks, and rifting Cenozoic basin fill and volcanics (See Figures 5 and 6). [Citation Note: Relevant formations to study area are referenced to Russel and Snelson (1994). Formation descriptions are referenced to the USGS Mineral Resources On-line Spatial Data for New Mexico.] The geometry of the individual formations is strongly tied to the location within the basin. The basin filling Cenozoic sediments reach thicknesses on the order of 23,000 feet near the center of the basin. This basin fill serves as a municipal water supply source for many of the cities located throughout the basin (Jiracek et al 1983). A detailed description of the Tertiary rocks is presented by Kelley (1977). In his work, Kelly divides the basin deposits into two types. The first type is the subsiding trough deposits that are not related to the Late Pleistoncene and Holocene deposits. The second type is those that are directly related. The formation that makes up a great part of the basin fill and is directly related rifting processes is the Sante Fe Group (Kelley 1977). The older Paleozoic and Mesozoic sedimentary rocks have been the target of numerous exploratory oil and gas wells but as of yet remains an undeveloped resource due to economic restrictions (Johnson et al. 2001). Detailed analysis of the Mesozoic; Jurassic, Triassic, and Cretaceous systems are presented by Mankin (1958) in NM OFR 49. Detailed analysis of the Mississippian, Pennsylvanian, and Permian aged rocks are presented by Siemers (1973) in NM OFR 54. These reports should provide relevant detailed information for the Albuquerque Basin because these formations were deposited across the region and are present unless they were eroded or cut out by faulting (Molenaar 1988). Penn State University | 2.0 Overview of Region 3PDF Image | GREAT NECK WATER POLLUTION CONTROL DISTRICT NASSAU COUNTY, NEW YORK MICROTURBINE INSTALLATION FEASIBILITY STUDY
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