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Papers by Shari Kelley
New Mexico Geological Society, 2013 Annual Spring Meeting, Proceedings Volume, Theme: "Hydrology and History of the Rio Grande"
New Mexico Geological Society Annual Spring Meeting
New Mexico Geological Society Annual Spring Meeting
Guidebook 67 - Geology of the Belen Area
New Mexico Geological Society, 2004 Annual Spring Meeting, Proceedings Volume
New Mexico Geological Society Annual Spring Meeting
Proceedings Volume: "Karst in New Mexico in recognition of 2022 being the International Year of Caves and Karst", New Mexico Geological Society, 2022 Annual Spring Meeting
New Mexico Geological Society Annual Spring Meeting
Geology of the Sacramento Mountains Region, 2014
Geology of the Mount Taylor area
This is an updated and simplified version of the New Mexico heat flow data already on the NGDS th... more This is an updated and simplified version of the New Mexico heat flow data already on the NGDS that was used for Play Fairway analysis.
This submission includes three files from two sources. One file is derived from USGS data and inc... more This submission includes three files from two sources. One file is derived from USGS data and includes a series of manipulations to evaluate only shallow wells with high estimated geothermal gradients. Two other files are springs and wells with discharge temperatures above 30°C from the NMBGMR Aquifer Mapping database
The boundary between Middle and Upper Pennsylvanian strata in central New Mexico is generally con... more The boundary between Middle and Upper Pennsylvanian strata in central New Mexico is generally considered to coincide with the contact between the Gray Mesa and the overlying Atrasado formations. This perception was advanced in the Manzano Mountains by D.A. Myers, who reported the early Missourian fusulinid Eowaeringella near the top of the Gray Mesa Formation from a single locality in Gotera Canyon at the northern end of the range. The Gotera Canyon locality was re-examined and the Eowaeringella horizon recovered, together with additional strata 20 to 25 meters higher in the section that contain early forms of Triticites, including T. cf. pygmaeus, T. wellsi, and T. cf. planus. Thus, at Gotera Canyon, the Eowaeringella Zone is present 50 meters above the top of the Gray Mesa Formation, near the base of the Tinajas Member of the Atrasado Formation. The overlying Triticites-bearing strata appear to be common in the lower part of the Tinajas Member, from as far south as the Gotera Cany...
Geological Society of America Abstracts with Programs, 2019
For the New Mexico Play fairway Analysis project, gamma ray geophysical well logs from oil wells ... more For the New Mexico Play fairway Analysis project, gamma ray geophysical well logs from oil wells penetrating the Proterozoic basement in southwestern New Mexico were digitized. Only the portion of the log in the basement was digitized. The gamma ray logs are converted to heat production using the equation (Bucker and Rybach, 1996) : A[µW/m3] = 0.0158 (Gamma Ray [API] – 0.8).
This file contains a compilation of BHT data from oil wells in southwestern New Mexico. Surface t... more This file contains a compilation of BHT data from oil wells in southwestern New Mexico. Surface temperature is calculated using the collar elevation. An estimate of geothermal gradient is calculated using the estimated surface temperature and the uncorrected BHT data.
Compilation of boron, lithium, bromine, and silica data from wells and springs throughout New Mex... more Compilation of boron, lithium, bromine, and silica data from wells and springs throughout New Mexico from a wide variety of sources. The chalcedony geothermometry calculation is included in this file.
New Mexico Geological Society, 2013 Annual Spring Meeting, Proceedings Volume, Theme: "Hydrology and History of the Rio Grande"
New Mexico Geological Society Annual Spring Meeting
New Mexico Geological Society Annual Spring Meeting
Guidebook 67 - Geology of the Belen Area
New Mexico Geological Society, 2004 Annual Spring Meeting, Proceedings Volume
New Mexico Geological Society Annual Spring Meeting
Proceedings Volume: "Karst in New Mexico in recognition of 2022 being the International Year of Caves and Karst", New Mexico Geological Society, 2022 Annual Spring Meeting
New Mexico Geological Society Annual Spring Meeting
Geology of the Sacramento Mountains Region, 2014
Geology of the Mount Taylor area
This is an updated and simplified version of the New Mexico heat flow data already on the NGDS th... more This is an updated and simplified version of the New Mexico heat flow data already on the NGDS that was used for Play Fairway analysis.
This submission includes three files from two sources. One file is derived from USGS data and inc... more This submission includes three files from two sources. One file is derived from USGS data and includes a series of manipulations to evaluate only shallow wells with high estimated geothermal gradients. Two other files are springs and wells with discharge temperatures above 30°C from the NMBGMR Aquifer Mapping database
The boundary between Middle and Upper Pennsylvanian strata in central New Mexico is generally con... more The boundary between Middle and Upper Pennsylvanian strata in central New Mexico is generally considered to coincide with the contact between the Gray Mesa and the overlying Atrasado formations. This perception was advanced in the Manzano Mountains by D.A. Myers, who reported the early Missourian fusulinid Eowaeringella near the top of the Gray Mesa Formation from a single locality in Gotera Canyon at the northern end of the range. The Gotera Canyon locality was re-examined and the Eowaeringella horizon recovered, together with additional strata 20 to 25 meters higher in the section that contain early forms of Triticites, including T. cf. pygmaeus, T. wellsi, and T. cf. planus. Thus, at Gotera Canyon, the Eowaeringella Zone is present 50 meters above the top of the Gray Mesa Formation, near the base of the Tinajas Member of the Atrasado Formation. The overlying Triticites-bearing strata appear to be common in the lower part of the Tinajas Member, from as far south as the Gotera Cany...
Geological Society of America Abstracts with Programs, 2019
For the New Mexico Play fairway Analysis project, gamma ray geophysical well logs from oil wells ... more For the New Mexico Play fairway Analysis project, gamma ray geophysical well logs from oil wells penetrating the Proterozoic basement in southwestern New Mexico were digitized. Only the portion of the log in the basement was digitized. The gamma ray logs are converted to heat production using the equation (Bucker and Rybach, 1996) : A[µW/m3] = 0.0158 (Gamma Ray [API] – 0.8).
This file contains a compilation of BHT data from oil wells in southwestern New Mexico. Surface t... more This file contains a compilation of BHT data from oil wells in southwestern New Mexico. Surface temperature is calculated using the collar elevation. An estimate of geothermal gradient is calculated using the estimated surface temperature and the uncorrected BHT data.
Compilation of boron, lithium, bromine, and silica data from wells and springs throughout New Mex... more Compilation of boron, lithium, bromine, and silica data from wells and springs throughout New Mexico from a wide variety of sources. The chalcedony geothermometry calculation is included in this file.