Geologic studies of Union County, New Mexico

Baldwin, Brewster; Muehlberger, William R.

doi:10.58799/b-63

Cited by 6 publications

(4 citation statements)

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“…To create a realistic representation of the Basin's subsurface hydrogeologic architecture, we based our model's hydrostratigraphy off Geldon (1989) and developed structure maps of the bottom of the shale-rich hydraulic barrier and top of the Precambrian basement (Figure S1 in Supporting Information S1). The structure maps were constructed using well lithology logs (COGCC, 2020;NMOCD, 2020), geologic maps (Baldwin & Muehlberger, 1959;Clark & Read, 1972;Fridrich et al, 2012;Garrabrant, 1993;Johnson, 1969Johnson, , 1974Johnson, , 1975Lindsey, 1995aLindsey, , 1995bLindsey, , 1996Pillmore, 2003;Vine, 1974;Wallace & Lindsey, 1996;Wanek et al, 1958) and Precambrian basement data (Hemborg, 1996). The stratigraphic data was interpolated using a natural neighbor algorithm to generate surfaces that encompasses the entire model domain.…”

Section: Structure Mapsmentioning

confidence: 99%

Pore Pressure Diffusion and Onset of Induced Seismicity

Stokes

Brown

et al. 2023

JGR Solid Earth

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Cameron Chambers. I particularly thank you for the effort you all put in to editing my work. A special thank you to Shemin Ge for the copious amounts of time and effort you have dedicated to both my research and development as a hydrogeologist. You have served as a mentor, teaching me technical skills while also serving as an example of how to be a professional, these skills will serve me for the rest of my career. Thank you to my fellow graduate students, particularly Stephen Sheehan, Cameron Chambers and Claudia Corona, for your technical and emotional support throughout my graduate schooling. To my family, thank you for the immeasurable effort you put into raising me and providing me with the platform to succeed, without your efforts I am certain I would not be where I am today.

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Section: Structure Mapsmentioning

confidence: 99%

Pore Pressure Diffusion and Onset of Induced Seismicity

Stokes

Brown

et al. 2023

JGR Solid Earth

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“…Structure contours on the base of the Dakota Formation across Union County were digitized from Baldwin and Muehlberger (1959;figure 14). Contours from Rawling (2013) were used within the area of that study.…”

Section: Identification Of Formation Of Completionmentioning

confidence: 99%

“…Structure contours of the "buried bedrock surface" of Baldwin and Muehlberger (1959;figure 12) were digitized. This surface represents the base of the Ogallala Formation, Tertiary and Quaternary volcanic rocks, and post-Ogallala age alluvial and aeolian deposits, the latter being generally unconsolidated.…”

Section: Identification Of Formation Of Completionmentioning

confidence: 99%

“…A previous study (Rawling 2013 and2014) focused on the Seneca, Clayton, and Sedan 15-minute quadrangles in the east-central portion of the county, an area of about 650 square miles. It included revisions to the geologic map of Baldwin and Muehlberger (1959), a groundwater surface map, subsurface structure contour, isopach, and saturated thickness maps for the Ogallala and Dakota Formations, and analysis and interpretation of new and historical water chemistry data. These data facilitated characterization of the aquifer system and allowed inferences to be drawn regarding groundwater flowpaths and residence time, and locations and timing of groundwater recharge.…”

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confidence: 99%

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Groundwater surface map of Union County and the Clayton Underground Water Basin, northeast New Mexico

Rawling¹

2015

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Studies in the Quercus Undulata Complex. V. The Type of Quercus Undulata

Tucker

1971

American J of Botany

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The original material of Quercus undulata Torr. was collected by Edwin James on Major Long's expedition to the Rockies in 1820. The type locality was stated by Torrey as “sources of the Canadian and the Rocky Mountains.” Evidence is here adduced that the type locality is on Ute Creek, a tributary of the Canadian River, in northeastern New Mexico. The site was found to harbor Q, gambelii, Q. grisea, and numerous intermediate hybrid forms. Certain of the latter match the type of Q. undulata quite closely. The type sheet includes three elements—a branchlet regarded as the type, a twig of Q. grisea, and an isolated acorn of Q. havardii. Torrey's new species was illustrated by a figure which does not closely resemble the type, but which is more similar to Q. havardii. The acorn of Q. havardii on the type sheet must have been collected in the Texas Panhandle or western Oklahoma, where Long's party would have encountered this species. In my opinion, Torrey's figure could have been drawn from a specimen collected there, which, except for the isolated acorn, has since been lost.

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Geologic studies of Union County, New Mexico

Cited by 6 publications

References 0 publications

Pore Pressure Diffusion and Onset of Induced Seismicity

Pore Pressure Diffusion and Onset of Induced Seismicity

Groundwater surface map of Union County and the Clayton Underground Water Basin, northeast New Mexico

Studies in the Quercus Undulata Complex. V. The Type of Quercus Undulata

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