NEW MEXICO GEOLOGICAL SOCIETY · SPRING MEETING
Spring Meeting Abstracts
Explore research presented at the NMGS Annual Spring Meeting. Browse abstracts from 1983 onward, choose a meeting year, or open an abstract to read the full text.
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2000
Hydrogeology and water resources at Eldorado and the Greater San Marcos watershed, Santa Fe, New Mexico
J. P. Frost New Mexico Office of the State Engineer “Eldorado” describes residential subdivisions created over the last thirty years by AMREP, also the developer of Rio Rancho. This city of gold covers about 40
Melt inclusion hosted excess argon (40ArE) in the quartz crystals of the Bishop and Bandelier magma systems
Jeffrey A. Winick1, Nelia W. Dunbar2 and William C. McIntosh2 1Dept. of Earth and Environmental Science, New Mexico Institute of Mining and Technology, Socorro, NM, New Mexico, 87801 2New Mexico Bureau of Mines and Mineral
The Esinaso Formation revealed in aeromagnetic data: south of Santa Fe, New Mexico: Preliminary interpretations
V. J. S. Grauch1, Alvis L. Lisenbee2 and Mark R. Hudson3 1U. S. Geological Survey, MS 964, Federal Center, Denver, CO, 80225, tien@usgs.gov 2South Dakota School of Mines, Rapid City, SD, 57701 3U. S. Geological
Quartz xenocrysts in a high-silica rhyolite melt: The El Cajete pumice, Jemez Mountains, New Mexico
M. G. Snow1 and J. N. Gardner1 1Los Alamos National Laboratory, Los Alamos, NM, 87545, snow@lanl.gov Quartz xenocrysts with granular, green halos are common in the rhyolitic EI Cajete pumice, Jemez Mountains, North-Central New Mexico.
The cementation and hydrogeology of two fossil geothermal systems hosted within the Camp Rice Formation at Box Canyon and San Diego Mountain, Dona Ana County, New Mexico
Drue E. Roberts Department of Geological Sciences/MSC 3AB, New Mexico State University, Las Cruces, NM, 88003 Fossil geothermal systems at Box Canyon and San Diego Mountain, in southern New Mexico, are hosted within the Plio-Pleistocene
Geochemical investigations at Carlsbad Caverns National Park: Implications for the origin of cave corrosion residue
Kathleen E. Dotson1, Rachel T. Schelble1, Michael N. Spilde1 and Laura J. Crossey1 1Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM, 87131 Lechuguilla and Spider caves provide the setting for a
Earthquake ground shaking hazard maps for the Albuquerque-Belen-Santa Fe, New Mexico corridor
I. Wong1, S. Olig1, M. Dober1, D. Wright1, P. Thomas1, W. Silva2, N. Gregor2 and S. Li2 1Seismic Hazards Group, URS Greiner Woodward Clyde, 500 12th Street, Oakland, CA, 95707 2Pacific Engineering & Analysis, El
Petroleum systems in late Paleozoic elevator basins, southern Ancestral Rocky Mountains
Ronald F. Broadhead New Mexico Bureau of Mines and Mineral Resources, a Division of New Mexico Tech, Socorro, NM, 87801 The Tucumcari, Estancia, Carrizozo, and Vaughn Basins are located in northeast and central New Mexico.
Regional analysis of the depositional environments of the lower Permian Yeso and Glorieta formations (abs)
Philip, A. Dinterman1 and Greg H. Mack1 1Dept of Geological Sciences, New Mexico State University, Las Cruces, NM, 88003 The Lower Permian (Leonardian) Veso Formation in New Mexico consists of up to 300 m of
Type sections of the Upper Pennsylvanian Bruton and Bursum Formations, Socorro County, New Mexico
Spencer G. Lucas1, Barry S. Kues2, G. L. Wilde3 and K. Krainer4 1New Mexico Museum of Natural History, 1801 Mountain Rd NW, Albuquerque, NM, New Mexico, 87104 2Department of Earth and Planetary Sciences, University of
Recommendations for revision of Pennsylvanian lithostratigraphic nomenclature in New Mexico
Barry S. Kues Dept. of Earth & Planetary Sciences, University of New Mexico, Albuquerque, NM, 87131 Pennsylvanian lithostratigraphic nomenclature in NM has developed in piecemeal fashion over the past century, and in some cases is
A soil-geomorphologic investigation of the upper tributaries of the Rio Cebolla drainage basin, Jemez Mountains, New Mexico
Tim Gere Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM, 87131, timg@unm.edu The Rio Cebolla drainage basin is a relatively large basin (area=120 km2) located in the western part of the Jemez Mountains
A Late Quaternary climate record from Alpine catchments in the southern Sangre de Cristo Mountains of northern New Mexico
Jake Armour1 and Peter J. Fawcett1 1E&PS, Univ. of New Mexico, Albuquerque, NM, 87131, jarmour@unm.edu The southern Sangre de Cristo Mountains of northern New Mexico contain evidence of Quaternary glaciation, including a distinctive set of