High Plains groundwater isotopic composition in northeastern New Mexico (USA): relationship to recharge and hydrogeologic setting

Author:

Phan Victoria A.,Zeigler Kate E.,Vinson David S.ORCID

Funder

Geological Society of America

Publisher

Springer Science and Business Media LLC

Subject

Earth and Planetary Sciences (miscellaneous),Water Science and Technology

Reference68 articles.

1. Baillie MN, Hogan JF, Ekwurzel B, Wahi AK, Eastoe CJ (2007) Quantifying water sources to a semiarid riparian ecosystem, San Pedro River, Arizona. J Geophys Res 112:G03S02

2. Bartnik SR, Hampton BA, Mack GH (2019) U-Pb detrital geochronology and provenance comparisons from the nonmarine strata of the Dakota group, Lytle sandstone, and Morrison formation in northeastern New Mexico. In: Ramos FC, Zimmerer MJ, Zeigler KE, Ulmer-Scholle DS (eds) Geology of the Raton-Clayton Area. New Mexico Geological Society Guidebook, 70th Field Conference, NM Geol. Soc., Socorro, NM, pp 55–65

3. Becker MF, Bruce BW, Pope LM, Andrews WJ (2002) Ground-water quality in the central High Plains Aquifer, Colorado, Kansas, New Mexico, Oklahoma, and Texas, 1999. US Geol Surv Water Resour Invest Rep 2002-4112

4. Chen Z, Nie Z, Zhang G, Wan L, Shen J (2006) Environmental isotopic study on the recharge and residence time of groundwater in the Heihe River basin northwestern China. Hydrogeol J 14:1635–1651

5. Clark ID, Fritz P (1997) Environmental isotopes in hydrogeology. Lewis, Boca Raton, FL

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