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Fred M Phillips

Biographic Data

ID1181563
NAMEFred M Phillips
GIVEN NAMESFred M
FAMILY NAMEPhillips
SIGNATUREPHILLIPS F M
AFFILIATIONSNew Mexico Institute of Mining and Technology
ORCID0000-0001-5735-8845
VERIFIEDYes
TOTAL WORKS4
TOTAL CITATIONS10
WORKS AS AUTHOR4
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1986
LATEST PUBLICATION YEAR2022
H-INDEX1
  • Chronofunctions for new Mexico, USA soils show relationships among climate, dust input, and soil development

    Open Access•Brad Sion, Bruce J Harrison et al.•ARTICLE•Quaternary International•2022

  • Terrestrial in situ cosmogenic nuclides

    Open Access•John C Gosse, John Gosse et al.•ARTICLE•Quaternary Science Reviews•2001

  • Maximum ages of the Côa valley (Portugal) engravings measured with Chlorine-36

    Open Access•Fred M Phillips, Montgomery Flinsch et al.•ARTICLE•Antiquity•1997•Cited by: 10•References: 13

    Panel faces in teh Côa valley, Portugal, were available for engraving during the Upper Palaeolithic, according to 36Cl exposure ages of 16,000 to 136,000 years

  • Paleoclimatic Inferences from an Isotopic Investigation of Groundwater in the Central San Juan Basin, New Mexico

    Open Access•Fred M Phillips, Leslie A Peeters et al.•ARTICLE•Quaternary Research•1986

    Groundwater from the Ojo Alamo and Nacimiento aquifers in the central San Juan Basin. New Mexico, has yielded 14 C ages ranging from modern to 35,000 yr B.P. The Pleistocene-age samples are characterized by a stable isotope content about 25‰ lighter in D and 3‰ lighter in 18 O than modern precipitation and groundwater. We attribute this difference to a colder mean annual temperature and perhaps increased winter precipitation. Consideration of var…

  • Maximum ages of the Côa valley (Portugal) engravings measured with Chlorine-36

    Open Access•Fred M Phillips, Montgomery Flinsch et al.•ARTICLE•Antiquity•1997•Cited by: 10•References: 13

    Panel faces in teh Côa valley, Portugal, were available for engraving during the Upper Palaeolithic, according to 36Cl exposure ages of 16,000 to 136,000 years

  • Paleoclimatic Inferences from an Isotopic Investigation of Groundwater in the Central San Juan Basin, New Mexico

    Open Access•Fred M Phillips, Leslie A Peeters et al.•ARTICLE•Quaternary Research•1986

    Groundwater from the Ojo Alamo and Nacimiento aquifers in the central San Juan Basin. New Mexico, has yielded 14 C ages ranging from modern to 35,000 yr B.P. The Pleistocene-age samples are characterized by a stable isotope content about 25‰ lighter in D and 3‰ lighter in 18 O than modern precipitation and groundwater. We attribute this difference to a colder mean annual temperature and perhaps increased winter precipitation. Consideration of var…

  • Maximum ages of the Côa valley (Portugal) engravings measured with Chlorine-36

    Open Access•Fred M Phillips, Montgomery Flinsch et al.•ARTICLE•Antiquity•1997•Cited by: 10•References: 13

    Panel faces in teh Côa valley, Portugal, were available for engraving during the Upper Palaeolithic, according to 36Cl exposure ages of 16,000 to 136,000 years

  • Terrestrial in situ cosmogenic nuclides

    Open Access•John C Gosse, John Gosse et al.•ARTICLE•Quaternary Science Reviews•2001

  • Chronofunctions for new Mexico, USA soils show relationships among climate, dust input, and soil development

    Open Access•Brad Sion, Bruce J Harrison et al.•ARTICLE•Quaternary International•2022

Geology and Paleoclimatology Research (4 works) · Geography (3 works) · Geology (3 works) · Geomorphology (3 works) · Geology (2 works) · Physical geography (2 works) · Pleistocene-Era Hominins and Archaeology (2 works) · Precipitation (2 works) · Structural basin (2 works) · Aeolian processes (1 work)

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