Tracer studies of the fluorine-rich skarn at McCullough Butte, Eureka County, Nevada.
Mark D Barton, Joaquin Ruiz, E. Ito, L. Jones
Calcite and dolomite from skarn veins (12) and altered host-rock (18) have delta 18O and delta 13C values (relative to PDB) between those of the unaltered host rock and magmatic water, indicating that it played a large part in skarn formation. Carbonates from veins lacking fluorite (5) show depletion in delta 18O only, indicating fluid dominated by meteoric water. Values for fluorite 87Sr/86Sr intermediate between host-rock and granite require at least two sources. Fluorite REE values resemble those of the host suggesting limited REE mobility.K.F.
Carnegie Institution of Washington Year Book
skarn
host rock
rare earth element
intermediate host
meteoric water
Earth and Planetary Sciences(all)
Barton, M. D., Ruiz, J., Ito, E., & Jones, L. (1982). Tracer studies of the fluorine-rich skarn at McCullough Butte, Eureka County, Nevada. In Carnegie Institution of Washington Year Book (Vol. 81, pp. 328-331)
Tracer studies of the fluorine-rich skarn at McCullough Butte, Eureka County, Nevada. / Barton, Mark D; Ruiz, Joaquin; Ito, E.; Jones, L.
Carnegie Institution of Washington Year Book. Vol. 81 1982. p. 328-331.
Barton, MD, Ruiz, J, Ito, E & Jones, L 1982, Tracer studies of the fluorine-rich skarn at McCullough Butte, Eureka County, Nevada. in Carnegie Institution of Washington Year Book. vol. 81, pp. 328-331.
Barton MD, Ruiz J, Ito E, Jones L. Tracer studies of the fluorine-rich skarn at McCullough Butte, Eureka County, Nevada. In Carnegie Institution of Washington Year Book. Vol. 81. 1982. p. 328-331
Barton, Mark D ; Ruiz, Joaquin ; Ito, E. ; Jones, L. / Tracer studies of the fluorine-rich skarn at McCullough Butte, Eureka County, Nevada. Carnegie Institution of Washington Year Book. Vol. 81 1982. pp. 328-331
@inbook{27fc189ee81a412093bdd25a6384c630,
title = "Tracer studies of the fluorine-rich skarn at McCullough Butte, Eureka County, Nevada.",
abstract = "Calcite and dolomite from skarn veins (12) and altered host-rock (18) have delta 18O and delta 13C values (relative to PDB) between those of the unaltered host rock and magmatic water, indicating that it played a large part in skarn formation. Carbonates from veins lacking fluorite (5) show depletion in delta 18O only, indicating fluid dominated by meteoric water. Values for fluorite 87Sr/86Sr intermediate between host-rock and granite require at least two sources. Fluorite REE values resemble those of the host suggesting limited REE mobility.K.F.",
author = "Barton, {Mark D} and Joaquin Ruiz and E. Ito and L. Jones",
booktitle = "Carnegie Institution of Washington Year Book",
T1 - Tracer studies of the fluorine-rich skarn at McCullough Butte, Eureka County, Nevada.
AU - Barton, Mark D
AU - Ruiz, Joaquin
AU - Ito, E.
AU - Jones, L.
N2 - Calcite and dolomite from skarn veins (12) and altered host-rock (18) have delta 18O and delta 13C values (relative to PDB) between those of the unaltered host rock and magmatic water, indicating that it played a large part in skarn formation. Carbonates from veins lacking fluorite (5) show depletion in delta 18O only, indicating fluid dominated by meteoric water. Values for fluorite 87Sr/86Sr intermediate between host-rock and granite require at least two sources. Fluorite REE values resemble those of the host suggesting limited REE mobility.K.F.
AB - Calcite and dolomite from skarn veins (12) and altered host-rock (18) have delta 18O and delta 13C values (relative to PDB) between those of the unaltered host rock and magmatic water, indicating that it played a large part in skarn formation. Carbonates from veins lacking fluorite (5) show depletion in delta 18O only, indicating fluid dominated by meteoric water. Values for fluorite 87Sr/86Sr intermediate between host-rock and granite require at least two sources. Fluorite REE values resemble those of the host suggesting limited REE mobility.K.F.
BT - Carnegie Institution of Washington Year Book