Published October 1989 | Version v1
Journal article Metadata-only

Oxygen isotope composition of anhyrite in early stage veins, mineral park porphyry system, wallapai mining district, Arizona, U. S. A

Creators

  • 1. Chengdu Coll. of Geology, SC (China)
  • 2. Arizona Univ., Tucson, AZ (USA). Dept. of Geosciences

Description

Based on the isotope fractionation theory, the origin and the evolution of the mineralization liquor in Am and AC veins by δ180 values (pure water) of the mineralization liquor calculated by the heterogeneous temperatures of the fluid inclutions and the sulfur isotopes are discussed

Additional details

Publishing Information

Journal Title
Journal of Chengdu College of Geology
Journal Volume
16
Journal Issue
4
Series
J. Chengdu Coll. Geol.
Journal Page Range
83-88
ISSN
0256-2197
CODEN
CHDIE

INIS

Country of Publication
China
Country of Input or Organization
China
INIS RN
21085908
Subject category
S37: INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY; S11: NUCLEAR FUEL CYCLE AND FUEL MATERIALS;
Descriptors DEI
ANHYDRIDES; ARIZONA; EQUILIBRIUM; FRACTIONATION; GEOLOGIC DEPOSITS; HYDROTHERMAL STAGE; INCLUSIONS; ISOTOPE RATIO; ISOTOPIC EXCHANGE; MASS SPECTROSCOPY; MINERALIZATION; OXYGEN 18; SAMPLE PREPARATION; SULFUR ISOTOPES
Descriptors DEC
DEVELOPED COUNTRIES; EVEN-EVEN NUCLEI; ISOTOPES; LIGHT NUCLEI; NORTH AMERICA; NUCLEI; OXYGEN ISOTOPES; SEPARATION PROCESSES; SPECTROSCOPY; STABLE ISOTOPES; USA