Compositional, Order/Disorder, and Stable Isotope Characteristics of Al‐Fe Epidote, State 2–14 Drill Hole, Salton Sea Geothermal System
暂无分享,去创建一个
D. Bird | L. Caruso | C. J. Janik | J. Liou | M. Cho
[1] D. Bird,et al. Prograde Phase Relations in the State 2–14 Well Metasandstones, Salton Sea Geothermal Field, California , 1988 .
[2] C. C. Carson,et al. Thermal Regime of the State 2–14 Well, Salton Sea Scientific Drilling Project , 1988 .
[3] D. Bird,et al. Epidote‐Bearing Veins in the State 2–14 Drill Hole: Implications for Hydrothermal Fluid Composition , 1988 .
[4] D. Bird,et al. Prehnite—Epidote Phase Relations in the Nordre Aputitëq and Kruuse Fjord Layered Gabbros, East Greenland , 1987 .
[5] Alan E. Williams,et al. Saline brines and metallogenesis in a modern sediment-filled rift: the Salton Sea geothermal system, California, U.S.A. , 1987 .
[6] S. D. Mcdowell. Composition and structural state of coexisting feldspars, Salton Sea geothermal field , 1986, Mineralogical Magazine.
[7] D. Bird,et al. Hydrothermal mineralogy of calcareous sandstones from the Colorado River delta in the Cerro Prieto geothermal system, Baja California, Mexico , 1985, Mineralogical Magazine.
[8] N. Shikazono. Compositional variations in epidote from geothermal areas. , 1984 .
[9] Alan E. Williams,et al. Calc-silicate mineralization in active geothermal systems , 1984 .
[10] K. Tazaki. Andradite Garnet in Altered Basalt From Borup Fiord, Ellesmere Island, Northwest Territories , 1983 .
[11] G. Cavarretta,et al. Formation of authigenic minerals and their use as indicators of the physicochemical parameters of the fluid in the Larderello-Travale geothermal field , 1982 .
[12] D. Bird,et al. Theoretical prediction of phase relations among aqueous solutions and minerals: Salton Sea geothermal system , 1981 .
[13] C. Graham. Experimental hydrogen isotope studies III: Diffusion of hydrogen in hydrous minerals, and stable isotope exchange in metamorphic rocks , 1981 .
[14] H. Helgeson,et al. Chemical interaction of aqueous solutions with epidote-feldspar mineral assemblages in geologic systems; 1, Thermodynamic analysis of phase relations in the system CaO-FeO-Fe 2 O 3 -Al 2 O 3 -SiO 2 -H 2 O-CO 2 , 1980 .
[15] S. Sheppard,et al. Experimental hydrogen isotope studies, II. Fractionations in the systems epidote-NaCl-H2O, epidote-CaCl2-H2O and epidote-seawater, and the hydrogen isotope composition of natural epidotes , 1980 .
[16] T. Heaton,et al. Experimental hydrogen isotope studies—I. Systematics of hydrogen isotope fractionation in the systems epidote-H2O, zoisite-H2O and AlO(OH)-H2O , 1980 .
[17] H. Taylor,et al. An Oxygen and Hydrogen Isotope Study of the Skaergaard Intrusion and its Country Rocks: a Description of a 55 M.Y. Old Fossil Hydrothermal System , 1979 .
[18] D. K. Bird. Chemical interaction of aqueous solutions with epidote-feldspar mineral assemblages in geologic systems , 1978 .
[19] H. Taylor,et al. 18 O/ 16 O, D/H, and 13 C/ 12 C studies of the Tertiary igneous complex of Skye, Scotland , 1977 .
[20] D. McDowell,et al. Active metamorphism in the Salton Sea geothermal field, California: mineralogical and mineral chemical changes with depth and temperature in sandstone , 1977 .
[21] H. Taylor,et al. Hydrogen and Oxygen Isotope Evidence for the Origins of Water in the Boulder Batholith and the Butte Ore Deposits, Montana , 1974 .
[22] J. Liou. Synthesis and Stability Relations of Epidote, Ca2Al2FeSi3O12 (OH) , 1973 .
[23] W. Dollase. Mössbauer spectra and iron distribution in the epidote-group minerals , 1973 .
[24] S. Ruby. Why Misfit When You Already Have X2 , 1973 .
[25] M. J. Holdaway. Thermal stability of Al-Fe epidote as a function of $$f_{{\text{o}}_{\text{2}} } $$ and Fe content , 1972 .
[26] P. Robinson,et al. Crustal Spreading in Southern California , 1972, Science.
[27] Y. Seki. LOWER-GRADE STABILITY LIMIT OF EPIDOTE IN THE LIGHT OF NATURAL OCCURRENCES , 1972 .
[28] James H. Dieterich,et al. Stress-history of folding , 1969 .
[29] L. Muffler,et al. Active Metamorphism of Upper Cenozoic Sediments in the Salton Sea Geothermal Field and the Salton Trough, Southeastern California , 1969 .
[30] H. Helgeson. Geologic and thermodynamic characteristics of the Salton Sea geothermal system , 1968 .
[31] N. Chatterjee. Experiments on the phase transition calcite+wollastonite+ +epidote=grossular-andraditess+CO2+H2O , 1967 .
[32] H. Craig. Isotopic Composition and Origin of the Red Sea and Salton Sea Geothermal Brines , 1966, Science.
[33] R. Strens. Stability and Relations of the Al-Fe Epidotes , 1965 .
[34] R. Kretz. Note on some equilibria in which plagioclase and epidote participate , 1963 .
[35] Donald K. Grubbs,et al. Geothermal Brine Well: Mile-Deep Drill Hole May Tap Ore-Bearing Magmatic Water and Rocks Undergoing Metamorphism , 1963, Science.
[36] W. S. FYFE. Stability of Epidote Minerals , 1960, Nature.
[37] A. Miyashiro,et al. Enlargement of the composition field of epidote and piemontite with rising temperature , 1958 .
[38] J. Harpum. FORMATION OF EPIDOTE IN TANGANYIKA , 1954 .
[39] H. Ramberg. The Facies Classification of Rocks: A Clue to the Origin of Quartzo-Feldspathic Massifs and Veins , 1949, The Journal of Geology.