PORPHYRY COPPER DEPOSIT EXPOSED IN LIBERTY OPEN-PIT MINE NEAR ELY NEVADA .2. FORMATION OF HYDROTHERMAL ALTERATION ZONES

[1] THE CALCULATED FUGACITY OF WATER TO 1000-DEGREES-C AND 10,000 BARS [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1964, 28 (MAY) : 713 - 715

[2] BONORINO FG, 1959, GEOL SOC AM BULL, V70, P53, DOI 10.1130/0016-7606(1959)70[53:HAITFR]2.0.CO

[3] 2

[4] PORPHYRY COPPER DEPOSIT EXPOSED IN LIBERTY OPEN-PIT MINE NEAR ELY NEVADA .I. SYNGENETIC FORMATION [J]. ECONOMIC GEOLOGY, 1967, 62 (01) : 57 - &

[5] Hemlery JJ., 1964, ECON GEOL BULL SOC, V59, P538, DOI [DOI 10.2113/GSECONGEO.59.4.538, 10.2113/gsecongeo.59.4.538]

[6] SOME MINERALOGICAL EQUILIBRIA IN THE SYSTEM K2O-AL2O3-SIO2-H20 [J]. AMERICAN JOURNAL OF SCIENCE, 1959, 257 (04) : 241 - 270

[7] HEMLEY JJ, 1961, 424D US GEOL SURV PR, pD338

[8] FUGACITY OF WATER AT HIGH TEMPERATURES AND PRESSURES [J]. JOURNAL OF PHYSICAL CHEMISTRY, 1954, 58 (04) : 316 - 317

[9] LOVERING TS, 1950, COLO SCH MINES Q, V45, P231

[10] MEYER C, 1963, 12 NATL AC SCI NAT R, P25

[1] THE CALCULATED FUGACITY OF WATER TO 1000-DEGREES-C AND 10,000 BARS [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1964, 28 (MAY) : 713 - 715

[2] BONORINO FG, 1959, GEOL SOC AM BULL, V70, P53, DOI 10.1130/0016-7606(1959)70[53:HAITFR]2.0.CO

[3] 2

[4] PORPHYRY COPPER DEPOSIT EXPOSED IN LIBERTY OPEN-PIT MINE NEAR ELY NEVADA .I. SYNGENETIC FORMATION [J]. ECONOMIC GEOLOGY, 1967, 62 (01) : 57 - &

[5] Hemlery JJ., 1964, ECON GEOL BULL SOC, V59, P538, DOI [DOI 10.2113/GSECONGEO.59.4.538, 10.2113/gsecongeo.59.4.538]

[6] SOME MINERALOGICAL EQUILIBRIA IN THE SYSTEM K2O-AL2O3-SIO2-H20 [J]. AMERICAN JOURNAL OF SCIENCE, 1959, 257 (04) : 241 - 270

[7] HEMLEY JJ, 1961, 424D US GEOL SURV PR, pD338

[8] FUGACITY OF WATER AT HIGH TEMPERATURES AND PRESSURES [J]. JOURNAL OF PHYSICAL CHEMISTRY, 1954, 58 (04) : 316 - 317

[9] LOVERING TS, 1950, COLO SCH MINES Q, V45, P231

[10] MEYER C, 1963, 12 NATL AC SCI NAT R, P25