A. C. Harris

Details der Publikationsliste

Zeitraum

1897 - 2008

Anzahl

21

Co-Autoren

Multimillion year thermal history of a porphyry copper deposit: application of U–Pb, 40Ar/39Ar and (U–Th)/He chronometers, Bajo de la Alumbrera copper–gold deposit, Argentina (2008)

Harris, A. C., Dunlap, W. J., Reiners, P. W., Allen, C. M., Cooke, D. R., White, N. C., ...

Application of multiple chronometers (including U–Pb and 40Ar/39Ar geochronology and zircon and apatite (U–Th)/He thermochronology) to porphyry intrusions at the Bajo de la Alumbrera porphyry...

Multimillion year thermal history of a porphyry copper deposit: application of U-Pb, 40Ar/39Ar and (U-Th)/He chronometers, Bajo de la Alumbrera copper-gold deposit, Argentina (2008)

Harris, A.C., Dunlap, W.J., Reiners, P.W., Allen, C.M., Cooke, D.R., White, N.C., ...

Application of multiple chronometers (including U–Pb and 40Ar/39Ar geochronology and zircon and apatite (U–Th)/He thermochronology) to porphyry intrusions at the Bajo de la Alumbrera porphyry...

Fluid Saturation in the Habo South Porphyry Cu-Au (Mo) System, Southern China: Application of Petrology to Mineral Exploration. (2007)

Harris, A. C., White, N. C., Cooke, D. R., Allen, C., Campbell, I. H.

The Habo South porphyry Cu-Au-(Mo) deposit, China, occurs in a series of granitic intrusions that have been overprinted by extensive K-feldspar-biotite alteration. Veins of quartz, quartz-magnetite,...

Fluid Saturation in the Habo South Porphyry Cu-Au (Mo) System, Southern China: Application of Petrology to Mineral Exploration. (2007)

Harris, A. C., White, N. C., Cooke, D. R., Allen, C., Campbell, I. H.

The Habo South porphyry Cu-Au-(Mo) deposit, China, occurs in a series of granitic intrusions that have been overprinted by extensive K-feldspar-biotite alteration. Veins of quartz, quartz-magnetite,...

Four million years of thermal history—the Bajo de la Alumbrera porphyry Cu–Au deposit, Argentina (2006)

Harris, A. C., Cooke, D. R., Dunlap, W. J., Reiners, P. W., Allen, C. M., White, Noel C., ...

The Bajo de la Alumbrera porphyry deposit formed at shallow crustal levels (2–3 km) during the emplacement of a cluster of silicic intrusions. Copper-gold-bearing veins and associated potassic,...

Four million years of thermal history—the Bajo de la Alumbrera porphyry Cu–Au deposit, Argentina (2006)

Harris, A. C., Cooke, D. R., Dunlap, W. J., Reiners, P. W., Allen, C. M., White, Noel C., ...

The Bajo de la Alumbrera porphyry deposit formed at shallow crustal levels (2–3 km) during the emplacement of a cluster of silicic intrusions. Copper-gold-bearing veins and associated potassic,...

Volatile Loss from High-level Magmas at Bajo De La Alumbrera Porphyry Cu-Au Deposit, NW Argentina (2005)

Harris, A. C., Cooke, D. R., White, N. C., Danyushevsky, L. V., Gilbert, S. E.

At Bajo de la Alumbrera, textural features such as interconnected miarolitic cavities and comb-quartz layers are consistent with volatiles streaming upwards through the mineralizing intrusions....

Volatile Loss from High-level Magmas at Bajo De La Alumbrera Porphyry Cu-Au Deposit, NW Argentina (2005)

Harris, A. C., Cooke, D. R., White, N. C., Danyushevsky, L. V., Gilbert, S. E.

At Bajo de la Alumbrera, textural features such as interconnected miarolitic cavities and comb-quartz layers are consistent with volatiles streaming upwards through the mineralizing intrusions....

The Magmatic-hydrothermal Transition: Volatile Separation in Silicic Rocks at Bajo de la Alumbrera Porphyry Cu-Au Deposit, NW Argentina (2004)

Harris, A. C., Kamenetsky, V. S., White, N. C.

Ore-bearing hydrothermal alteration in porphyry-related deposits largely form from exsolved magmatic fluids derived from crystallising, upper crustal silicic magmas

A Long-lived Porphyry Ore Deposit and Associated Upper Crustal Silicic Magma Bidy, Bajo de la Alumbrera, Argentina (2004)

Harris, A. C., Allen, C. M., Reiners, P. W., Dunlap, W. J., Cooke, D. R., Campbell, I. H., ...

Porphyry Cu deposits form within and adjacent to small porphyritic intrusions that are apophyses to larger silicic magma bodies that reside in the upper parts of the Earth's crusts. Centred on these...

The Magmatic-hydrothermal Transition: Volatile Separation in Silicic Rocks at Bajo de la Alumbrera Porphyry Cu-Au Deposit, NW Argentina (2004)

Harris, A. C., Kamenetsky, V. S., White, N. C.

Ore-bearing hydrothermal alteration in porphyry-related deposits largely form from exsolved magmatic fluids derived from crystallising, upper crustal silicic magmas

A Long-lived Porphyry Ore Deposit and Associated Upper Crustal Silicic Magma Bidy, Bajo de la Alumbrera, Argentina (2004)

Harris, A. C., Allen, C. M., Reiners, P. W., Dunlap, W. J., Cooke, D. R., Campbell, I. H., ...

Porphyry Cu deposits form within and adjacent to small porphyritic intrusions that are apophyses to larger silicic magma bodies that reside in the upper parts of the Earth's crusts. Centred on these...