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...
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...
Unusual Zn-Au mineralization at the Caijiaying Mine, Hebei, China (2007)
Chang, Z., White, N.C., Crowe, R.W.A., Woodhouse, W., Wilson, N., Whalan, G.
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,...
Unusual Zn-Au mineralization at the Caijiaying Mine, Hebei, China (2007)
Chang, Z., White, N.C., Crowe, R.W.A., Woodhouse, W., Wilson, N., Whalan, G.
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,...
Session 8b
Yoo, B. C., Lee, H. K., White, N. C.
The Gubong deposit consists of five massive, gold-bearing mesothermal quartz veins that fill fractures oriented northeast and northwest along fault shear zones over an area of 14 km2 in Precambrian...
Harris, A. H., Golding, S. D., White, N. C.
Alteration zones at the gold-rich Bajo de la Alumbrera porphyry copper deposit in northwestern Argentina are centered on several porphyritic intrusions. They are zoned from a central copper-iron...
Harris, A. H., Cooke, D. R., White, N. C., Dunlap, W. J., Allen, C. M., Campbell, I., ...
Abstract. Dacitic rocks at the Bajo de la Alumbrera porphyry Cu- Au deposit (NW Argentina) preserve textures that suggest volatiles streamed upwards through intrusions temporally related to ore...
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....
Harris, A. H., Golding, S. D., White, N. C.
Alteration zones at the gold-rich Bajo de la Alumbrera porphyry copper deposit in northwestern Argentina are centered on several porphyritic intrusions. They are zoned from a central copper-iron...
Harris, A. H., Cooke, D. R., White, N. C., Dunlap, W. J., Allen, C. M., Campbell, I., ...
Abstract. Dacitic rocks at the Bajo de la Alumbrera porphyry Cu- Au deposit (NW Argentina) preserve textures that suggest volatiles streamed upwards through intrusions temporally related to ore...
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....
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
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...
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
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...