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pro vyhledávání: '"G.J.S. Govett"'
Autor:
G.J.S. Govett
Publikováno v:
Geochemistry: Exploration, Environment, Analysis. 10:237-249
Professor John S. Webb of the Department of Mining Geology at the Royal School of Mines, Imperial College, London, took his first PhD student (Tony Millman) to Africa in 1949 to try some of the just-emerging geochemical prospecting techniques. In 195
Publikováno v:
Journal of Geochemical Exploration. 43:1-23
In geochemical exploration programs, analytical sub-sample representivity must be maximised to ensure the greatest probability of correctly identifying background and mineralized sites. In the case of particulate gold, the level of representativity i
Autor:
D.S. Clarke, G.J.S. Govett
Publikováno v:
Journal of Geochemical Exploration. 35:225-240
The bedrock geochemical response to epithermal gold mineralization has implications for genetic modelling and secondary media exploration, as well as for rock-geochemistry exploration programmes. Although there is little documentation of the geochemi
Autor:
G.J.S. Govett, M.H. Govett
Publikováno v:
Resources Policy. 2:4-10
Autor:
G.J.S. Govett
Publikováno v:
Journal of Geochemical Exploration. 8:591-599
Autor:
G.J.S. Govett, M.H. Govett
Publikováno v:
Resources Policy. 4:106-114
Whereas the ultimate world supply of minerals is controlled by geological factors, the actual supply at any particular time is controlled by economic factors. Mineral production is a function of investment in exploration, mining, and processing - and
Autor:
G.J.S. Govett
Publikováno v:
Journal of Geochemical Exploration. 6:359-382
Geochemical responses to deeply buried mineralization in surface soils may possibly be overlooked because of a preoccupation with magnitude of response rather than relative magnitude of response in adjacent samples; i.e., the shape or form of the pro
Publikováno v:
Journal of Geochemical Exploration. 18:195-204
An anomalous Pb pattern occurs in drainage channel soils adjacent to the Elura Zn-Pb-Ag deposit and forms a fan shaped train extending at least 5 km on a mature weathering surface in semi-arid central-west New South Wales. This Pb pattern without a Z