Abstract Laterites are regoliths developed under tropical to subtropical conditions and are host to key deposit types, notably bauxites (major sources of Al, derived from weathering of aluminosilicate rocks) and Ni-Co laterites (derived from ultramafic rocks). Research on the western Tethys region, where bauxites and Ni-Co laterites developed during the Mesozoic and Cenozoic, probably peaking at the Paleocene-Eocene thermal maximum when geology, paleogeography, and climate were ideal for the deep weathering of favorable lithologies, is reported in this article. Bauxites were developed on the rocks forming the continental margins to the various branches of the Tethys Ocean and were already forming in the Triassic, whereas the Ni-Co laterites developed on fragments of obducted ophiolite from the Tethys Ocean, which were only uplifted and exposed to weathering after the Jurassic. Residual lateritic bauxites are known in the region but karst bauxites are much more common. Ni-Co laterites are found as residual profiles, ranging from oxide, to clay-silicate, to hydrous-silicate types, but are also represented by distinctive, extensively redeposited clay-oxide ores. This diversity of styles probably reflects differences in topography and uplift history because the deposits all formed within a similar, restricted climatic time window. The bauxite belt extends from Spain in the west, through the type locality of Les Baux in France, and intermittently through the Balkans, Greece, and Turkey to Iran and beyond. Bauxite resources in Europe constitute around 2% of the world’s current known stock. Significant Ni-Co laterites are found in a more restricted geographic area stretching from Serbia to Turkey. The bulk of both Al and Ni-Co production currently comes from Greece, today accounting for around 1% of world production of both Ni and bauxite, and with published resources on the order of 650 Mt @ >50% Al 2 O 3 ; other mines are located in Turkey, Albania, and Kosovo. Ferronickel plants are located in Greece, but also in the Former Yugoslav Republic of Macedonia, and Kosovo. The region has significant potential for the discovery of additional bauxite resources, although they would most likely be karst bauxites, less suited to large-scale mining efforts. Many undeveloped Ni-Co deposits are recorded in the region, with a recent focus to unlock the potential of oxide mineralization using novel hydrometallurgical technologies. Particularly noted is the potential for large low-grade redeposited lateritic Ni-Co-Fe deposits: Mokra Gora in Serbia, for example, has a resource of more than 1 Gt @ 0.7% Ni and 0.05% Co.

ABSTRACT (S.K. Donovan) Dr. Verners Aleksandrs Zans was a Latvian geologist with wide interests who worked as an associate professor at the University of Riga until 1944. After the Second World War, he and his family were interned in a camp for displaced persons near Hamburg, where they lived until Zans was appointed government geologist in Jamaica, at the head of the modern Geological Survey Department. Zans and his family arrived in Jamaica in October 1949. The Survey grew and flourished under Zans. His work in Jamaica was diverse, including studies of mineral deposits, bauxite genesis, karst hydrology, and the marine physiography of the near shore. Zans formulated a new theory of bauxite formation, alumina-rich deposits derived from older, but topographically higher, beds accumulating in karst depressions on the surface of the mid-Cenozoic White Limestone Group. Under his leadership the Survey published the 1958 1:250,000 provisional geological map of Jamaica, the first new map of the island since 1865. Zans died unexpectedly in September 1961.

The completeness of an exploration project is of crucial importance for making a decision to start or to give up a mining investment, or to continue the exploration to get complementary information. The authors discuss this problem on the example of the Halimba bauxite deposit, Hungary. Two-hundred thirty-seven core drills were executed on a 14 ha area. Resource calculations were carried out in 12 subsequent stages by fuzzy arithmetic with the aim to quantify the uncertainties of ore tonnage and grade. Prior information and prior probabilities were applied to complete the exploration data. Their validity was checked by the subsequent stages. Ranges of influence for the main variables were calculated by geostatistical methods (variograms). Spatial variability and spatial continuity of the orebodies were mathematically evaluated. The authors found that there is no single “overall” value to express the completeness of a mineral exploration program, but the main geological, mining, and economic factors must be evaluated separately and ranked according to their importance. The reliability of the results can be quantified by the application of new “uncertainty-oriented” mathematical methods.