Gold mineralisation in the Caledonides of the British Isles with special reference to the Dolgellau Gold-belt, North Wales and the Southern Uplands, Scotland. Available in 2 volumes.

Two aspects of gold mineralisation in the Caledonides of the British Isles have been investigated: gold-telluride mineralisation at Clogau Mine, North Wales; and placer gold mineralisation in the Southern Uplands, Scotland. The primary ore assemblage at Clogau Mine is pyrite, arsenopyrite, cobaltite, pyrrhotine, chalcopyrite, galena, tellurbismuth, tetradymite, altaite, hessite, native gold, wehrlite, hedleyite, native bismuth, bismuthunite and various sulphosalts. The generalised paragenesis is early Fe, Co, Cu, As and S species, and later minerals of Pb, Bi, Ag, Au, Te, Sb. Electron probe micro-analysis (EPMA) of complex telluride-sulphide intergrowths suggests that these intergrowths formed by co-crystallisation/replacement processes and not exsolution. Minor element chemical variation, in the sulphides and tellurides, indicates that antimony and cadmium are preferentially partitioned into telluride minerals. Mineral stability diagrams suggest that during gold deposition log bf aTe2 was between -7.9 and -9.7 and log bf aS2 between -12.4 and -13.8. Co-existing mineral assemblages indicate that the final stages of telluride mineralisation were between c. 250 - 275oC. It is suggested that the high-grade telluride ore shoot was the result of remobilisation of Au, Bi, Ag and Te from low grade mineralisation elsewhere within the vein system, and that gold deposition was brought about by destabilisation of gold chloride complexes by interaction with graphite, sulphides and tellurbismuth. Scanning electron microscopy of planer gold grains from the Southern Uplands, Scotland, indicates that detailed studies on the morphology of placer gold can be used to elucidate the history of gold in the placer environment. In total 18 different morphological characteristics were identified. These were divided on an empirical basis, using the relative degree of mechanical attrition, into proximal and distal characteristics. One morphological characteristic (a porous/spongy surface at high magnification) is considered to be chemical in origin and represent the growth of `new' gold in the placer environment. The geographical distribution of morphological characteristics has been examined and suggests that proximal placer gold is spatially associated with the Loch Doon, Cairsphairn and Fleet granitoids. Quantitative EPMA of the placer gold reveals two compositional populations of placer gold. Examination of the geographical distribution of fineness suggests a loose spatial association between granitoids and low fineness placer gold. Also identified was chemically heterogeneous placer gold. EPMA studies of these heterogeneities allowed estimation of annealing history limits, which suggest that the heterogeneities formed between 150 and 235oC. It is concluded, on the basis of relationships between morphology and composition, that there are two types of placer gold in the Southern Uplands: (i) placer gold which is directly inherited from a hypogene source probably spatially associated with granitoids; and (ii) placer gold that has formed during supergene processes.

Device for Counting of the Glass Bottles on the Conveyor Belt

In the present paper the results from designing of device, which is a part of the automated information system for counting, reporting and documenting the quantity of produced bottles in a factory for glass processing are presented. The block diagram of the device is given. The introduced system can be applied in other discrete productions for counting of the quantity of bottled production.

Armed Groups and Violence in Paraguay

Armed violence in Paraguay is not a recent phenomenon. During the second half of the XX Century, Paraguay saw the rise of a larger number of underground, revolutionary movements that sought the overthrow of the Alfredo Stroessner’s (1954-1989) government. From among those movements emerged the Partido Patria Libre (or, Free Fatherland, also known for its acronym PPL), made up of a two branches: one legal and the other one, operational. The latter was based on people’s power, as represented by “Ejército del Pueblo Paraguayo” (or, the Paraguayan People’s Army, with acronym EPP). After EPP broke with PPL in March 2008, this Marxist-oriented revolutionary project, which was apparently oriented to put an end to the social, political and economic inequalities in Paraguay, began to carry out markedly criminal activities, which included bank robberies, kidnappings, assassinations, terrorist attacks and armed confrontations. Its strategies and modus operandi utilized by the Armed Revolutionary Forces of Colombia (FARC). Paraguay features a farm sector in a state of crisis, in which cattle-ranchers, peasants and agro-exporting companies live in a constant strife. The Paraguayan Departments that are the most affected by this situation are Concepciόn, San Pedro, Canindeyú y Caazapá, which also suffer from a weak government presence. This deficiency has made these departments ripe for drug-trafficking activity by Brazilian groups such as Primer Comando Capital (i.e., First Capital command), also PCC and Comando Vermelho, (i.e., The Red Command). That is why many peasants, now recruited by EPP, have joined the drug-trafficking business and that, not only as marihuana growers but as “campanas” (i.e., early warning sentinels) for the organization. This helps shape their attitudes for their future involvement in all areas of drug-trafficking. Paraguayan society is the result of social inequity and inequality, such as those resulting from a lack of opportunity. Although Paraguay has successfully recovered from the last world economic crisis, economic growth, by itself, does not ensure an improvement in the quality of life. As long as such economic and social gaps persist and the government fails to enact the policies that would result in a more just society and toward EPP neutralization or containment, the latter is bound to grow stronger. In this context, the situation in Paraguay calls for more research into the EPP phenomenon. It would also seem necessary for Paraguay to promote an open national debate that includes all sectors of society in order to raise consciousness and to induce society to take actual steps to eliminate the EPP, as well as any other group that might arise in the immediate future. EPP has strong connections with the Frente Patriόtico Manuel Rodríguez in Chile and other armed groups and peasant movements in other countries of this region. Although most governments in the region are aware that the armed struggle is not a solution to current problems, it might be worth it to hold a regional debate about armed or insurgent groups in Latin American to seek common strategies and cooperation on dealing with them since the expansion of these armed groups is a problem for all.

On the Mediterranean conveyor belt system

The Mediterranean Sea is a semi-enclosed sea, connected to the Atlantic Ocean through the Gibraltar Strait and subdivided in two different regions by the Sicily Strait. The geographical extension of the basin, the surface heat flux, and the water inflow from the Gibraltar Strait are some of the basic factors determining its horizontal and vertical circulation. In the Mediterranean strong salinity and temperature zonal gradients contribute to maintain the zonal-vertical circulation, while meridional-vertical cells are equally forced by winds and deep water mass formation in three regions, the Gulf of Lyon, the southern Adriatic and the Cretan Sea areas. The objective of this thesis is to study how these cells combine together to form the Mediterranean conveyor belt system. This has never been attempted before so the conclusions are necessarily preliminary. In the first part we discuss the vertical zonal and meridional circulation by reconstructing the Wust Mediterranean vertical salinity and temperature structures in an attempt to evaluate the water mass structure consistent with modern data. Our results confirm that Wust depicted vertical circulation from scarce data is reproduced by the past 27 years observations. The structure of both meridional and zonal circulations was discussed using velocity vertical streamfunctions with two different methods. The first one, eulerian, allowed us to observe vertical structures that were already reported in the literature. Recent studies in the Atlantic Ocean have shown that gyres and eddies have an important influence in the isopycnal vertical circulation. This is called the residual circulation which was computed in this study for the first time. A possible interpretation of horizontal connection between the meridional and zonal cells was discussed using horizontal streamfunction. In the last part of the thesis we have been developing an idealized numerical model to study the vertical circulation in the Mediterranean.

Temperatures, salinity, wind speed, grain sizes and foraminifera abundance in the Great Belt Channel, western Baltic Sea

The Great Belt, the largest inlet to the Baltic Sea, has a deep and well defined channel system. A distinct thermohaline layer at roughly 18 to 20 m of water depth separates the saltier and generally cooler deeper North Sea water from the brackish and warmer surface water. It is practically a current dominated area, with the strongest bottom currents due to prolonged west winds. The size and shape of the surface sediments and their grain size distributions show a close relationship with the prevailing hydrographical conditions. Southerly current marks predominate while northerly directions are confined to 10 to 14 m of water depth. The degree of bioturbation is highest in the uppermost sedimentary cover where practically all original stratification has been destroyed. Various bioturbate structures have been identified with the fauna. Coiling ratios of Ammonia beccarii (Linnaeus) have been successfully applied for correlation in the postglacial sediments of the early Littorina Transgression. The succession shows that in the Boreal brackish water conditions were probably followed by peat and limnic sediments as the sea regressed. With the Littorina Transgression, the sea again entered the area and high sedimentation rates resulted in the major deposits of the Great Belt. At least for the last 4000 years, sedimentation rates had been very low. Present day currents sweep out the sediments, mainly to the southern marginal areas.