Lorándite

Abstract: Here we report the first example of a thallium-only deposit, which was discovered in the northeast margin of the Yangtze block, eastern China, in the transition zone between the Yangtze Block, North China Block and Dabie orogenic belt. Ore from the Xiangquan deposit will be mined, ore-dressed and smelted independently for thallium. The ore deposit is hosted in Lower Ordovician micrite, calcilutite and marl within the Dalongwang Mountain Xiao Mountain anticline. The ore zones are fold and fault controlled. Thallium occurs mainly in pyrite but minor amounts form as lorandite (TlAsS2) and hutchinsonite (TlFeS2). Fluid inclusion studies of two stages of fluorite intimately associated with ore-forming pyrite yielded homogenization temperatures of 120 to 220 °C with a salinity of 1.5 to 6.0 equivalent wt.% NaCl. Thallium was originally derived by hydrothermal emanations onto the sea floor and deposited in calcareous sediments. Subsequently in the Early Cretaceous (Yanshanian period) these source beds were reworked to form thallium enriched minerals in hydrothermal veins.

Abstract: Very few investigations have dealt with the environmental impact of the highly toxic metal thallium (Tl), and its subsequent dispersion through natural processes and human activities such as mining and farming. This study is focused on high concentrations of Tl in rocks in SW Guizhou, China, that are related to several widely scattered disseminated gold–mercury–arsenic and coal deposits, and a primary Tl deposit within an Au–As–Hg–Tl metallogenic belt of the Huijiabao anticline. The Tl, Hg and As in the Lanmuchang Hg–Tl deposit area are associated with the abundant occurrence of sulfide minerals such as lorandite, realgar, orpiment and cinnabar. Concentrations of Tl range from 100 to 35 000 ppm in sulfide ores, and 39–490 ppm in host rocks. The enrichment of Au, Tl, Hg, As, and Sb in the Yanshang gold mineralized area reflects the occurrence of Au mineralization and its mineral assemblage of Tl–Hg–As–Sb sulfides. Thallium ranges from 0.22 to 16 ppm in Au ores and host rocks. Thallium in coals is enriched up to 46 ppm within the Au–As–Hg–Tl metallogenic belt, and is derived from the regional Au–As–Hg–Tl mineralization. Mercury and As show a similar distribution to Tl with high concentrations in sulfide ores, coals and host rocks. Human populations living near and downstream of Tl deposits and Tl-bearing ore deposits are susceptible to Tl contamination because of its high toxicity and high uptake rate by crops. The dispersion of Tl, Hg and As associated with the primary mineralization of Au–As–Hg–Tl can be traced through physical erosion and chemical weathering, producing secondary dispersion into soils, groundwater and surface water and crops. Mining activities compound the natural processes, readily dispersing Tl into the surface environment. The Lanmuchang area illustrates Tl contamination related to a Tl-rich deposit due to both natural processes and the impact of mining. The Yanshang area demonstrates Tl contamination related toa Tl-bearing gold deposit, caused by natural processes in the absence of mining activity.

Abstract: A method for the determination of major and trace elements in some minerals (orpiment, realgar, lorandite, dolomite and markasite) from the Allchar mine, Republic of Macedonia, based on k 0 -instrumental neutron activation analysis (k 0 -INAA) is presented. The concentration of U and Th in all investigated minerals was found to be 50%), especially in realgar and orpiment, due to the high background produced by 76 As activity after irradiation by thermal neutrons, makes the determination of short-lived radionuclides present at micro levels by k 0-INAA impossible. To increase the accuracy of the determination and to enlarge the number of elements measured, arsenic should be separated from the samples.