Litosfera = Lithosphere 20(3), 411-431 (2020). doi:10.24930/1681-9004-2020-20-3-411-431

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The temperature range of the formation of skarns suggests the melting of limestones in the heat-and-mass transfer columns of the Earth’s crust. The ontogenic analysis of structures of the carbonate rocks in some Ural skarn objects indicates the presence of bodies, which...

REE and Y patterns for calcite and pyrite of the Orlovka gold deposit were considered. Two environments, in which evolved ore-forming fluid, are determined: early high-temperature (>200-250ºC) and later low-temperature (

Research subject. Geochemistry and mineralogy of chromium in the Paleozoic carbonate rocks of the Northern Urals. A recent review of these data, published more than half a century ago during the flourishing of Russian geology (1980– 1997), showed that these data were un...

Subject of research . The upper Permian reefs of the Yangtze block of southern China are considered. Among them there are two species which differ in location in the basin and the nature of the internal structure. Methods and results. On the basis of geological and lith...

In the paper we report experimental study of biomineralization processes occurring on biogeochemical barriers involving community of bacteria from natural groundwater . After 2-years experiment, the formation of a crystalline iron-containing mineral occurred in the cont...

This publication provides an overview of the rare earth elements systematics in Pre-Ordovician phosphorites from various regions of the world. Based on the analysis of significant data bank it shows that currently there are no universal parameters, guided by which, coul...