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020 _a9783031609664
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024 7 _a10.1007/978-3-031-60966-4
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072 7 _aSCI019000
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245 1 0 _aGeology, Petrochemistry and Ore Content of Carbonaceous Deposits of the Kumak Ore Field
_h[electronic resource] /
_cedited by Alexandra V. Panteleeva, Aleksandr V. Snachev.
250 _a1st ed. 2024.
264 1 _aCham :
_bSpringer Nature Switzerland :
_bImprint: Springer,
_c2024.
300 _aVII, 126 p. 42 illus., 38 illus. in color.
_bonline resource.
336 _atext
_btxt
_2rdacontent
337 _acomputer
_bc
_2rdamedia
338 _aonline resource
_bcr
_2rdacarrier
347 _atext file
_bPDF
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490 1 _aSpringer Geology,
_x2197-9553
505 0 _aGeological structure and history of exploration of the Anikhov graben (Southern Urals, Russia) -- Geological structure of the Kumak ore field (Southern Urals, Russia) -- Petrographic features and carbonaceous matter of the black shales of the Kumak deposit (Southern Urals, Russia) -- Petrogeochemical features and conditions of accumulation of carbonaceous deposits of the Bredy Formation (Southern Urals, Russia) -- Ore potential of carbonaceous deposits of the Kumak deposit (Southern Urals, Russia) -- Model of formation of the Kumak gold deposit (Southern Urals, Russia) -- The concept of industrial development of gold deposits in the Kumak ore field (Southern Urals, Russia).
520 _aThe main prospects for expanding the mineral resource base of gold are associated with the discovery of typical ore objects within the distribution of productive black shale strata in the Orenburg part of the Southern Urals. The solution of this problem is significantly associated with the discovery, evaluation and involvement in the industrial development of gold deposits lying in the black shale strata. Their practical significance, based on existing concepts, can be considered in several aspects: first of all, it is a possible source of metals, and secondly, they are a reducing geochemical barrier for the deposition of ore matter of deep fluids. The formations of the black shale formation are a favorable geochemical environment for the primary concentration of gold, platinum group elements, tungsten, molybdenum and other metals. Areas of manifestation of tectonic activity, zonal and contact metamorphism, and the dyke complex are of great importance. Moreover, carbonaceous deposits are a very informative material for the reconstruction of paleogeographic and physico-chemical conditions of their accumulation. In this regard, the ore-containing black shales of the Kumak deposit, whose rocks have a specialization in gold, seem to be a very attractive object for a comprehensive study of ore content. They may be of great practical importance for the search for new deposits in the Southern Urals and in other regions with a similar geological structure.
650 0 _aEarth sciences.
_965010
650 0 _aGeography.
_962292
650 0 _aSedimentology.
_965837
650 0 _aPaleontology .
650 0 _aMineralogy.
_966552
650 0 _aGeology.
_965838
650 0 _aGeochemistry.
_970590
650 1 4 _aEarth and Environmental Sciences.
_967852
650 2 4 _aSedimentology.
_965837
650 2 4 _aPaleontology.
650 2 4 _aMineralogy.
_966552
650 2 4 _aGeology.
_965838
650 2 4 _aGeochemistry.
_970590
700 1 _aPanteleeva, Alexandra V.
_eeditor.
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_1https://orcid.org/0000-0003-1463-1615
_4edt
_4http://id.loc.gov/vocabulary/relators/edt
_980425
700 1 _aSnachev, Aleksandr V.
_eeditor.
_0(orcid)0000-0002-9275-0081
_1https://orcid.org/0000-0002-9275-0081
_4edt
_4http://id.loc.gov/vocabulary/relators/edt
_980426
710 2 _aSpringerLink (Online service)
773 0 _tSpringer Nature eBook
776 0 8 _iPrinted edition:
_z9783031609657
776 0 8 _iPrinted edition:
_z9783031609671
776 0 8 _iPrinted edition:
_z9783031609688
830 0 _aSpringer Geology,
_x2197-9553
_974538
856 4 0 _uhttps://doi.org/10.1007/978-3-031-60966-4
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