A REVIEW OF THE NON-METALLIC INDUSTRIAL MINERALS OF MONGOLIA: THE IMPACT OF GEOLOGICAL AND GEOGRAPHICAL FACTORS ON THEIR FORMATION AND USE
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dc.contributor.author | Dill H.G. | |
dc.contributor.author | Khishigsuren S. | |
dc.contributor.author | Majigsuren Y. | |
dc.contributor.author | Myagmarsuren S. | |
dc.contributor.author | Bulgamaa J. | |
dc.contributor.author | Hongor O. | |
dc.date.accessioned | 2025-01-18T06:27:55Z | |
dc.date.available | 2025-01-18T06:27:55Z | |
dc.date.issued | 2006 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=14443262 | |
dc.identifier.citation | International Geology Review, 2006, 48, 2, 129-173 | |
dc.identifier.issn | 0020-6814 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/47500 | |
dc.description.abstract | Mongolia is one of the countries of the Asian continental interior rich in ore and non-metallic deposits. Non-metallic commodities of high-unit and high-place value commodities are found throughout the country. Some reference types are discussed in this paper: (1) feldspar-quartz pegmatites; (2) graphite-bearing skarns; (3) contact-metamorphic marbles; (4) igneous and sedimentary gemstone deposits; (5) coarse-grained aggregates (alluvial-fluvial); (6) fine-grained aggregates (fluvial-aeolian); (7) arenaceous-argillaceous byproducts of coal mining; (8) and argillaceous deposits. (Paleo)geography and climate were decisive for the accumulation (e.g., clay and sand deposits) and alteration (e.g., calcareous and gemstone deposits) of many of the non-metallic deposits. The recent geographical and climatic situation is responsible for the poorly developed infrastructure and especially affect the high-value commodities. Acquisition of digital data in the field is a must in a country of the continental interior of Eurasia, in order to save time and space for the transport of samples to accelerate data acquisition. A portable IR mineral analyzer (PIMA) is essential in exploration for industrial minerals and its applicability may be rated as follows, in order of decreasing applicability for different commodities: (1) carbonates, (2) sulfate-bearing rocks, (3) argillaceous rocks, (4) clay-bearing arenaceous rocks, and (5) rocks abundant in alumosilicates/ framework silicates. Copyright © 2006 by V. H. Winston & Son, Inc. All rights reserved. | |
dc.title | A REVIEW OF THE NON-METALLIC INDUSTRIAL MINERALS OF MONGOLIA: THE IMPACT OF GEOLOGICAL AND GEOGRAPHICAL FACTORS ON THEIR FORMATION AND USE | |
dc.type | Статья | |
dc.identifier.doi | 10.2747/0020-6814.48.2.129 |
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