The use of space survey materials Resurs-P, Canopus-PSS, ASTER and landsat for forecasting uranium-molybdenum and chromite-platinum mineralization in the Polar Urals

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Methods of complex analysis of the results of space, gravimetric and magnetometric surveys for localization of ore-promising sites in the Polar Urals within the nomenclature sheets R-42, Q-42 have been developed. When decoding the materials of multi-zone satellite imagery of medium (ASTER, Landsat) and high (Canopus-PSS, Resurs-P) resolution, linear, arc and ring structural elements controlling the localization of uranium-molybdenum and chromite-platinum mineralization of the Polar Urals were revealed. The decoding of zones of metasomatically altered rocks in various spectral IR channels made it possible to localize areas for detailed work. Based on high-resolution satellite imagery, large-scale structural and tectonic schemes have been prepared and areas of detail for ground-based verification work have been outlined.

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作者简介

G. Milovsky

Scientific Geoinformation Center of the Russian Academy of Sciences

编辑信件的主要联系方式.
Email: oregas@mail.ru
俄罗斯联邦, Moscow

A. Aparin

Scientific Geoinformation Center of the Russian Academy of Sciences

Email: oregas@mail.ru
俄罗斯联邦, Moscow

A. Ibragimov

Scientific Geoinformation Center of the Russian Academy of Sciences

Email: oregas@mail.ru
俄罗斯联邦, Moscow

A. Kirsanov

All-Russian Scientific Research Geological Institute named after A.P. Karpinsky

Email: oregas@mail.ru
俄罗斯联邦, St. Petersburg

K. Lipiyainen

All-Russian Scientific Research Geological Institute named after A.P. Karpinsky

Email: oregas@mail.ru
俄罗斯联邦, St. Petersburg

参考

  1. Boytsov V.E., Vercheba A.A. Geologo-promyshlennye tipy mestorozhdenij urana: M.: KDU, 2008. 310 p.
  2. Geologicheskaya karta SSSR. Masshtab 1:200000. Seriya Severo-Ural’skaya. List Q-42-I. Ob”yasnitel’naya zapiska. M.: VSEGEI, 1984. (Ministerstvo geologii SSSR, Glavnoe Tyumenskoe PGO).
  3. Gosudarstvennaya geologicheskaya karta Rossijskoj Federacii. Masshtab 1:200000. Vtoroe izdanie. Seriya Polyarno-Ural’skaya. List R-42-XXXI, XXXII. Ob”yasnitel’naya zapiska. SPb., VSEGEI, 2003. (MPR Rossii po Yamalo-Neneckomu AO).
  4. Gosudarstvennaya geologicheskaya karta Rossijskoj Federacii. Masshtab 1 : 1000000 (tret’e pokolenie). Seriya Zapadno-Sibirskaya. List Q-42 Salekhard: Ob”yasnitel’naya zapiska. SPb.: VSEGEI, 2014. 396 p.
  5. Gurskaya L.I., Smelova L.V. Platinometal’noe mineraloobrazovanie i stroenie massiva Syum-Keu (Polyarnyj Ural) // Geologiya rudnyh mestorozhdenij, 2003, 45, 4, 353-371.
  6. Dodin D.A., Dodina T.S., Zoloev K.K., Koroteev V.A., Chernyshov N.M. Platina Rossii: sostoyanie i perspektivy // Litosfera. 2010. № 1. P. 3–36.
  7. Mashkovtsev G.A., Konstantinov A.K., Michuta A.K., Shumilin M.V., Shchetochkin V.N. Uran rossijskih nedr. M.: VIMS, 2010, 850 p.
  8. Milovsky G.A., Kirsanov A.A., Lipiyainen K.L., Aparin A.D. Prognozirovanie zoloto-serebryanogo orudeneniya v predelah Pepenveemskoj rudnoj zony CHukotskogo poluostrova na osnove kosmicheskoj s”emki Resurs, Kanopus i ASTER // Issled. Zemli iz kosmosa. 2023. № 4. P. 26‒41.
  9. JPL (https://speclib.jpl.nasa.gov/library).
  10. USGS (https://crustal.usgs.gov/speclab/QueryAll07a.php).

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1. JATS XML
2. Fig. 1. Tectonic scheme at a scale of 1:500000. R-42-XXXI. Legend in Fig. 1a.

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3. Fig. 2. Maps of gravitational and magnetic fields at a scale of 1:500000. R-42-XXXI.

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4. Fig. 3. Map of metasomatic rocks based on ASTER space survey materials. R-42-XXXI.

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5. Fig. 4. Khakharempe detail area. Mineral resources map at scale 1:200000. R-42-XXXI. See Fig. 4a for legend.

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6. Fig. 5. Detailed area of ​​Khakharempe. Space imagery Resurs-P route No. 9861_1. Channel 10. R-42-XXXI.

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7. Fig. 6. Geological scheme of the southern part of the hyperbasite massif Syum-Keu with the allocation of ore fields. Q-42-I. Legend in Fig. 6a.

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8. Fig. 7. Khadatinsky detailing area.

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9. Fig. 8. Khadatinsky detailing area. Structural features of dunite bodies.

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10. Fig. 9. Detailed section Khadatinsky. Resource-P route No. 2960_1.

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11. Fig. 10. Detailed section of the South Khadatinsky area.

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