1887
ASEG2006 - 18th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Different-aged (from recent to Paleozoic ones) fluvial valley and channel systems are collectors for mineral deposits of wide spectrum: from distal gravitational accumulations (placers of Au, PGE, Sn) through proximal placers (diamond, heavy minerals, and finegrained gold) to leached deposits on complex geochemical barriers (U, Mo, TR). The wide tectonic diversity in the Eurasia North (cratons, different-aged plates and erogenic belts) allows to compare styles of palaeovalley and palaeochannel minerageny according to the type of the Earth crust.

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/content/journals/10.1071/ASEG2006ab130
2006-12-01
2026-01-14
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References

  1. Afanasiev A.M., 2004, Features of sedimentary sequences and ore-forming processes in uranium-bearing regions of young platform covers - Geology of mineral deposits of uranium, rare and rare-earth metals: VIMS, Moscow, 37 – 46, (in Russian).
  2. Kartashov, I.P., Geological features of alluvial placers: Economic Geology, 1971, v.66, 879 - 885.
  3. Patik-Kara N.G., 1995. Placer mineral deposits in arid environments: Lithology and Mineral Resources, v.l. p. 1 – 13.
  4. Patik-Kara, N.G., Konoplev A.D., Spasskaia, I.L, 2003, Late Cenozoic paleochannel mineral deposits of the Trans-Ural peneplain: XVIINQUA Congress, Reno, Nevada. Abstracts.
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  • Article Type: Research Article
Keyword(s): mineral deposits; paleochannels
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