Showing 1 - 20 results of 537 for search '"speleothem"', query time: 0.20s Refine Results
  1. 1

    The Internal Organization of Speleothems by Charles A. Self

    Published 2016-05-01
    “…Članek podaja kratek vodnik po terminologiji ontogenije s poudarkom na jamskih mineralih. Speleothems are secondary cave mineral deposits whose internal organization can be studied by mineralogical techniques. …”
    Get full text
    Article
  2. 2

    Broken Speleothems as Indicators of Tectonic Movements by Stanka Šebela

    Published 2008-12-01
    “…In karst caves broken and non-ideal speleothems are very wide­spread. Mostly they develop because of the instability of the ground due to its composition (loose sand or loam). …”
    Get full text
    Article
  3. 3

    Dolomite in speleothems of Snežna Jama cave by Andrea Martín Pérez, Adrijan Košir, Bojan Otonicar

    Published 2015-07-01
    “…In Snežna Jama cave, Slovenia, extensive speleothems composed of dolomite, aragonite and hydromagnesite have been found, occurring as 5 cm thick globular crusts coating the host rock. …”
    Get full text
    Article
  4. 4
  5. 5
  6. 6

    Speleothem Laminae Counting and Growth Rate by Corey Wilson

    Published 2012-01-01
    Subjects: “…Speleothems, Laminae, Uranium Dating…”
    Get full text
    Article
  7. 7
  8. 8

    Cryogenic ridges: a new speleothem type by Bogdan Onac, Daniel Cleary, Oana Dumitru, Victor Polyak, Ioan Povara, Jonathan Wynn, Yemane Asmerom

    Published 2023-01-01
    “…Here, we report on a new speleothem type (cryogenic ridges) identified in Sohodoalele Mici Cave (SW Romania) within a large chamber near the entrance shaft. …”
    Get full text
    Article
  9. 9
  10. 10
  11. 11
  12. 12
  13. 13
  14. 14
  15. 15
  16. 16
  17. 17
  18. 18
  19. 19

    Features of carbonate speleothems from the Belaya Cave (Zabaykalsky Krai) by Filenko R. A.

    Published 2023-01-01
    “…The research gives the first data on mineralogical studies of carbonate speleothems in the karst cave named Belaya. Dolomite-calcite, calcite-magnesite and hydromagnesite compositions of secondary carbonate sediments in various grottoes of the cave were determined by thermal analysis (TG-DSC) and X-ray diffraction (XRD). …”
    Get full text
    Article
  20. 20