Yayınlanmış 1 Ocak 2012
| Sürüm v1
Dergi makalesi
Açık
Cave development and Quaternary uplift history in the Central Pannonian Basin derived from speleothem ages
Oluşturanlar
- 1. MTA CSFK GGI, H-1112 Budapest, Hungary
- 2. HAS Geol Geophys & Space Sci Res Grp, H-1117 Budapest, Hungary
- 3. Eotvos Lorand Univ, Dept Phys & Hist Geol, H-1117 Budapest, Hungary
Açıklama
Several thermal karstic caves are known in the Rozsadomb area of Budapest, Hungary. On a small, 5-6 km(2) territory more than 50 km of cave passages were mapped and documented to host significant cave raft deposits. Cave rafts precipitate at the surface of karst water lakes, and are potential indicators of former karst water levels.
Dosyalar
bib-1d94dbb8-4d96-4a4b-976f-c90ea05657b9.txt
Dosyalar
(198 Bytes)
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