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Artigo Revisado por pares

Csaba Lorinţ, Monica Rădulescu, Grigore Buia,

Tópico(s): Heavy metals in environment

2011 - Springer Science+Business Media | Environmental Geochemistry and Health

Capítulo de livro

Ioan Povară,

Comarnic Cave is situated in southwestern Romania, in a region in which the Mesozoic limestones cover an ... streams that recharge permanent or temporary karst springs. Comarnic Cave (6201 m) represents a hydrological penetration of ... level, erosional and/or solutional features are abundant. Comarnic Cave is well known for its spectacular chert ...

Tópico(s): Marine and environmental studies

2018 - Springer International Publishing | Cave and karst systems of the world

Artigo Revisado por pares

Piotr Karnkowski, Henryk Jurkiewicz,

... OF THE WĘGLOWIC MARLS WITH MARLS FROM THE COMARNIC AREA (RUMANIA) The Weglowiec marls, being an object of comparison with the Comarnic marls, belong to the Subsilesian unit of the ... series. The microfauna from both the Weglowiec and Comarnic marls listed in the Polish text and in ... The fauna from the middle pad of the Comarnic marls corresponds to a foraminifer assemblage of the middle part of the Weglowiec marls. The Comarnic assemblage consists of the same foraminifer species as ... mentioned above. The discussed part both of the Comarnic and the Weglowiec marIs is of upper Campanian ...

Tópico(s): Ancient and Medieval Archaeology Studies

1963 - Polish Geological Institute | Geological Quarterly

Artigo Revisado por pares

Alfred Bögli,

Solutional landforms in limestone have been described for over a hundred years, but landforms of similar morphology on highly siliceous sandstones and quartzites have also been identified in a wide variety of environments and generally termed pseudokarst. These include large bedrock pinnacles and towers, caves, corridors, grikes, solution basins and runnels, and even silica speleothems. Quartzites and quartz sandstones have been held to be amongst the most chemically resistant of rocks, but the ...

Tópico(s): Linguistics and language evolution

1974 - Elsevier BV | Geoforum