Pregled bibliografske jedinice broj: 113664
Diagenetic concretions from the cave clastic sediment, Cave in Tounj quarry, Croatia.
Diagenetic concretions from the cave clastic sediment, Cave in Tounj quarry, Croatia. // Acta carsologica, XXVII/2 (1998), 6; 97-103 (podatak o recenziji nije dostupan, članak, znanstveni)
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Naslov
Diagenetic concretions from the cave clastic sediment, Cave in Tounj quarry, Croatia.
Autori
Lacković, Damir
Izvornik
Acta carsologica (0583-6050) XXVII/2
(1998), 6;
97-103
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
cave concretions; cave sediment; Cave in Tounj quarry; Croatia
Sažetak
Diagenetic concretions from Cave in Tounj quarry (central Croatia) are studied. Concretions are found in non-cemented unsorted clastic cave deposit. They consist of particles of different size (clay to pebble) and from diferent provenance. One part of calcite and clay minerals are coming from speleothems and cave walls limestone. Detrital particles: chert, quartz, muscovite, chlorite, ilmenite, magnetite, and most of clay, are probable transported into the cave from Triassic and Pleistocene clastic sediments from the surface. Autochtonous constituents of concretions are limonitic pizoids and some calcite cement. Composition of concretion is similar to the composition of surrounding non-cemented sediment.
Izvorni jezik
Engleski
