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The Bauxites discovered on Mt. Ravna Gora in Hrvatsko Zagorje (Geological Setting, Composition, Origin) (CROSBI ID 79022)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Šinkovec, Boris ; Šimunić, Antun The Bauxites discovered on Mt. Ravna Gora in Hrvatsko Zagorje (Geological Setting, Composition, Origin) // Rudarsko-geološko-naftni zbornik, 8 (1996), 67-76

Podaci o odgovornosti

Šinkovec, Boris ; Šimunić, Antun

engleski

The Bauxites discovered on Mt. Ravna Gora in Hrvatsko Zagorje (Geological Setting, Composition, Origin)

Clayey bauxites originally underlain by the Anisian dolomites and overlain by Middle Eocene sediments was discovered on Mt. Ravna gora in 1992. in overturned position. The bauxite is of kaolinitic- diasporic-boehmitic composition and resembles the Oligocene bauxites of Slovenia. On the basis of the bauxite textures, the contents of microelements and other indicators it was tentatively contents of microelements and other indicators it was tentatively concluded that this bauxite has been resedimented from bauxites of Triassic age.

Clayey bauxite; Diaspore; Eocene; Hrvatsko Zagorje

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Podaci o izdanju

8

1996.

67-76

objavljeno

0353-4529

Povezanost rada

Geologija

Indeksiranost