Tectonic and eustatic control of bauxite formation in the Transdanubian Central Range (Hungary)

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Abstract

A significant part of factors control the karst-bauxite formation is connected with transgressive-regressive (T-R) facies cycles. An analysis of the role of tectonically vs. eustatically controlled T-R cycles in the bauxite genesis was carried out. The primary bauxite deposits are connected with 2nd order unconformities and they are covered by 2nd order facies cycles. These "productive' unconformities are tectonically controlled. -from Author

Original languageEnglish
Pages (from-to)253-262
Number of pages10
JournalActa Geologica Hungarica
Volume34
Issue number3
Publication statusPublished - 1991

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bauxite
unconformity
tectonics
karst

ASJC Scopus subject areas

  • Geology

Cite this

Tectonic and eustatic control of bauxite formation in the Transdanubian Central Range (Hungary). / Haas, J.

In: Acta Geologica Hungarica, Vol. 34, No. 3, 1991, p. 253-262.

Research output: Contribution to journalArticle

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