Early dolomitisation of Late Triassic platform carbonates in the Transdanubian Range (Hungary)
J Haas, A Demény - Sedimentary Geology, 2002 - Elsevier
In the Late Triassic, a large carbonate platform system came into existence in the
Transdanubian Range (TR) producing a 1.5-to 2-km-thick carbonate succession. The lower
part of the platform carbonate series is made up of cyclic peritidal dolomite (Main Dolomite
Formation), while the upper one consists of cyclic peritidal limestone (Dachstein Limestone
Formation). However, there is a transitional member of remarkable thickness between them
consisting of partially dolomitised limestone and calcitic dolomite. This study focuses on the …
Transdanubian Range (TR) producing a 1.5-to 2-km-thick carbonate succession. The lower
part of the platform carbonate series is made up of cyclic peritidal dolomite (Main Dolomite
Formation), while the upper one consists of cyclic peritidal limestone (Dachstein Limestone
Formation). However, there is a transitional member of remarkable thickness between them
consisting of partially dolomitised limestone and calcitic dolomite. This study focuses on the …
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