Mesz-dolomit a Buda-Pilisi-hegysegben; alternance de calcaire et de dolomie dans la montagne Buda-Pilis

Sikabonyi, L.

Pages 76-80 1952

1952


Document Number: 419566
On the basis of microchemical and microscope analyses of alternating limestone and dolomite layers in the upper Triassic sequence of the Buda-Pilis mountain, Hungary, it is concluded that the sediments are not of biogenic origin but are the porduct of chemical precipitation.

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