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Excerpt from Beiträge zur Paläontologie und Geologie Österreich-Ungarns und des Orients, 1908, Vol. 21: Mitteilungen des Geologischen und Paläontologischen Institutes der Universität Wien
Nr. 7. An einem anderen Stücke durchsetzt das Bitumen das ganze Gestein.
Nr. 8. In die gleiche Abteilung gestellt wurde ein Gestein aus bläulichem Quarz, gelblich ver witterndem Kaolin und fein'schuppigem Muskovit.
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