10th IAS Regional Meeting on Sedimentology
[Abstracts]
Földtudományok, földrajz
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Geológia, földtörténet
"The stratiform bauxite deposit of the Halimba basin in the Transdanubian Central Range, is situated on the slightly karstified surface of the Upper Triassic dolostones and limestones, and is covered by Senonian and/or Eocene beds. The formation of this deposit was in close connection with sedimentation during the Senonian and Eocene cycles."
2020-03-26
Megtekinthető verziók
PDF URL: https://mek.oszk.hu/20200/20226 URN: http://nbn.urn.hu/N2L?urn:nbn:hu-157684Látogatások: 2 617