Interaction of basin-margin faults and tidal currents on nearshore sedimentary architecture and composition: a case study from the Early Miocene of northern Hungary

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• 作者：Sztan&oacute ; O. ; J&oacute ; zsa ; S.
• 关键词：conglomerate ; tidal currents ; fault-controlled delta ; pebble composition
• 刊名：Tectonophysics
• 出版年：1996
• 出版时间：December 15, 1996
• 年：1996
• 卷：266
• 期：1-4
• 页码：319-341
• 全文大小：1.73 M

文摘

The Darnó Conglomerate and the Pétervására Sandstone with conglomeratic intercalations, both cropping out in northern Hungary, were formed along the eastern margin of the shallow Early Miocene sea within the Carpathian arc. Ophiolite-derived clastic components in both formations indicate a close genetic relationship with each other and with the activity of the basin-margin Darnó Fault, which seems to correspond with the coeval shoreline.