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- W2612594316 abstract "In the Alpine-Carpathian Foredeep and the Vienna Basin inAustria deposits of the Hollabrun-Mistelbach Foration of theupper Miocene have been studied in 65 outcrops between Kremsund Zistersdorf. Two genetically related depositionalenvironment were recognised. The depositional environment of agravel-bed river is dominant in the majority of the outcrops.Towards the east this sytem developed into a braid-deltaenvironment. Larger scale architectural elements recognisedwithin the gravel-bed river deposits are gravelly chennelfills, sandy channel fills and overbank deposits. The studieddeposits of the braid-delta represent the proximal part of thedelta and can be subdivided into deposits of distributarychannels, mouth bars, gravelly beaches, foreshore and shorefacedeposits and interdistributary areas." @default.
- W2612594316 created "2017-05-19" @default.
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- W2612594316 date "2004-01-01" @default.
- W2612594316 modified "2023-09-23" @default.
- W2612594316 title "The Hollabrunn-Mistelbach Formation (Upper Miocene, Pannonian)in the Alpine-Carpathian Foredeep and the Vienna Basin in theLower Austria - An example of a Coarse-grained Fluvial System" @default.
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