The studied sections are situated on the northwestern margin of the Vienna Basin. They
represent a characteristic marginal facies of Lake Pannon in the late Miocene Pannonian …

Late Miocene sedimentary environments were related to the shallow brackish-to fresh-water
lake in the Slovak part of the Vienna Basin. During the Pannonian time, the geological …

There is a successive change in the Lower to Middle Miocene stratigraphy, from terrestrial-
fluviatile sedimentation, with a lower alluvial fan/braided river facies and an upper …

In order to determine the relative contributions of tectonics and eustasy to the sedimentary
infill of the Vienna Basin a high-resolution stratigraphic record of a Middle to Late Miocene …

With the beginning of the Late Pannonian, the long-lived Lake Pannon retreated from the
Vienna Basin. A fluvial system, which already developed during the Early Pannonian in the …

A continuous succession of Ottnangian-Badenian sediments along the southern margin of
the Pannonian Basin System indicates transition from lacustrine to marine depositional …

Sarmatian and Pannonian cores, drilled at the western margin of the Vienna Basin in the
City of Vienna, reveal a complex succession of marine and lacustrine depositional …

A multidisciplinary study was performed on a c. 30m thick, limnic–deltaic sequence in the
Styrian Basin (Austria). Geophysical (gamma ray activity, rock magnetism), geochemical …

The paleogeographic evolution of Lake Pannon within the Pannonian basin is reconstructed
with eight maps, ranging from the Middle Miocene to the Early Pliocene. The maps are …

Abstract The Vienna Basin, depositional systems of alluvial plains, deltas, littoral and neritic
areas have been characterized to recognize the development of aquatic and terrestrial …