The Sarmatian/Pannonian boundary at the western margin of the Vienna Basin (City of Vienna, Austria)-Reference-Cited by-同舟云学术

The Sarmatian/Pannonian boundary at the western margin of the Vienna Basin (City of Vienna, Austria)

Published:2018-09-01 Issue:1 Volume:111 Page:26-A4
ISSN:2072-7151
Container-title:Austrian Journal of Earth Sciences
language:en
Short-container-title:

Author:

Harzhauser Mathias¹,Mandic Oleg¹,Kranner Matthias²,Lukeneder Petra²,Kern Andrea K.³,Gross Martin⁴,Carnevale Giorgio⁵,Jawecki Christine⁶

Affiliation:

1. Geological-Paleontological Department, Natural History Museum, Vienna, Burgring 7, Vienna , Austria

2. Geological-Paleontological Department, Natural History Museum, Vienna, Burgring 7, 1010 Vienna , Austria

3. Department of Sedimentary and Environmental Geology, University of Sao Paulo, Rua do Lago 562, Sao Paulo , Brazil

4. Universalmuseum Joanneum, Department for Geology & Palaeontology, Weinzöttlstraße 16, 8045 Graz , Austria

5. Universita degli Studi di Torino, Dipartimento di Scienze della Terra, Via Valperga Caluso, 35, Torino , Italy

6. Magistratsabteilung 29, Brückenbau und Grundbau, Wilhelminenstraße 93, Vienna , Austria

Abstract

Abstract 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 environments during the middle to late Miocene transition. Two Sarmatian and two Pannonian transgressive-regressive sequences were studied in detail. Identical successions of benthic faunal assemblages and similar patterns in magnetic susceptibility logs characterise these sequences. This allows a correlation of the boreholes over a distance of ~3.5 km across one of the major marginal faults of the Vienna Basin. Biostratigraphic data, combined with rough estimates of sedimentation rates, reveal large gaps between these sequences, suggesting that only major transgressions reached this marginal area. In particular, during the Sarmatian-Pannonian transition, the basin margin completely emerged and turned into a terrestrial setting for at least 600 ka.

Publisher

Austrian Geological Society (OGG)

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