An exceptional rocky shore preserved during Oligocene (Late Rupelian) transgression in the Upper Rhine Graben (Mainz Basin, Germany)

@article{Rouss2012AnER,
  title={An exceptional rocky shore preserved during Oligocene (Late Rupelian) transgression in the Upper Rhine Graben (Mainz Basin, Germany)},
  author={St{\'e}phane Rouss{\'e} and Philippe Duringer and Karl Georg Stapf},
  journal={Geological Journal},
  year={2012},
  volume={47}
}
The Early Oligocene (Late Rupelian) Alzey Formation (Mainz Basin, Upper Rhine Graben, Germany) records the development of a rocky coast depositional system during transgression. The formation unconformably overlies Permian bedrock across a composite transgressive ravinement surface. Exposure of the surface shows a succession of subplanar bedrock terraces, separated by near‐vertical risers. Terraces show a broad staircase geometry and display wave‐erosional features (notches, sea stacks, furrows… 

Transgressive Eocene clastic–carbonate sediments from the Circum‐Rhodope belt, northeastern Greece: implications for a rocky shore palaeoenvironment

Locally exposed Middle to Upper Eocene conglomerates in the western part of the Cenozoic Thrace Basin are interpreted as products of continuous marine erosion of a rocky coast (consisting of Lower

The complete lithostratigraphic section of the geothermal wells in Rittershoffen (Upper Rhine Graben, eastern France): a key for future geothermal wells

Between 2012 and 2014, in Rittershoffen, in the Upper Rhine Graben, two geothermal boreholes (GRT-1 and GRT-2) reached the granitic basement at a depth of around 2150 m. The wells crossed about 1160

Assessment of deep geothermal research and development in the Upper Rhine Graben

Deep geothermal energy represents a key element of future renewable energy production due to its base load capability and the almost inexhaustible resource base. Especially with regard to heat

Evidence for Two sympatric sirenian species (Mammalia, Tethytheria) in the early Oligocene of Central Europe

Abstract. The early Oligocene (Rupelian) sirenian Halitherium schinzii Kaup, 1838, which represents the type species of the genus Halitherium Kaup, 1838, is revised herein based on a morphological

Revision of the Halitherium-species complex (Mammalia, Sirenia) from the late Eocene to early Miocene of Central Europe and North America

The genus Halitherium includes a number of fossil sirenian species, or sea cows, ranging from the late Eocene to early Miocene, and is paraphyletic comprising mainly genera that are invariably paraphYletic as well.

References

SHOWING 1-10 OF 86 REFERENCES

Uplifted Marine Terraces Along the Alpine Fault, New Zealand

Three types of evidence indicate that marine terraces are widespread in the Southern Alps of New Zealand. (i) Remnants of shore platforms occur as distinct levels of notched ridge crests and flat

Obliquity‐dominated glacio‐eustatic sea level change in the early Oligocene: evidence from the shallow marine siliciclastic Rupelian stratotype (Boom Formation, Belgium)

Our results prove that glacio‐eustatic sea level oscillations in the early Oligocene were dominantly obliquity controlled with additional influence of the ∼100‐ and 405‐kyr eccentricity cycles. This

The Calcarenite di Gravina Formation in Matera (Southern Italy): New Insights for Coarse-Grained, Large-Scale, Cross-Bedded Bodies Encased in Offshore Deposits

Excellent outcrops of the upper Pliocene-lower Pleistocene Calcarenite di Gravina around Matera (southern Italy) provide continuous exposure of coarse-grained, clastic basin-margin, shoreline to

Coarse-grained storm beds of the Upper Cretaceous Chungo Member (Wapiabi Formation), southern Alberta, Canada

The Upper Cretaceous Chungo Member of the Wapiabi Formation at Mount Yamnuska, Alberta is composed of three cycles: two coarsening-upward progradational successions overlain by a fining-upward

Rocky shore-gravelly beach transition, and storm/post-storm changes of a holocene gravelly beach (Kos island, Aegean sea): Stratigraphic significance

SummaryOn Kos island, Greece, along an investigated coastal segment 3 km in length, four adjacent sectors were distinguished, (1) Empros beach, a rocky shore with plunging cliffs and a steeply

The northern Upper Rhine Graben: basin geometry and early syn-rift tectono-sedimentary evolution

A large-scale transfer zone subdivides the northern parts of the Upper Rhine Graben into a northern and a southern sub-basin. These sub-basins display the geometry of asymmetric half-grabens with
...