Edge Rewrite
// HTMLRewriter · presentation

This page was redesigned at the edge.

Cloudflare fetched the original article and streamed it through HTMLRewriter to apply an entirely new visual system without rebuilding the source page.

// request.cf · coarse context

A page that knows where it met you.

Only coarse request metadata is shown. This demo does not display or persist visitor IP addresses.

Country
US
Cloudflare location
CMH
Connection
HTTP/2
Language
Not provided

Ray ID: a244b4f179ec2a83

Jump to content

Main Dolomite

From Wikipedia, the free encyclopedia
(Redirected from Main dolomite)
Main Dolomite
Hauptdolomit
Fődolomit
Dolomia Principale
Stratigraphic range: Carnian-Norian
Typical grey Main dolomite (Hauptdolomit) from rock quarry near Hradište pod Vrátnom, Slovakia
TypeGeological formation
Thickness0–2,200 m (0–7,218 ft)
Lithology
PrimaryDolomite
OtherLimestone
Location
RegionLimestone Alps & Apennines
Central Europe
CountryAustria
Germany
Hungary
Italy
Slovakia
Type section
Named for"Main Dolomite"
Named byGümbel
Year defined1857
Main dolomite of the Langbathscholle, Kaltenbachwildnis, Austria

Main Dolomite (German: Hauptdolomit, Hungarian: Fődolomit, Italian: Dolomia Principale) is a lithostratigraphic unit in the Alps of Europe. Formation was defined by K.W. Gümbel in 1857.

Middle to Late Triassic sedimentary record in the Alpine realm is characterized by presence of various masses of dolomitic rock formations. In the Northern Calcareous Alps the dolomitic mass of Ladinian - Norian age is divided by the Carnian sandstones and shales of Lunz Formation to the Ladinian - Carnian Wetterstein Dolomite and Norian Main Dolomite.[1] The Main Dolomite reaches higher thickness than underlying dolomites in Alps, therefore it is considered as more important "Main".

Extent

[edit]

The formation is found in:

Description

[edit]

It is primarily made of dolomite, ranging from 0 to 2,200 metres (0 to 7,218 ft) in thickness. Main Dolomite is represented by the medium bedded dolomitic layers often with characteristic stromatolitic lamination. The formation was deposited in shallow lagoons during the Late Carnian and Early Norian ages of the Late Triassic Epoch in the Triassic Period, during the Mesozoic Era.

Fossil content

[edit]

Fossil sauropodomorph tracks, likely made by a plateosaurid, have been reported from the formation.[2]

See also

[edit]

References

[edit]
  1. Tollmann, A., 1976: Analyse des klassischen nordalpinen Mesozoikums, Wien, Franz Deuticke, 580 pp.
  2. Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 517-607 ISBN 0-520-24209-2