The calcareous stone of Muschelkalk Brown comes from a Franconian region in southern Germany
The Muschelkalk water infiltrated under conditions similar to those prevailing today.
Based on their carbonate isotope values, the calcites from open fractures and druses in the Muschelkalk are non-marine in character and are not in equilibrium with the Muschelkalk water as it occurs in Siblingen today.
In the middle, you see the calcareous shingle of the Muschelkalk, grey with very fine grain, and yellow shingle of the Jurassic.
The interpretation of data from the underlying aquifer groups (Dogger, Lias, Keuper; Muschelkalk; Buntsandstein-Permian-Crystalline) is still in progress.
They may have papular lesions on the outer edges [9], [10].
It offers pebbled, limestone-marl soils that are very uniform, shallow and rich in fossils, especially in the extreme western part, where the Muschelkalk (shell-limestone layer) is predominant.
Testing of the Muschelkalk at 74.95 to 117.85 m depth is discussed by Schmassmann (1985).
It offers pebbled, limestone-marl soils that are very uniform, shallow and rich in fossils, especially in the extreme western part, where the Muschelkalk (shell-limestone layer) is predominant.
It offers pebbled, limestone-marl soils that are very uniform, shallow and rich in fossils, especially in the extreme western part, where the Muschelkalk (shell-limestone layer) is predominant.
Isotope measurements on dissolved sulphate gave values which do not lie within the range for typical Muschelkalk sulphates.
It offers pebbled, limestone-marl soils that are very uniform, shallow and rich in fossils, especially in the extreme western part, where the Muschelkalk (shell-limestone layer) is predominant.
The hydrochemical modelling showed, compared with other Muschelkalk waters from Northern Switzerland, a marked undersaturation with respect to dolomite.
The Ca-Mg-SO4-(HCO3)-type water in the Muschelkalk and the Na-HCO3-Cl-(SO4)-type water in the Buntsandstein show a much lower degree of mineralisation.
Conversely, it was found that the Upper Muschelkalk formation below the Swiss Plateau is generally not suitable for hydrothermal electricity production.
Its soil consists of conglomerate limestone of the Muschelkalk (Triassic shell limestone -230Ma) and Jurassic limestone (from -130Ma to -200 Ma) imbedded with sandstone marl.
The Lower Muschelkalk consists mainly of an approximately 34 m thick sequence of dark grey to black claystones with thin sandstone beds and small isolated carbonate banks.
The upper section of the borehole down to the base of the Malm limestones and the Upper and Middle Muschelkalk were drilled using a clay-freshwater drilling fluid.
Towards the Schnekelsbourg, one finds muschelkalk at depth providing better hydration and minerals in an area which suffers greatly from its poor soil.
Muschelkalk and Zechstein salts release chloride ions into the deep rockwater in a natural process that forms mineralised waters.
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