Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Mathias H. Köster"'
Publikováno v:
Clay Minerals. 52:161-190
The Landshut bentonites that formed from Ca- and Mg-poor rhyolitic tuffs in a fluviatile-lacustrine depositional environment of the Miocene Upper Freshwater Molasse, southern Germany, contain abundant palustrine, pedogenic and groundwater carbonates.
Pedogenic, palustrine and groundwater dolomite formation in non-marine bentonites (Bavaria, Germany)
Autor:
Mathias H. Köster, H. A. Gilg
Publikováno v:
Clay Minerals. 50:163-183
Dolomite and calcite in Bavarian bentonites, southern Germany, were investigated using petrography, field-emission scanning electron microscopy and stable isotope geochemistry to explore the role of authigenic carbonate formation during bentonitizati
Autor:
H. Albert Gilg, Franz Neubauer, Friedrich Finger, Christoph Leitner, Sebastian Wiesmaier, Mathias H. Köster
Publikováno v:
GSA Bulletin.
The Permian Haselgebirge Formation of the eastern Alps is among the most highly deformed evaporites worldwide. In underground salt mines, it is composed of a melange of halite, anhydrite, and mudstone, with a subordinate amount of magmatic rocks. The
Publikováno v:
Scopus-Elsevier
The salt of the late Permian Haselgebirge Fm. exposes large proportions of mudrock. The mud was trapped in a basin without a connection to the open sea. The mudrock comprises earthquake structures. An enrichment of magnesium minerals (mainly magnesit