Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Matthias Piecha"'
Autor:
Karl-Heinz Ribbert, Matthias Piecha
Publikováno v:
Palaeobiodiversity and Palaeoenvironments. 102:557-572
Autor:
Manfred Gereke, Matthias Piecha
Publikováno v:
PalZ.
Autor:
Vincent Casanova, Lluis Fontboté, Kalin Kouzmanov, Nicolas Saintilan, Adam D. Sproson, James J. Zambito, Bertrand Rottier, Robert A. Creaser, David Selby, Manfred Gereke, Matthias Piecha
Publikováno v:
Chemical Geology, Vol. 564, No 120053 (2021)
Chemical Geology, 564
Chemical geology, 2021, Vol.564, pp.120053 [Peer Reviewed Journal]
Chemical Geology, 564
Chemical geology, 2021, Vol.564, pp.120053 [Peer Reviewed Journal]
In the magmatic-hydrothermal environment, fluids with similar metal concentrations and sources may yield contrasting mineral assemblages in successive stages of sulphide mineralization. These differences are linked to the physico-chemical conditions
Autor:
Eberhard Schindler, Matthias Piecha, Friedrich Wilhelm Luppold, Dieter Stoppel, Manfred Gereke
Publikováno v:
Zeitschrift der Deutschen Gesellschaft für Geowissenschaften. 165:145-162
Autor:
Matthias Piecha, Karl-Heinz Ribbert
Publikováno v:
Palaeobiodiversity and Palaeoenvironments. 94:411-423
During the Frasnian the carbonate platform of the Rhenish Massenkalk reef development was affected by (1) the decline of the stromatoporoid—coral community during the rhenana conodont zone and its replacement by a crinoid-brachiopod-calcimicrobiali
Autor:
Bettina Dölling, Matthias Piecha
Publikováno v:
Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften. 73:45-52
Publikováno v:
Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins. 90:149-185
Autor:
Matthias Piecha
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 181:195-211
The Frasnian/Famennian (F/F) boundary interval on the Rhenish shelf carbonate platform of northwestern Germany is characterized by a remarkable stratigraphic gap in two reference sections, which was caused by a rapid regression phase leading to the o
Publikováno v:
Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften. 66:66-67