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Meisenheim Formation

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SW–NE section documenting the complex architecture of the <b>Meisenheim</b> <b>Format</b>...
Published: 01 September 2002
Figure 3. SW–NE section documenting the complex architecture of the Meisenheim Formation and the lithostratigraphic positions of the major tuff horizons along the SE-flank of the Pfalz Anticline (for location see Fig. 1b ). Rapid lateral thickness changes of the sequence occur across
Journal Article
Published: 01 September 2002
Geological Magazine (2002) 139 (5): 541–558.
...Figure 3. SW–NE section documenting the complex architecture of the Meisenheim Formation and the lithostratigraphic positions of the major tuff horizons along the SE-flank of the Pfalz Anticline (for location see Fig. 1b ). Rapid lateral thickness changes of the sequence occur across...
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Journal Article
Published: 01 September 2020
Journal of Paleontology (2020) 94 (5): 819–828.
...Xin-fa Li; Guo-biao Li; Christopher L. Garvie; Tian-yang Wang; Jun Zhao Abstract During recent stratigraphical and micropaleontological investigations of the Gulupu section in Tüna, Yadong, of the Eocene Zhepure Formation, numerous holoplanktonic mollusks (pteropods) were recovered. Four species...
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Generalized Stephanian and ‘Rotliegend’ stratigraphy of the Saar–Nahe Basin...
Published: 01 September 2002
Figure 2. Generalized Stephanian and ‘Rotliegend’ stratigraphy of the Saar–Nahe Basin illustrating the stratigraphic positions of the studied section and important tephrostratigraphic marker horizons of the Meisenheim Formation. The question marks indicate the uncertain position
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Classification of tuff samples in the slightly modified Nb–Zr diagram of  L...
Published: 01 September 2002
Figure 4. Classification of tuff samples in the slightly modified Nb–Zr diagram of Leat et al. (1986) and legend of the examined tephrostratigraphic markers of the Meisenheim Formation. Dashed line divides an area of samples predominantly of the Jeckenbach Subformation (open symbols) from
Image
Location of the Saar–Nahe Basin (SNB) within (a) the palaeogeography at the...
Published: 01 September 2002
Figure 8. Location of the Saar–Nahe Basin (SNB) within (a) the palaeogeography at the Carboniferous/Permian boundary (modified from Scotese & Langford, 1995 ) and (b) the recent geological framework of Central Europe showing the distances of the studied tuff horizons of the Meisenheim
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1944
AAPG Bulletin (1944) 28 (10): 1528–1533.
... and the Mountain Glen formations in the Darty Creek section in Union County, Illinois. This is the same unconformity as the one between the New Albany black shale and the lop of the Devonian limestone in Marion County, Illinois. In the Sandoval pool the formation immediately below the Meisenheimer...
FIGURES
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2004
DOI: 10.1144/GSL.SP.2004.234.01.07
EISBN: 9781862394827
.... Lithostratigraphic sequence of continental sediments, major tephra horizons, and major lava flows of the Donnersberg-Formation in the Nahe-Subgroup of the Rotliegend. The Nahe-Subgroup represents the former Upper Rotliegend in the Saar-Nahe Basin. Maar-diatreme volcanoes form when rising magma interacts...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.181.01.02
EISBN: 9781862394292
... Abstract Comparative studies are made on the development of lamination in Recent, Paleogene and Permian lake sediments. The study concentrates on the relationship between primary production and lamina formation. The main phytoplankton development in lakes is correlated with environmental...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.179.01.15
EISBN: 9781862394278
... a quantitative interpretation of the reconstructed thermal history, resulting from fundamental orogenic processes such as basin formation, uplift and erosion, and magmatism. In particular, information was obtained on the heat flow evolution and the amount of erosion related to the Variscan Orogeny. Figure 1...
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Journal Article
Published: 01 September 2016
Journal of Paleontology (2016) 90 (5): 785–814.
...Arden R. Bashforth; William A. DiMichele; Cortland F. Eble; W. John Nelson Abstract A macrofloral assemblage dominated by elements of the Euramerican dryland biome is described from the Brazil Formation in Clay County, Indiana (Illinois Basin). Fossils were recovered from a thin heterolithic unit...
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Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2012
DOI: 10.1306/13291397M953495
EISBN: 9781629810096
... of almost 8 km (5 mi) today was calculated by means of the well sections Saar 1, Wemmetsweiler-Nord 1, Meisenheim 1, and Olm 1, following the stratigraphic record from bottom to top (used for the setup of Figures 3 , 4 ). 10 km (6.2 mi). Paper shales are abundant in the Breitenbach Formation...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2010
DOI: 10.1144/SP339.12
EISBN: 9781862395879
... and Early Permian ( Poplin 1994 ; Fluteau 2003 ; Roscher & Schneider 2006 ), the studied branchiosaurid samples represent populations that inhabited the same large-scale climatic zone. These populations fall in three different time slices (L-O-6, L-O-7, L-O-8 of Meisenheim Formation) that might have...
FIGURES
Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP450.6
EISBN: 9781786203311
... Oberhof – after Martens (1983 a , fig. 25), Lochbrunnen near Oberhof village, Lower Oberhof Fomation, Sakmarian–Artinskian, Thuringian Forest Basin; ( 23 ) Palaeolimnadiopsis obenaueri – after Martens (1984 , fig. 3 ), Meisenheim Formation, Humberg bank (Lebach geods), Artinskian, Saar–Nahe Basin...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.265.01.09
EISBN: 9781862395138
... and La Queue d’Etang, Bourbon l’Archambault Basin, French Massif Central; Beds of Bert (Autunian or Lower Rotliegend, Sakmarian) from Bert, Blanzy Basin, French Massif Central; Uppermost Meisenheim Formation (L-0 10, Lower Rotliegend, Sakmarian) from Humberg, Wörsbach or Lebach, Saar–Nahe...
FIGURES
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.265.01.15
EISBN: 9781862395138
..., as in the still blattid-rich and very diverse insect faunas of the Salagou Formation of the Lodeve Basin, southern France, and the playa lake deposits of the Wellington Formation of Kansas and Oklahoma. Obviously, spiloblattinids occur in a wide range of biotopes from humid to semi-arid conditions. They seem...
FIGURES
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.265.01.05
EISBN: 9781862395138
... of about 3300 km 2 . Within the overlying Meisenheim Formation, approximately 40 tuff horizons occur in grey-brown to grey sandstones with sporadic regional coal seams. The fluvio-lacustrine middle part, with black shales and red sandstones, grade upward to lacustrine grey-brown to grey fine sandstones...
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Journal Article
Published: 01 April 2014
Bulletin de la Société Géologique de France (2014) 185 (4): 233–252.
... Mansfeld, ces poissons sont entourés de lycopodolites. Les poissons de Münster Appel, dans le Palatinat, de même que ceux du Mont Tonnère, se trouvent en rognons dans la partie supérieure du terrain houiller (grès rouge). Comme les poissons de Goldlauter prouvent la liaison qui existe entre deux formations...
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Journal Article
Published: 01 August 1999
Journal of the Geological Society (1999) 156 (4): 801–808.
... SE-trending strike- slip faults which are interpreted to represent transfer faults sensu Gibbs (1990). Since the W E extensional stress regime that dominated during the post-Westphalian basin formation (Henk 1993; Stollhofen 1998) was oblique to the pre-existing fault pattern, the common slip...
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1956
AAPG Bulletin (1956) 40 (7): 1543–1581.
... stratigraphic tests were drilled under the supervision of the Service Geologique de Belgique. The Turnhout well, mentioned in previous reports on European developments, drilled on the north flank of the Brabant Massif, was cored continuously below 649 meters. The following formations were logged...
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