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Eggerding Formation

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Journal Article
Journal: Palynology
Published: 02 October 2019
Palynology (2019) 43 (4): 660–668.
...Ali Soliman; Hamid Slimani Abstract The organic-walled dinoflagellate cyst Molassedinium bicornutum gen. et sp. nov. described in this paper is recorded in the Oligocene (Rupelian) organic-rich sediments of the Eggerding Formation from the North Alpine Foreland Basin (Molasse Basin), Austria...
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Isopach maps of ( a ) Schöneck <b>Formation</b>, ( b ) Dynow Marlstone and ( c ) ...
Published: 01 November 2006
Fig. 12 Isopach maps of ( a ) Schöneck Formation, ( b ) Dynow Marlstone and ( c ) Eggerding Formation. Maps were constructed using a “simple Kriging” approach. The fault pattern is shown according to Wagner (1998) .
Journal Article
Journal: Palynology
Published: 03 April 2019
Palynology (2019) 43 (2): 268–291.
... and Phthanoperidinium comatum ) and early Rupelian or older (occurrence of Lentinia serrata ) for another, establishing time equivalence with the Upper Eocene–Oligocene Dabaa Formation. The palynological assemblages reflect fluctuating conditions on the southern margin of the Tethys/Paratethys Ocean, with the frequent...
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W–E-trending seismic sections showing erosional features near the top of th...
Published: 01 November 2006
Fig. 14 W–E-trending seismic sections showing erosional features near the top of the Eggerding Formation ( a ), ( b ). Vertical axis is in two-way travel time (TWT). ( c ) Sonic log and synthetic seismogram of the Radhof 1 well provide a tie between log data and seismic data.
Journal Article
Published: 01 November 2006
Petroleum Geoscience (2006) 12 (4): 363–377.
...Fig. 12 Isopach maps of ( a ) Schöneck Formation, ( b ) Dynow Marlstone and ( c ) Eggerding Formation. Maps were constructed using a “simple Kriging” approach. The fault pattern is shown according to Wagner (1998) . ...
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S–N-trending profiles. The profiles show the wide lateral continuity of Low...
Published: 01 November 2006
exhibit a different facies. Note also the highly structured logs of the Eggerding Formation in some wells (Oberhofen 1, Grünau 1, Steinfelden 1), which might be due to re-deposited material from the upper slope. Parts of the Lower Oligocene section in the Steindlberg 2 and Steinfelden 1 wells are missing
Journal Article
Journal: AAPG Bulletin
Published: 01 March 2017
AAPG Bulletin (2017) 101 (3): 289–319.
... (Solenovian event). Anoxic conditions prevailed and were only interrupted for longer periods during deposition of the lower part of the lower Oligocene Pshekha Formation, the Polbian Bed, and the lower Miocene Olginskaya Formation. Total organic carbon (TOC) contents range up to 3.5 wt. %. Hydrogen index...
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Typical logs for wells from different bathymetric settings within the Molas...
Published: 01 November 2006
Fig. 7 Typical logs for wells from different bathymetric settings within the Molasse Basin (cf. Fig. 5 ): ( a ) proximal position (Eggerding 2); ( b ) upper slope (Perneck 1); ( c ) lower slope (Oberhofen 1); ( d ) basin floor (allochthonous part of Oberhofen 1). Only the lower part
Journal Article
Journal: AAPG Bulletin
Published: 01 February 2014
AAPG Bulletin (2014) 98 (2): 253–277.
..., and Eggerding Formations are considered to be the source rocks ( Schulz et al., 2002 ; Sachsenhofer et al., 2010 ). Because of scaling problems caused by limited thicknesses of these layers, the three formations are merged to one source rock interval ( Table 1 ). The entire interval has a net thickness...
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Journal Article
Journal: AAPG Bulletin
Published: 01 June 2017
AAPG Bulletin (2017) 101 (6): 789–806.
... and Sachsenhofer, 2011 ). The correlated source rocks for the thermogenic gas (and oil) are the lower Oligocene (Kiscellian) shales of the Schöneck Formation (Fish Shale) and banded marls of the Eggerding Formation ( Schulz et al., 2002 ; Sachsenhofer and Schulz, 2006 ; Sachsenhofer et al., 2010 ; Gratzer et al...
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Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP464.1
EISBN: 9781786203724
... of the Paratethys, worsened the environment for calcareous nannoplankton ( Schulz et al. 2005 ). Oxygen-deficient conditions continued during deposition of the Eggerding Formation (NP23–NP24), typically about 45 m thick. Salinity variations are recorded in the lower part of the formation, consisting of dark...
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Journal Article
Journal: Interpretation
Published: 30 May 2017
Interpretation (2017) 5 (3): T387–T398.
... H. G. Bechtel A. , 2010 , Deposition, erosion and hydrocarbon source potential of the Oligocene Eggerding Formation (Molasse basin, Austria) : Austrian Journal of Earth Sciences , 103 , 76 – 99 , doi: http://dx.doi.org/10.1016/j.marpetgeo.2015.08.034 . Schmoker J. W. , 1979...
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Journal Article
Journal: Geophysics
Published: 08 October 2013
Geophysics (2013) 78 (6): D445–D459.
... A. , 2010 , Deposition, erosion and hydrocarbon source potential of the Oligocene Eggerding Formation (Molasse Basin, Austria) : Austrian Journal of Earth Sciences , 103 , 76–99 . Vernik L. Milovac J. , 2011 , Rock physics of organic shales : The Leading Edge , 30 , 318–323 , doi...
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Journal Article
Journal: AAPG Bulletin
Published: 01 October 2013
AAPG Bulletin (2013) 97 (10): 1805–1831.
... biogenic gas system ( Malzer et al., 1993 ; Wagner, 1996, 1998 ). The lower Oligocene Schöneck, Dynow, and Eggerding Formations ( Figure 2 ) all have source rock potential ( Schulz et al., 2002 ; Sachsenhofer and Schulz, 2006 ). The oil kitchen is assumed to be located underneath the Alpine nappes...
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Series: Geological Society, London, Special Publications
Published: 01 January 2018
DOI: 10.1144/SP468.1
EISBN: 9781786203687
... exchange reactions in geological settings, for example, (a) mechanisms and rates of 2 H/ 1 H exchange, and (b) equilibrium 2 H/ 1 H fractionation. In the Alpine foreland basin, a variety of Oligocene source rocks in the Schöneck, Dynow and Eggerding formations, with shaly to marly lithologies...
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