Iron porphyrins in the Permian Kupferschiefer of the lower Rhine Basin, N.W. Germany

1989 ◽  
Vol 14 (6) ◽  
pp. 659-666 ◽  
Author(s):  
C.B. Eckardt ◽  
M. Wolf ◽  
J.R. Maxwell
Keyword(s):  
Iron Porphyrins ◽  
Rhine Basin ◽  
Lower Rhine Basin ◽  
Lower Rhine

Anatomy of a channel-bank collapse structure in Tertiary fluvio-lacustrine sediments of the Lower Rhine Basin, Germany

1990 ◽  
Vol 127 (5) ◽  
pp. 445-451 ◽  
Author(s):  
H. Williams ◽  
S. Flint
Keyword(s):  
Coastal Plain ◽  
Lacustrine Sediments ◽  
General Application ◽  
Rhine Basin ◽  
Deformation Feature ◽  
Multi Stage ◽  
Failure Event ◽  
Lower Rhine Basin ◽  
Bank Collapse ◽  
Lower Rhine

AbstractAn exceptionally well-preserved synsedimentary deformation feature is described from uppermost Miocene fluvio-lacustrine coastal plain sediments, exposed in lignite mines of the Lower Rhine Basin, Germany. The feature is interpreted as a complex, multi-stage channel-bank collapse structure. Rotational slumping of bank material into the channel along two failure surfaces extending below the channel toe generated a series ofminor compressional ‘thrust/backthrust’ structures within the muddy channel-fill sediments. A reconstruction of the failure event is proposed which is linked toa lowering of river stage and subsequent channel abandonment. The accurate description of this unusually well-preserved channel-bank collapse structure may have general application in the interpretation of similar, but less-well-exposed-preserved phenomena elsewhere.

Miocene depositional environment and climate in western Europe: The lignite deposits of the Lower Rhine Basin, Germany

2016 ◽  
Vol 157 ◽  
pp. 2-18 ◽  
Author(s):  
Alexander T. Stock ◽  
Ralf Littke ◽  
Andreas Lücke ◽  
Laura Zieger ◽  
Thomas Thielemann
Keyword(s):  
Western Europe ◽  
Depositional Environment ◽  
Rhine Basin ◽  
Lower Rhine Basin ◽  
Lignite Deposits ◽  
Lower Rhine

scholarly journals New subsurface temperature maps for the Tertiary Lower Rhine Basin and the adjacent Variscan Basement - Germany, The Netherlands, Belgium

2004 ◽  
Vol 83 (2) ◽  
pp. 135-146 ◽  
Author(s):  
H. Karg ◽  
C. Bücker ◽  
R. Schellschmidt
Keyword(s):  
Temperature Field ◽  
Coal Mine ◽  
Temperature Data ◽  
Depth Interval ◽  
Subsurface Temperature ◽  
Rhine Basin ◽  
Lower Rhine Basin ◽  
Temperature Maps ◽  
Variscan Basement ◽  
Lower Rhine

AbstractThe regional subsurface temperature field at the transition between the Palaeozoic Variscan Basement and the Cenozoic Lower Rhine Basin in Dutch, German and Belgium territories was mapped up to a depth of 1000 m. Temperature data from 66 wells and 11 coal mine subcrops were available. In 46 wells, temperature logs, covering a cumulative depth interval of 6600 m, were measured for this study.

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