Towards a balanced 3D kinematic model of a faulted domain - The Bergheim open pit mine, Lower Rhine Basin

Geologie en Mijnbouw/Netherlands Journal of Geosciences

Volumn 81, Issue 2, 2002, Pages 241-250

  Thomsen, A ^a   Siehl, A ^a  

^a UNIVERSITY OF BONN   (Germany)

Author keywords

Balanced kinematic restoration; Bergheim lignite mine; Geological space time models; Object oriented database; Rouby's method

Indexed keywords

FAULTING; KINEMATICS; OPEN PIT MINE; SEDIMENTATION; TECTONIC EVOLUTION; THREE-DIMENSIONAL MODELING;

GERMANY; LOWER RHINE BASIN;

EID: 0036701696     PISSN: 00167746     EISSN: None     Source Type: Journal    
DOI: 10.1017/S0016774600022496     Document Type: Article

References (25)

1. Space-time modelling of the Lower Rhine Basin supported by an object-oriented database
2. From GeoStore to GeoToolKit: The second step
3. Extending geoToolKit to access distributed spatial data and operations
4. Spatial and temporal database support for geologists - An example from the lower Rhine basin
5. Recent movement pattern of the Lower Rhine Basin from tilt, gravity and GPS data
6. From palinspastic reconstruction to kinematic basin models
7. Kinematic subsidence modelling of the Lower Rhine Basin
8. Die rechnergestützte Modellierung eines 3D-Flächenverbandes der Erftscholle (Niederrheinische Bucht)
9. Die Geologie der Krefelder Scholle
10. GOCAD: A computer aided design program for geological applications
11. Das Krefelder Gewölbe in der Niederrheinischen Bucht - Teil einer großen Horizontalverschiebungszone?
12. A concept for time-dependent processes
13. Über pleistozäne Gebirgsbildung und rezente Krustenbewegungen in der Niederrheinischen Bucht
14. Displacements, strains, and rotations within the Afar depression (Djibouti) from restoration in map view
15. 3-D Restoration of complexly folded and faulted surfaces using multiple unfolding mechanisms
16. Cenozoic block rotation according to a conjugate shear system in Central Europe - Indications from palaeomagnetic measurements
17. Towards a balanced kinematic model of a faulted domain in the lower Rhine basin
18. Finite difference modelling of Hangingwall deformation
19. The relationship between the geometry of normal faults and that of the sedimentary layers in their Hanging walls