The Cenozoic Lower Rhine Basin–rifting, sedimentation, and cyclic stratigraphy
T Utescher, M Klett, M Valdivia-Manchego - International Journal of Earth …, 2005 - Springer
Abstract In the Cenozoic, the Lower Rhine Basin formed as a rift at the southeastern
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …
[PDF][PDF] The Cenozoic Lower Rhine Basin–rifting, sedimentation, and cyclic stratigraphy
A Schafer, T Utescher, M Klett… - Int J Earth Sci (Geol …, 2005 - researchgate.net
Abstract In the Cenozoic, the Lower Rhine Basin formed as a rift at the southeastern
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …
[PDF][PDF] The Cenozoic Lower Rhine basin: rifting, sedimentation, and cyclic
A Schäfer - International journal of earth sciences, 2005 - doc.rero.ch
Abstract In the Cenozoic, the Lower Rhine Basin formed as a rift at the southeastern
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …
The Cenozoic Lower Rhine Basin–rifting, sedimentation, and cyclic stratigraphy
A Schäfer, T Utescher, M Klett… - International Journal of …, 2005 - infona.pl
In the Cenozoic, the Lower Rhine Basin formed as a rift at the southeastern terminus of the
Dutch German Central Graben, while the Rhenish Massif was uplifted. The study focusses …
Dutch German Central Graben, while the Rhenish Massif was uplifted. The study focusses …
The Cenozoic Lower Rhine Basin rifting, sedimentation, and cyclic stratigraphy
A Schäfer, T Utescher, M Klett… - … Journal of Earth …, 2005 - ui.adsabs.harvard.edu
Abstract In the Cenozoic, the Lower Rhine Basin formed as a rift at the southeastern
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …
[PDF][PDF] The Cenozoic Lower Rhine Basin–rifting, sedimentation, and cyclic stratigraphy
A Schafer, T Utescher, M Klett… - Int J Earth Sci (Geol …, 2005 - academia.edu
Abstract In the Cenozoic, the Lower Rhine Basin formed as a rift at the southeastern
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …
The Cenozoic Lower Rhine Basin-rifting, sedimentation, and cyclic stratigraphy
A Schäfer, T Utescher, M Klett… - … Journal of Earth …, 2005 - search.proquest.com
Abstract In the Cenozoic, the Lower Rhine Basin formed as a rift at the southeastern
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …
[PDF][PDF] The Cenozoic Lower Rhine Basin–rifting, sedimentation, and cyclic stratigraphy
A Schafer, T Utescher, M Klett… - Int J Earth Sci (Geol …, 2005 - academia.edu
Abstract In the Cenozoic, the Lower Rhine Basin formed as a rift at the southeastern
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …
terminus of the Dutch German Central Graben, while the Rhenish Massif was uplifted. The …