Crustal structure of the Rhenish Massif: results of deep seismic reflection lines Dekorp 2-North and 2-North-Q
- 1 October 1990
- journal article
- research article
- Published by Springer Nature in International Journal of Earth Sciences
- Vol. 79 (3) , 523-566
- https://doi.org/10.1007/bf01879201
Abstract
No abstract availableKeywords
This publication has 49 references indexed in Scilit:
- Variscan plate tectonics in Central Europe—current ideas and open questionsPublished by Elsevier ,2003
- Tectonics and plate tectonics model for the Variscan belt of EuropePublished by Elsevier ,2003
- The Variscan Belt in Central Europe: Main structures, geodynamic implications, open questionsPublished by Elsevier ,2003
- The conrad discontinuity and the top of the reflective lower crust—do they coincide?Tectonophysics, 1989
- Anisotropy of Vp and Vs in an amphibolite of the deeper crust and its relationship to the mineralogical, microstructural and textural characteristics of the rockTectonophysics, 1989
- Seismic anisotropy in mylonites: an example from the Mannin Thrust Zone, southwest Connemara, IrelandTectonophysics, 1988
- Geological interpretation of DEKORP 2-S: A deep seismic reflection profile across the Saxothuringian and possible implications for the Late Variscan structural evolution of Central EuropeTectonophysics, 1987
- A three-dimensional crustal model of southwest Germany derived from seismic refraction dataTectonophysics, 1987
- Crustal evolution of the Rhinegraben area. 1. Exploring the lower crust in the Rhinegraben rift by unified geophysical experimentsTectonophysics, 1987
- Rifts at high angles to orogenic belts; tests for their origin and the Upper Rhine Graben as an exampleAmerican Journal of Science, 1978