Laminated veins and hydrothermal breccia as markers of low-angle faulting, Rhenish Massif, Germany
- 1 August 1992
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 208 (4) , 413-430
- https://doi.org/10.1016/0040-1951(92)90438-c
Abstract
No abstract availableKeywords
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