Madrid, España
The structural charasteristics of fibrous vein of gypsum are described. Two types appears in this area: a syntaxial veins with parabolically-shaped, and other in 'double antitaxial perharps new model that it is proposed, with sigmoid-shape.
Both indicate a reverse, overthrust-like relative movement. The geometry afld distribution of the structures indicate that events it is kept pace with a flexural-slip folds, during sorne phase post-0ligocene.
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