Genesis of self-organized zebra textures in burial dolomites: Displacive veins, induced stress, and dolomitization

Genesis of self-organized zebra textures in burial dolomites: Displacive veins, induced stress, and dolomitization

The dolomite veins making up rhythmites common in burial dolomites are not cement infillings of supposed cavities, as in the prevailing view, but are instead displacive veins, veins that pushed aside the host dolostone as they grew. Evidence that the veins are displacive includes a) small transform-...

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Bibliographic Details
Main Authors: E. MERINO, À. CANALS I SABATÉ, R. C. FLETCHER
Format: Article
Language:English
Published: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2006-01-01
Series:Geologica Acta
Subjects:
Rhythmite
Zebra texture
Breccia texture
Displacive veins
Induced stress
Self-organitzations
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/1883

Internet

https://revistes.ub.edu/index.php/GEOACTA/article/view/1883

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