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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Detalles Bibliográficos

Autores principales:	Canals Sabaté, Angels, Fletcher, R.C., Merino Muedra, Enrique
Formato:	Artículo
Lenguaje:	inglés
Publicado:	Institut de Ciències de la Terra "Jaume Almera" 2006
Materias:	Rhythmite Zebra texture Breccia texture Displacive Veins Induced stress Self-organization Burial dolomitization
Acceso en línea:	https://dialnet.unirioja.es/servlet/oaiart?codigo=2052965
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