@article{10272/9705,
year = {2001},
url = {http://hdl.handle.net/10272/9705},
abstract = {Microstructural surveying of pebbles of the early Cambrian «Anguiano Conglomerates» permits to recognize a variety of microstructures and textures that resulted from syn-metamorphic (up to 400°C, low-temperature greenschists facies) ductile deformations. The source area of the conglomerates was likely a Neoproterozoic basement that recorded the imprint of the Cadomian orogeny and that contained penetratively deformed metamorphic rocks in addition to the arc-related ingeous suites that have been detected or inferred so far in other realms of the northern Iberian Massif},
publisher = {Sociedad Española de Geología},
title = {Nuevos datos microestructu rales sobre la existencia de deformaciones precámbricas en la Sierra de la Demanda (Cordillera Ibérica)},
title = {New microstructural data on the existence of precambrian deformations in the Sierra de la Demanda (Iberian Range)},
author = {Ábalos, Benito},
}