Publication Date:
2011-01-01
Description:
Tectonothermal analysis of a mainly carbonate unit located in the external part of the Variscan orogen in NW Spain is dealt with using the conodont colour alteration index (CAI) and the study of textures of these microfossils. The Kubler index of the illite (KI) is used as a complementary method. The area is characterized by a great uniformity in the CAI values, which in most cases are
Print ISSN:
0016-7568
Electronic ISSN:
1469-5081
Topics:
Geosciences