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Magma flow and thermal contraction fabric in tabular intrusions inferred from AMS analysis. A case study in a late-Variscan folded sill of the Albarracín Massif (southeastern Iberian Chain, Spain)

✍ Scribed by A. Gil-Imaz; A. Pocoví; M. Lago; C. Galé; E. Arranz; C. Rillo; E. Guerrero


Book ID
113756742
Publisher
Elsevier Science
Year
2006
Tongue
English
Weight
896 KB
Volume
28
Category
Article
ISSN
0191-8141

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