Abstract
The Pogallo Line is a major crustal shear zone which separates crystalline middle amphibolite-granulite facies rocks of the Ivrea zone from lower-middle amphibolite facies rocks of the Strona-Ceneri zone. U/Pb, Rb/Sr and K/Ar whole-rock and mineral ages for samples from this region indicate that the two zones pursued different time-T paths after Caledonian peak metamorphism. Cooling curves for the two terrains finally converge in the late Triassic-early Jurassic, a time of large-scale crustal extension in the south Alps that anticipated the opening of the western Tethys. The Pogallo Line may represent a low-angle normal fault that developed at intermediate crustal levels during this period of extension and attained its present subvertical orientation during Alpine deformation. (Authors' abstract)-C.N.
Original language | English (US) |
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Pages (from-to) | 151-155 |
Number of pages | 5 |
Journal | Geology |
Volume | 12 |
Issue number | 3 |
State | Published - 1984 |
Externally published | Yes |
ASJC Scopus subject areas
- Geology