Pogallo Line, south Alps, northern Italy: an intermediate crustal level, low-angle normal fault?

Kip Hodges, D. M. Fountain

Research output: Contribution to journalArticle

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 languageEnglish (US)
Pages (from-to)151-155
Number of pages5
JournalGeology
Volume12
Issue number3
StatePublished - 1984
Externally publishedYes

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normal fault
rock
granulite facies
Caledonian orogeny
amphibolite
Tethys
amphibolite facies
shear zone
metamorphism
Triassic
Jurassic
cooling
mineral

ASJC Scopus subject areas

  • Geology

Cite this

Pogallo Line, south Alps, northern Italy : an intermediate crustal level, low-angle normal fault? / Hodges, Kip; Fountain, D. M.

In: Geology, Vol. 12, No. 3, 1984, p. 151-155.

Research output: Contribution to journalArticle

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