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Extensional detachment faulting on the Tyrrhenian margin of the southern Apennines contractional belt (Italy)
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Abstract:
The tectonic evolution of the Campania margin during the late Pliocene-Pleistocene is characterized by extensional deformation coeval with the opening of the Marsili oceanic basin. The initial stages of stretching are represented in the analysed area by the development of low-angle normal faults that extended the belt in the same direction as the direction of spreading recognized for the oceanic basin. Detachment faulting was accompanied by the onset of magmatic activity and by major uplifts that resulted in the accumulation of thick conglomerate successions in the half-grabens that ...
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Barak's second career
Newspaper article from: Jerusalem Post
; Amotz Asa-El Jerusalem Post 09-26-1997 When he chased Napoleon out of Russia, Mikhail Ilarionovich Kutuzov was already 67, and a mere several months away from his death by natural causes. Field Marshal Montgomery still actively commanded...
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