Novel Application Of The Anisotropy Of Magnetic Susceptibility (AMS) In Cenozoic Strata Across The Central Italian Apennines As A Paleogeodetic Measure Of Strain And The Eastward March Of Extension Above A Foreland Dipping Detachment
Novel Application Of The Anisotropy Of Magnetic Susceptibility (AMS) In Cenozoic Strata Across The Central Italian Apennines As A Paleogeodetic Measure Of Strain And The Eastward March Of Extension Above A Foreland Dipping Detachment
