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      Midcrustal shear zones in postorogenic extension: Example from the northern Tyrrhenian Sea

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          Extension in the Tyrrhenian Sea and shortening in the Apennines as result of arc migration driven by sinking of the lithosphere

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            Dynamics of orogenic wedges and the uplift of high-pressure metamorphic rocks

            J. PLATT (1986)
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              Geological evolution of the tethys belt from the atlantic to the pamirs since the LIAS

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                Author and article information

                Journal
                Journal of Geophysical Research: Solid Earth
                J. Geophys. Res.
                American Geophysical Union (AGU)
                01480227
                June 10 1998
                June 10 1998
                : 103
                : B6
                : 12123-12160
                Article
                10.1029/97JB03616
                2b328247-9192-4210-8628-0bdc49fc57af
                © 1998

                http://doi.wiley.com/10.1002/tdm_license_1.1

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