A palaeomagnetic investigation at four sites in 1.4 Ma basaltic lavas and two sites in the Upper Pliocene-Lower Quaternary sediments document the lack of rotational deformation along the Nea Anchialos Fault System, Central Greece.
Palaeomagnetic evidence of non rotational deformation along the Nea Anchialos Fault System, Central Greece
CAPUTO, Riccardo
1997
Abstract
A palaeomagnetic investigation at four sites in 1.4 Ma basaltic lavas and two sites in the Upper Pliocene-Lower Quaternary sediments document the lack of rotational deformation along the Nea Anchialos Fault System, Central Greece.File in questo prodotto:
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