Abstract
In this paper the Author suggests to regard the lower
limit of the category of the so-called shallow earthquakes identical with the
level of the regional isostatic compensation and the upper limit of the
so-called deep shocks identical with the Byerly-discontinuity.
limit of the category of the so-called shallow earthquakes identical with the
level of the regional isostatic compensation and the upper limit of the
so-called deep shocks identical with the Byerly-discontinuity.
Full Text:
PDFReferences
DOI: https://doi.org/10.4401/ag-5214
Published by INGV, Istituto Nazionale di Geofisica e Vulcanologia - ISSN: 2037-416X