SCIENTIFIC-RESEARCH STUDY ON EARTHQUAKE FORECASTING

This scientific paper provides an extensive review and alternative theoretical paradigm regarding the genesis of tectonic earthquakes, challenging the traditional elastic rebound theory. Utilizing long-term observation data from the historical Niigata Experiment (Japan, 1964), volcanic inflation trends in Yellowstone Caldera (USA, 1973), and seismic wave velocity anomalies (Vp/Vs) recorded in the Garma region (Tajikistan, 1955–1966), a unified mechanism is established. The paper argues that earthquakes are predominantly triggered by vertical, buoyancy-driven migration of lower-density fluid masses (magma or fluid reservoirs) accumulating beneath the highly irregular base of the solid lithosphere (calderas). A comprehensive, two-phase empirical forecasting methodology is presented: incorporating long-term geodetic GPS monitoring of anomalous ground deformation rates with short-term, localized crustal seismic wave velocity profiling.

Authors

Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2026-09-11
DOI
https://doi.org/10.5281/zenodo.22710308
Primary Topic
earthquake and tectonic studies
Type
preprint
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preprint

SCIENTIFIC-RESEARCH STUDY ON EARTHQUAKE FORECASTING

Zoran Ilinčić
Zenodo (CERN European Organization for Nuclear Research)
earthquake and tectonic studies
preprint

SCIENTIFIC-RESEARCH STUDY ON EARTHQUAKE FORECASTING

Zoran Ilinčić
preprint en

Abstract

This scientific paper provides an extensive review and alternative theoretical paradigm regarding the genesis of tectonic earthquakes, challenging the traditional elastic rebound theory. Utilizing long-term observation data from the historical Niigata Experiment (Japan, 1964), volcanic inflation trends in Yellowstone Caldera (USA, 1973), and seismic wave velocity anomalies (Vp/Vs) recorded in the Garma region (Tajikistan, 1955–1966), a unified mechanism is established. The paper argues that earthquakes are predominantly triggered by vertical, buoyancy-driven migration of lower-density fluid masses (magma or fluid reservoirs) accumulating beneath the highly irregular base of the solid lithosphere (calderas). A comprehensive, two-phase empirical forecasting methodology is presented: incorporating long-term geodetic GPS monitoring of anomalous ground deformation rates with short-term, localized crustal seismic wave velocity profiling.

Zenodo (CERN European Organization for Nuclear Research)
Climate action
earthquake and tectonic studies
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