A GIANT QUASI-RING MANTLE STRUCTURE BENEATH THE EASTERN MEDITERRANEAN: INTERPRETATION OF NEW SEISMIC-TOMOGRAPHY, MAGNETIC FIELD, AND PALEOBIOGEOGRAPHIC DATA
- Authors: Eppelbaum L.V.1,2, Katz Y.I.3, Ben-Avraham Z.1
-
Affiliations:
- Tel Aviv University, Faculty of Exact Sciences
- Azerbaijan State Oil and Industry University (ASOIU)
- Steinhardt Museum of Natural History – National Research Center, Tel Aviv University, Faculty of Life Sciences
- Issue: No 2 (2025)
- Pages: 3-31
- Section: Articles
- URL: https://journal-vniispk.ru/0016-853X/article/view/304362
- DOI: https://doi.org/10.31857/S0016853X25020011
- EDN: https://elibrary.ru/egrkdv
- ID: 304362
Cite item
Abstract
In the presented article, a quantitative reinterpretation of the residual satellite gravity anomaly is carried out. Additional necessary confirmation is provided by the distribution of anomalies in the regional magnetic field ΔZ, reduced to a height of 2.5 km above sea level. Based on the analysis of detailed paleomagnetic studies, the average rotation rate of the surface projection of the deep structure over the past 70 million years is estimated at about 18 mm/year. The authors constructed a paleobiogeographic map showing the counterclockwise displacement of the typical Ethiopian fauna to the northwest. The influence of the rotating deep structure on stress in the overlying blocks of the Earth’s crust and lithosphere before the catastrophic earthquakes with magnitudes M=7.9 and M=7.8 that occurred on 06.02.2023 in Turkey is shown. The synthesis of seismic tomography profiles made it possible to construct a seismotomographic scheme of the location of the deep structure. This scheme agrees with the analysis of satellite gravity and marine/terrestrial gravity studies, geoid anomalies, magnetic anomaly distributions, paleomagnetic data, regional GPS vector directions, seismological and tectonic-structural, and mineralogical-petrological data. The integrative combination of all these factors is indisputable to confirm the existence of an anomalous deep rotating structure beneath the Eastern Mediterranean and adjacent regions.
About the authors
L. V. Eppelbaum
Tel Aviv University, Faculty of Exact Sciences; Azerbaijan State Oil and Industry University (ASOIU)
Author for correspondence.
Email: levap@tauex.tau.ac.il
Ramat Aviv, 6997801 Tel Aviv, Israel; bld. 20, Azadlyg Ave., AZ1010 Baku, Azerbaijan
Yu. I. Katz
Steinhardt Museum of Natural History – National Research Center, Tel Aviv University, Faculty of Life Sciences
Email: levap@tauex.tau.ac.il
Ramat Aviv, 6997801 Tel Aviv, Israel
Z. Ben-Avraham
Tel Aviv University, Faculty of Exact Sciences
Email: levap@tauex.tau.ac.il
Ramat Aviv, 6997801 Tel Aviv, Israel
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