Modelling of tsunami generated by the giant Late Bronze Age eruption of Thera, South Aegean Sea, Greece
نویسندگان
چکیده
منابع مشابه
Chronology for the Aegean Late Bronze Age 1700-1400 B.C.
Radiocarbon (carbon-14) data from the Aegean Bronze Age 1700-1400 B.C. show that the Santorini (Thera) eruption must have occurred in the late 17th century B.C. By using carbon-14 dates from the surrounding region, cultural phases, and Bayesian statistical analysis, we established a chronology for the initial Aegean Late Bronze Age cultural phases (Late Minoan IA, IB, and II). This chronology c...
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When Cadogan wrote ‘Dating the Aegean Bronze Age without radiocarbon’ (1978), this writer agreed completely with the view that the absolute dating of the Aegean Late Bronze Age was already established. Correlations with Egypt and other parts of the eastern Mediterranean seemed secure, and virtually all Aegean prehistorians felt that radiocarbon dates could be ‘tested’ by comparison with the Aeg...
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a Institute of Applied and Computational Mathematics, FORTH, GR-70013 Heraklion, Crete, Greece b Department of Applied Mathematics, University of Crete, GR-71409 Heraklion, Greece c Department of Environmental Engineering, Technical University of Crete, GR-73100 Chania, Greece d School of Civil & Environmental Engineering, Cornell University, Ithaca, USA e Department of Earth and Planetary Scie...
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The role of volcanogenic halogen-bearing (i.e. chlorine and bromine) compounds in stratospheric ozone chemistry and climate forcing is poorly constrained. While the 1991 eruption of Pinatubo resulted in stratospheric ozone loss, it was due to heterogeneous chemistry on volcanic sulfate aerosols involving chlorine of anthropogenic rather than volcanogenic origin, since co-erupted chlorine was sc...
متن کاملZoned, birefringent garnets from Thera Island, Santorini Group (Aegean Sea)
A garnetite that occurs locally in phyllitic schists exposed by the Santorini caldera consists mainly of euhedral garnet crystals showing alternating isotropic and birefringent lamellae. X-ray diffraction revealed two garnets with unit cell dimensions a of I2.o52:ko-oo2 and I~'984-ko-oo5 A, corresponding respectively to almost pure andradite and a granditic phase. Mean compositions determined b...
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ژورنال
عنوان ژورنال: Geophysical Journal International
سال: 2011
ISSN: 1365-246X,0956-540X
DOI: 10.1111/j.1365-246x.2011.05062.x