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Seismic stratigraphy od Santorini's Caldera: a contribution to the understanding of the Minoan eruption. Sakellariou D.
1. SEISMIC STRATIGRAPHY OF SANTORINI’S
CALDERA: A CONTRIBUTION TO THE
UNDERSTANDING OF THE MINOAN ERUPTION
Sakellariou D.1, Rousakis G.1, Sigurdsson H.2, Nomikou P.3,
Katsenis I.4, Croff Bell K.L.2, Carey S.2
1
Inst. Oceanography, Hellenic Centre for Marine Research
2
Graduate School of Oceanography, University of Rhode Island, USA
3
Geology Dptm , National Kapodistrian University of Athens, Ilissia, Greece,
4
Geology Dptm., University of Patras
10ο Πανελλήνιο Συμπόσιο Ωκεανογραφίας & Αλιείας
7-11 Μαϊου 2012, Αθήνα
2. HCMR surveys Cape Riva
in the Caldera Caldera
Multibeam bathymetry 2001,
2006, 2012
Airgun 10ci seismic profiling
2006 & 2012
n
si
Chirp & 3.5kHz subbottom Ba
profiling 2012 rth
No
Side scan sonar imaging
2012
Submersible Thetis dives West Basin
2006
ROV Max Rover dives 2012 South Basin
Seafloor sampling 2006, 2012
19. RESULTS
(i) the thickness of the Minoan deposits on the caldera seafloor
exceeds 100 m locally,
(ii) post Minoan deposits are negligible,
(iii) the lower, gently sloping parts of the slopes around Kameni
islands are of Minoan age,
(iv) all three subbasins of the caldera existed prior to the Minoan
eruption and were filled with pyroclastics during and after the 17 th
cent. BC eruption
(v) the Minoan eruption center was located where the present day
Kameni islands are.
21. EUROFLEETS
Caldera 2012
Mapping gas concentration in real time
with the TETHYS mass spectrometer,
mounted on THETIS submersible
1.00E-06
CO2
ambient vent
1.00E-07 CH4
CO
ion peak intensity (Torr)
H2S
1.00E-08
Hydrocarbon?
1.00E-09
NOx
1.00E-10
1.00E-11
10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40 42 44 46
mass-to-charge ratio
22. EUROFLEETS
Caldera 2012
January 2012
ROV Max Rover dive
North of Nea Kameni
380m depth
Small crater on the Caldera’s seafloor