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R. Catalano et al./ Tectonophysics 260 (1996) 291-323                                                                    297

schematic deep geologica! sections of the area. Part                  and in the Sardinia Channel (Barbieri et al., 1984;
of this research, focused on the northeastern Sicily                  Catalano et al., 1985; Torelli et al., 1985; Antonelli
Straits and southern Sicily offshore (Fig. I), demon-                 et al., 1991 ). The stratigraphic scheme in Fig. 6
strated close relations between the regional tectonic                 refers to the offshore formations and to westernmost
grain of Sicily and the offshore region (Catalano et                  Sicily. Some type successions of the Sicily Straits-
al., 1989a; Casero and Roure, 1994).                                  Sicily Channel area appear comparable to or continu-
                                                                      ous with the successions of westernmost Sicily and
4. Stratigraphy and facies domains                                    are believed to pass westwards to the stratigraphic
                                                                      sequences of eastern Tunisia and its offshore (Sestini
   The stratigraphy of the studied area is well known                 and Flores, 1986; Catalano, 1987; Antonelli et al.,
on land (Fig. 5 and generai schemes in Catalano and                   1991 ).
D'Argenio, 1982; Montanari, 1989). At sea the doc-
umentation, based on commerciai wells, seismic fa-                       In the submerged area between the Egadi and the
cies analysis and dredge hauls, is fairly good in the                 Malta Islands ali the available data indicate a sedi-
Sicily Straits and Sicily Channel (Catalano, 1987;                    mentary succession consisting of widespread Trias-
Catalano et al., 1989a; Antonelli et al., 1991; Casero                sic-Lower Liassic carbonate platform deposits over-
and Roure, 1994) but poor north of the Egadi Islands                  lain by Jurassic-Paleogene seamount and slope to
                                                                      basin, marly and sandy carbonates, in turn uncon-
                                                                      formably covered by Neogene foredeep deposits (Fig.

              TRATIGRAPHY A N D FACIES DOMAINS

                                                                                                                   DEEP CARBONATE
                                                                                                                      LMS & MARLS

                                                                                                                         (RAGUSA)

        :144                                                                  MARLV LMS {HYB~)
                                                                      CALPIONELUD LIME~HONES

u  '"'                                                                NODULARUIS                                   MARLYLMS(SUCCHER/)

o                                                                     "ROSSO            "AOSSO.f.JIIIICWrtiTICO'      "ROSSO

N                                                                     AMMOIITlCO' f 1rfrR~AT.                      AMMOtlllCO" BASINAL

o                                                                                  BASINAESED.                                            UIS

"'l>l Early                                                           (INICI) ~~~-~S'·(INICI)                      STREPPENOSA~-'

::; j213                                                                                                            Sl~~~ACUSAJ

                                                                      C A AB ,

    DOMAINS        -s.~c~OO.T- Wt.--.inmOir-Ski~OiiS.~  NildePiateau  -w.-stem SiCiiY      swSiliily-.r,r- -r
   LOCATIONS  L_ -~~- WESTERN~!!._Ii_ __ _                PanJ811e~a    ~ OffShorr~ __
                                                                                        ~'!'!~ ~a_!r_ r?!!St~t?re

Fig. 6. Stratigraphy and facies domains of westemmost Sicily and Sicily offshore (time scale according to Harland et al., 1990).
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