Page 2 - CatalanoInfuso1992
P. 2
Si\RDINIAN Mi\RGIN CORNAGL!J\ BASIN WESTERN ll/\NK
Figuro 3a. Geologica! cross scction oi \Sardinia Channel area !rom seismic profilo. 1. Post· C]
Messin ian deposits, 2. Messinian hori~on1 3. Syn·rift deposits, 4. ?meso~oic·tertiary deposits, 5.
Figure 1. Sardinia Channel and Sicily Straits location map. Sardinian type basernont. 6 . C<~labrian type basoment.
Fguro 2. SINCVralmapot ,.,...,c:::r.=:::--------- - - - - - - - -- ,r:::J :l'III .CJ ..rft.ID
rne Sardnia Channel.sdy CJ.c:"."J..c·r
S1rai1s ar~>a. t) Easlcrn ..P o# oo11!' .,f"'
SMinia SlnJCilJral tni!S; 2) Figure 3b. Eastern Sardinia margin. Detail of the Figure 3a
is shown by the NW-SE' soismic fina. Thick ?mesozoic·
Kabilo-Pelontan Uni!S; 3) tertìary deposits covering the inferred crustal crystalline
substrate were folded and faulted prior lo the Messinian.
Sidlian·Maghrot>an Uni!S; Synrift deposits contain Mossinian hori~ons. Faulting and
tilling continued In more rocanttimo.
4) Dolormed Tononian
tcrrains: 5) Oclormed
1owcr Pfocxnc tooam: 6)
Plio·Picistoccnc <XliiC<; 7)
Mc<..o-Ccnozcic substraiO;
C) Thrusl; 9) Posi·
Mcssinian hall grabcms:
IO) Syrdnc: I l ) 1\nlicinc;
12) Normal laulls.Tho
toctonic schcmc, in lho lcft
corner shows : A:
superimposod cxle<lsion.
B: Plio-Oualernary
volcanoes. C: Corsica·
SMinia. 0: ~Ate.
Kabilias and
4ntemal"ftysch ophioliles,
E: Maghreb-Sicily-
Southern Apen-nines
imtri:al'35, F: forecl9ep, G:
mildly lolded loroland, H:
mail o.oertlvust front