Page 71 - Maldonado_Stanley_1976

YEARS BEFORE PRESE NT (x 10 3 )
IO 15 20 25 30 35 40 45

l.l1 A 105 AS-8(a) AS-8(b) SHALLOW PLATFORM .•.....
0:: \"
w NERITIC-BATHYAL
l- 100 7G\ DEEP SLOPE
w ., ·,_ (lonian, Balearic)
2 '·,_ '~\
'·-!~
1-- ·,
z ·,_
w2oo '· '·
u '·, ·,
e
z 7

<( 300
l.l1 ..........
w l.l1
0:: 0::
o w
0 4oo 100 l-
w
z 2
I ' · .. , 1-
z
l- 500 200 w
0.... ··., ..
w .......... u
o z
' ~-........
'· ··, .. .,_ 300 co
··,· .. , l/)
w
··., .. 53 0:::
i\ .................. o
i' 400 u
;\ .................. NORTH MARITTIMO -------
\ . z
\~ .......... SMALL STRAIT BASI N - ... - ... -
'r l l ' \ "-· •• ~ PANTELLERIA ·····•·•••·••·••·•••·•
6~ l i \ \ ··.,.. MALTA -·-·-·-·- I
\ l \ 1-
800 \ i \ 500 (L
\ '-.................... ~INOSA w
' L~ \_"'
lr\ -~~ o
~ "·
\<D ' \ ' ···,,·,· .. ,
l
6~\\\ \,\
CORES 9 · .......... ....... 600
\ ·Gioo · .. ,
LYNCH Il- 3,4,5,5A,6,6A,7
l .,,
i
ATLANTIC SEAL- A-7,A-8
i
i
GESITE - KS-12,53,63,69, 100,105,109,118,120 i
b1o9 . 120 700
33 = RATE OF SEDIMENTATION
IN CM/YEARS 103
• 118
800
FIGURE 38.-Rates of sedimentation based on carbon-14 data from cores in the different Strait of
Sicily environments: A, shallow platform, neritic-bathyal, and deep slope environments; B, deep
basins and small Strait Narrows basin. (Data from core KS 69 provided by the Station de
Géologie Sous-Marine de Villefranche of the University of Paris, and from LY 11-7 from Rupke
and Stanley, 1974.)