Page 159 - Carbonate Platforms Facies, Sequences, and Evolution

12"E 13"E 14"E
PLIENSBACHIAN PALEOGEOGRAPHY
44"N 44"N
Adriatic Sea 20"N Bagnolo Platform
-� '-''l<l
0:
m Pliocene · Quaternary volcanics () : 0 0
!v:
. � 19•N o
UMBRIA - MARCHES APENNINES ' .
;;; 0
0 ' 0 0 n D
D Plio-Pleistocene deposits � 'Umbria-Marches
P o v,._
,
0. ' , :, Basin 0 Isolated Platforms
� Flysch of the Tuscan Nappe .
� 18"N .. . a
� �
·-,;(� I
.. "· "'/ :'�
• Liguride Allochthon � ' � 0 "0 ';
"'
EJ Miocene siliciclastic flysch
17"N
ITIIIi U. Triassic through Oligocene carbonates
ABRUZZI CARBONATE PLATFORM
43"N
43"N � Miocene siliciclastic and calcareous flysch
� U. Triassic through Oligocene platform carbonates
f53
�� � carbonate facies between platform and basin HETTANGIAN PALEOGEOGRAPHY
U. Triassic through Oligocene transitional
0 Teramo 20"N
� 1£)
v v v j 19"N
v v v
v v v v " 2
v v v v �
v v 'v v v 0 . � 18"N
v v v v v l
v v v v v v "'
42"N 42"N
17"N
12"E 13"E 14"E
Fig. 1. Index map, generalized geology and palaeogeography of the study area. Hettangian palaeogeography
platform. Pliensbachian palaeogeography shows scene after extension and break-up of pre-existing platform
Mattavelli (1986) and Bosellini et al. (1981). Palaeolatitudes from palaeomagnetic data of Channell et a