-
which lasted between the
Cambrian and the
Early Tri****ic,
while the
Neotethys formed during the Late Tri****ic and
lasted in some form up to the Oligocene–Miocene...
- the
Eurasia margin as the
Neotethys crust was
subducted beneath it. A
separate intra-oceanic
subduction zone in the
Neotethys resulted in the obuction...
- Superterranes.
During the
Early Permian, this rift
developed into the
Neotethys ocean (Fig. 2). From that time on, the
Cimmerian Superterranes drifted...
- part. At
about the same time, 170 mya in the Jur****ic period, a
small Neotethys ocean basin formed shortly before the
Tethys Sea was
closed at the eastern...
- age and are well
known for fish fossils.
Lebanon was
submerged in the
Neotethys ocean at the time, but some
small islands were exposed. The only known...
-
forming during the Late
Cretaceous epoch as a
result of the
closure of the
Neotethys Ocean that
caused shortening of the
continental margin with reactivation...
- China; SC=South China; PA=Panthal****ic Ocean; PT=Paleotethys Ocean; NT=
Neotethys Ocean.
Orogens shown in red.
Subduction zones shown in black. Spreading...
- Ocean; it is now
known to be a
structurally younger basin,
called the
Neotethys,
which was
first formed by the
convergence of the
African Plate and Eurasian...
-
Neotethys during the
Oligocene (Rupelian, 33.9–28.4 mya)...
- p****ive
continental margin on the
Arabian Plate. However, the
obduction of
Neotethys oceanic crust during the
Cretaceous (145–66 mya), and the continental...
