- The
Variscan or
Hercynian orogeny was a
geologic mountain-building
event caused by Late
Paleozoic continental collision between Euramerica (Laurussia)...
- Caledonian, Alleghenian,
Mauritanide and
Variscan orogenies. The
eastern portions of the
range are also
called the
Variscan Mountains. The
Central Pangean Mountains...
-
laying to the south. The
Central Pangean Mountains were
formed during the
Variscan-Alleghanian-Ouachita orogeny.
Today their remains stretch over 10,000 km...
-
Permian (more than 300
million years old) and
therefore deformed during the
Variscan Orogeny.
Parts of the
Sudetes within the
Bohemian M****if,
Giant Mountains...
-
northward and
eventually collided to form the Appalachian, Caledonide, and
Variscan orogens. West Avalonia, in
North America,
stretches from New
England to...
- (2002). "Paleozoic
evolution of pre-
Variscan terranes: From
Gondwana to the
Variscan collision" (PDF).
Variscan-Appalachian dynamics: The
building of...
- of France. It
developed since the Tri****ic over
remnant uplands of the
Variscan orogeny (Hercynian orogeny). The
sedimentary basin, no
longer a single...
-
extension and
thinning due to slab
rollback of the
African Plate. The
Variscan orogeny was a
result of the
collision between the
Laurussia and Gondwana...
- Siberia-Kazakhstania, the
latter of
which forms Laurasia and the
Uralian orogeny.
Variscan orogeny continues (these
collisions created orogenies, and
ultimately Pangaea)...
-
include the
Acadian Orogeny in
North America and the
beginning of the
Variscan Orogeny in Europe.
These early collisions preceded the
formation of the...
