「orogeny」の共起表現(2語左で並び替え)

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共起表現

「orogeny」の共起表現一覧(2語左で並び替え)

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The Alice Springs	Orogeny was a major tectonic (mountain building) epis
uring the Variscan mountain building episode (	orogeny) in the Carboniferous Period of geological hi
In later continental drift and	orogeny it became most of Spain and Portugal.
brian age and first uplifted during Grenville	Orogeny then again during the Alleghenian Orogeny, in
ly by tectonic uplift during the early Alpine	orogeny, caused by the Adriatic Plate's northwest mov
In this	orogeny the Southern alps are being formed because th
though was active again in the later Variscan	orogeny.
building, the latest Neoproterozoic Petermann	Orogeny and Palaeozoic Alice Springs Orogeny, to leav
The lake was formed from the formation of an	orogeny of the Himalayas 249 million years ago, and o
alf of the period was an episode of intensive	orogeny on virtually all continents.
lcanic island arc in the Southern Alleghenian	orogeny.
indications of inversion during the Variscan	Orogeny, but the fault was reactivated in a normal se
Ordovician, (ca 450 Ma) to create the Taconic	Orogeny.
ry, which was created during the Trans-Hudson	orogeny, of tectonic origin between the Belcher Fold
t and collisions, starting with the Grenville	Orogeny nearly 1.5 billion years ago.
About 400 million years after the Grenville	orogeny during the Catoctin Formation, deposition of
400 million years ago during the Appalachian	orogeny, when the North American and African plates c
ferous inversion associated with the Variscan	Orogeny.
in of palaeozoic rocks folded in the Variscan	Orogeny, similar to the South Wales coalfield to the
from the mountains thrown up by the Cimmerian	orogeny through the arid lands of continental East As
zoic period and uplifted during the Grenville	Orogeny.
ars ago) by the side effects of the Himalayan	orogeny and thus the Damodar excavated its new deep a
the Penokean	orogeny (1890-1830 Ma)
200 million years ago during the Appalachian	orogeny.
metamorphosed and deformed during the Acadian	Orogeny and the Alleghenian Orogeny.
sin was locally deformed during the Petermann	Orogeny (late Neoproterozoic - Cambrian), and more ex
ss related to deformation of the Trans-Hudson	orogeny.
ateral) strike-slip fault during the Variscan	Orogeny.
The area was uplifted by the Laramide	orogeny during latest Cretaceous.
d 400 million years ago during the Caledonian	orogeny.
200-300 million years during the Appalachian	orogeny.
s are believed to derive from the Appalachian	orogeny events.
also received sediments from the Appalachian	orogeny during the Pennsylvanian.
on from rivers which predated the Alleghenian	orogeny.)
rnubian batholith, formed during the Variscan	orogeny.
During the Variscan	orogeny, magma intruded along structural zones, but c
pe structures towards the end of the Variscan	orogeny.
cale forming event during the Trans-Hudsonian	orogeny.
uthwesternmost visible extent of the Ouachita	orogeny, lies the Solitario.
d by a diapir generated during the alpinotype	orogeny of the Tertiary period.
During the Appalachian	orogeny, the sedimentary rock layers in this area fol
d down in a coastal plain during the Laramide	orogeny.
e area from the southeast during the Ouachita	orogeny.
lted and tightly folded during the Caledonian	Orogeny.
cient folded mountains formed by the Ouachita	orogeny existed in the eastern part of the Metroplex
ted over the European plate during the Alpine	orogeny.
asin was a foreland basin during the Ouachita	Orogeny during the Pennsylvanian and Permian Periods.
American landmass as part of the Appalachian	orogeny.
the deposition of the sediments, the Variscan	orogeny caused the intrusion of the Cornish granites
At this time, the Alpine	Orogeny, the major mountain building event that was t
The Ouachita	orogeny was a mountain building event that resulted i
present form was shaped during the Innuitian	orogeny in the middle of the Mesozoic era when the No
200 million years ago during the Appalachian	orogeny, when the North American and African plates c
ion years ago at the start of the Pan-African	orogeny.
rata in the basin were formed by the Ouachita	orogeny, which also formed the Ouachita Mountains of
ctivation of the fault during the Alleghenian	Orogeny caused further separation of underlying rock
Permian time, the last phase of the Variscan	orogeny.
of uplift has taken place during the Kaikoura	Orogeny but most of this has been eroded away.
in a molasse sequence produced by the Taconic	orogeny.
the Churchill terrain during the Trans-Hudson	orogeny.
e approximately 70-65 MYA during the Laramide	orogeny that created the modern Rocky Mountains.
years ago, the area underwent the Delamerian	orogeny where the geosynclinal sequence was folded an
200 million years ago during the Appalachian	orogeny, when the collision of the North American and
on the mountain, formed during the Grenville	Orogeny about a billion years ago.
mately 700 million years after the Greenville	Orogeny, the Iapetus Ocean began to close resulting i
osion of mountains created during the Taconic	orogeny.
ed at the northern margin of the Trans-Hudson	orogeny on central Baffin Island, Nunavut, Canada.
-400 million years ago during the Alleghenian	orogeny, when the collision of two continental plates
of mountain building, including the Grenville	orogeny, and subsequent erosion.
tamorphism, which is more associated with the	orogeny and erosion of mountain ranges on a regional

共起表現

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「orogeny」の共起表現一覧(2語左で並び替え)