「orogeny」の共起表現(1語左で並び替え)

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共起表現

「orogeny」の共起表現一覧(1語左で並び替え)

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

共起表現

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