「orogeny」の共起表現(1語右で並び替え)

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「orogeny」の共起表現一覧(1語右で並び替え)

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on the mountain, formed during the Grenville	Orogeny about a billion years ago.
ars ago) by the side effects of the Himalayan	orogeny and thus the Damodar excavated its new deep a
metamorphosed and deformed during the Acadian	Orogeny and the Alleghenian Orogeny.
building, the latest Neoproterozoic Petermann	Orogeny and Palaeozoic Alice Springs Orogeny, to leav
tamorphism, which is more associated with the	orogeny and erosion of mountain ranges on a regional
of mountain building, including the Grenville	orogeny, and subsequent erosion.
indications of inversion during the Variscan	Orogeny, but the fault was reactivated in a normal se
of uplift has taken place during the Kaikoura	Orogeny but most of this has been eroded away.
the deposition of the sediments, the Variscan	orogeny caused the intrusion of the Cornish granites
ctivation of the fault during the Alleghenian	Orogeny caused further separation of underlying rock
ly by tectonic uplift during the early Alpine	orogeny, caused by the Adriatic Plate's northwest mov
Continued	orogeny created a large fault zone in the bedrock thr
About 400 million years after the Grenville	orogeny during the Catoctin Formation, deposition of
The area was uplifted by the Laramide	orogeny during latest Cretaceous.
also received sediments from the Appalachian	orogeny during the Pennsylvanian.
asin was a foreland basin during the Ouachita	Orogeny during the Pennsylvanian and Permian Periods.
s are believed to derive from the Appalachian	orogeny events.
cient folded mountains formed by the Ouachita	orogeny existed in the eastern part of the Metroplex
uring the Variscan mountain building episode (	orogeny) in the Carboniferous Period of geological hi
present form was shaped during the Innuitian	orogeny in the middle of the Mesozoic era when the No
In later continental drift and	orogeny it became most of Spain and Portugal.
uthwesternmost visible extent of the Ouachita	orogeny, lies the Solitario.
During the Variscan	orogeny, magma intruded along structural zones, but c
t and collisions, starting with the Grenville	Orogeny nearly 1.5 billion years ago.
The lake was formed from the formation of an	orogeny of the Himalayas 249 million years ago, and o
ry, which was created during the Trans-Hudson	orogeny, of tectonic origin between the Belcher Fold
d by a diapir generated during the alpinotype	orogeny of the Tertiary period.
alf of the period was an episode of intensive	orogeny on virtually all continents.
ed at the northern margin of the Trans-Hudson	orogeny on central Baffin Island, Nunavut, Canada.
in of palaeozoic rocks folded in the Variscan	Orogeny, similar to the South Wales coalfield to the
e approximately 70-65 MYA during the Laramide	orogeny that created the modern Rocky Mountains.
During the Appalachian	orogeny, the sedimentary rock layers in this area fol
At this time, the Alpine	Orogeny, the major mountain building event that was t
In this	orogeny the Southern alps are being formed because th
mately 700 million years after the Greenville	Orogeny, the Iapetus Ocean began to close resulting i
brian age and first uplifted during Grenville	Orogeny then again during the Alleghenian Orogeny, in
from the mountains thrown up by the Cimmerian	orogeny through the arid lands of continental East As
The	orogeny was centred in an area that had previously be
The Ouachita	orogeny was a mountain building event that resulted i
The Alice Springs	Orogeny was a major tectonic (mountain building) epis
400 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 North American and African plates c
200 million years ago during the Appalachian	orogeny, when the collision of the North American and
-400 million years ago during the Alleghenian	orogeny, when the collision of two continental plates
years ago, the area underwent the Delamerian	orogeny where the geosynclinal sequence was folded an
rata in the basin were formed by the Ouachita	orogeny, which also formed the Ouachita Mountains of

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