「Gabbro」の共起表現(1語右で並び替え)

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共起表現

「Gabbro」の共起表現一覧(1語右で並び替え)

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clude picrite, peridotite, dunite, pyroxenite,	gabbro and granophyre.
Intrusive equivalents (	gabbro and diorite) are collectively known as the Kam
	Gabbro and norite often occur in the upper portions o
remainder of the volcano today is dominated by	Gabbro and granophyre and is also so site of a noted
It occurs with	gabbro and other mafic to ultramafic rocks in layered
common mafic igneous rocks such as basalt and	gabbro, as well as in anorthosites.
rphic rocks such as granite, syenite, diorite,	gabbro, basalt, andesite, gneiss, and schist.
slip Liquine-Ofqui fault zone and include some	gabbro bodies.
ting a hybrid origin involving assimilation of	gabbro by high-temperature syenitic magma.
	Gabbro can be formed as a massive, uniform intrusion
Basalt and	gabbro commonly exhibit an equigranular texture.
uring the early 1900s in describing the Duluth	gabbro complex in northern Minnesota and adjacent Ont
Examples of phaneritic igneous rocks are	gabbro, diorite and granite.
o their coarser-grained intrusive equivalents (	gabbro, diorite, granodiorite, and granite).
Glacier and is the northwesternmost summit in	Gabbro Hills.
c volcanic rocks; in nodules of peridotite and	gabbro in alkalic basalts; in syenites, monzonites an
A feeder dike of olivine	gabbro is exposed "below" the now tilted sequence.
	Gabbro is usually equigranular in texture, although i
	Gabbro often contains valuable amounts of chromium, n
	Gabbro or norite is also quarried from parts of the C
Essexite can be considered as an alkali	gabbro or monzodiorite primarily composed of nephelin
ted as having been reset by later intrusion of	gabbro sills at 604 - 718 Ma).
basaltic sequence, a sheeted dike complex and	gabbro stocks.
ks in Jay Cooke are built with local basalt or	gabbro stone and dark planks and logs.
stal sage scrub habitat on rocky sandstone and	gabbro substrates.
Examples include the Duluth	gabbro, the Sudbury Igneous Complex of Ontario, the B
roduced a maskelynite-like glass by subjecting	gabbro to an explosive shock wave.
ith extend from 47 to 55 °S and include mafic (	gabbro) to felsic (granite) bodies.
	Gabbro was named by the German geologist Christian Le
Limestone and	gabbro were used as flux.
Rica and into a layer of igneous rock known as	gabbro, which is formed from solidified magma.
ajority of the Earth's surface is underlain by	gabbro within the oceanic crust, produced by basalt m
Norite is essentially indistinguishable from	gabbro without thin section study under the petrograp

共起表現

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「Gabbro」の共起表現一覧(1語右で並び替え)