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Weblio 辞書 > 英和辞典・和英辞典 > Metamorphismの意味・解説 > Metamorphismに関連した共起表現

「Metamorphism」の共起表現一覧(1語右で並び替え)

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used in geology to determine the degree of metamorphism a rock has experienced.
ensely deformed and subjected to high grade metamorphism along with the Churchill terrain during the
The Torlesse Greywacke has undergone metamorphism and been transformed into Haast Schist.
rals such as rhodocrosite during low oxygen metamorphism and metasomatism
his provided unambiguous evidence for shock metamorphism, and confirmed the impact origin of the Red
Clinohumite is a product of contact metamorphism and is commonly found as indistinct grains
egorical dual of a hylomorphism is called a metamorphism, and is a catamorphism followed by an anamo
In his published papers he dealt with metamorphism and crystalline schists, discussed the orig
where they have been subject to high-grade metamorphism and intense deformation.
ng sedimentary rocks gave rise to extensive metamorphism and mineralisation, and this led to Cornwal
At Otago he became interested in metamorphism and studied the unexplored metamorphic rock
the understanding of the processes of rock metamorphism and the origins of granite".
nomena and igneous rocks, to the effects of metamorphism, and to mineral veins, in various parts of
Sperrylite is formed by contact metamorphism, as in indicated by the development of trip
ly is one of the best mineral indicators of metamorphism at very high pressures (UHP, or ultrahigh-p
The lack of shock metamorphism at the site further backs the latter claim.
Cornish granites and the subsequent contact metamorphism created the metamorphic rocks seen today.
Retrograde metamorphism has occurred, leaving a serpentine-anthophy
cult to distinguish from one another if the metamorphism has been great.
denying the occurrence of shock metamorphism in Azuara rocks.
s to 1912, when G.M. Barrow mapped zones of metamorphism in southern Scotland.
hirine is primarily a product of high grade metamorphism in environments poor in silica and rich in
Contact metamorphism is caused by the interaction of rock with h
The maximum temperature for metamorphism is typically 700 - 900°C, depending on the
Marialite occurs in regional and contact metamorphism: marble, calcareous gneiss, granulite and g
the Alps, Corsica, etc., and the subject of metamorphism occupied his attention.
ite and spurrite are formed through contact metamorphism of limestone.
Tremolite forms by metamorphism of sediments rich in dolomite and quartz.
Metamorphism of the carbonaceous material is expressed i
ield can indicate high temperature regional metamorphism of the surrounding rocks.
teration of other manganese minerals during metamorphism of manganese deposits.
It occurs as a product of metamorphism of phosphate bearing peraluminous sediments
occurs as an alteration mineral in contact metamorphism of limestone.
odite is formed within terrestrial rocks by metamorphism of peridotite and dunite via a process of n
has been proposed as a geobarometer for the metamorphism of low grade schists.
It is a product of contact metamorphism of siliceous limestones and dolostones, and
Metamorphism of ultramafic rocks in the presence of wate
, and was probably formed during the alpine metamorphism of the Alps.
ve rocks, on the structure of the Jura, the metamorphism of the Western Alps, on the formation of oo
ic rocks that experience deformation during metamorphism, porphyroblasts may grow before, during, or
students of geological history, but because metamorphism produced gold deposits which were mined ext
atism, which is a chemical change caused by metamorphism, recrystallization is a physical process.
en generally found in areas of medium-grade metamorphism, reported from the Hoggar Mountains of Alge
During metamorphism, rocks which were originally sedimentary or
During metamorphism, sulfur and nickel within the olivine latti
This means that the metamorphism was the result of igneous intrusion directl
wer greenschist through to granulite facies metamorphism when the rock in question is subjected to m
reme temperature conditions during prograde metamorphism, where partial melting occurs in pre-existi
semblage has not been altered by retrograde metamorphism, which can be assessed using an optical mic
mont and Georgia are the result of regional metamorphism, which is more associated with the orogeny
Contact metamorphism would also be responsible for the very conc
                                                                                                    


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