「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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