「MAGMAS」の共起表現(1語右で並び替え)

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共起表現

「MAGMAS」の共起表現一覧(1語右で並び替え)

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riving the crystallisation of volatile-bearing	magmas, a process that can occur without any attendan
ough his work on the experimental petrology of	magmas and volatiles.
plexes, in pegmatites associated with alkaline	magmas and in or associated with carbonatite intrusiv
part of the crystallization of minerals within	magmas, and they can be found in both volcanic and pl
They are primitive because nearly all	magmas and lavas come from the same source material:
Calc-alkaline	magmas are typically hydrous, and also typically are
alkaline igneous rocks, although calc-alkaline	magmas are known in the region.
istry is similar to modern-day subduction zone	magmas, but there is disagreement as to whether moder
artial melting of the crust, creating granitic	magmas, during the emplacement of large volumes of re
	Magmas erupted from the Erebus hotspot are similar to
Both Sr and Rb are found in most	magmas, however as fractional crystallization occurs
of the earth that were carried up by ascending	magmas; kimberlite is the most common host of such xe
ization and to be at least partly derived from	magmas of basalt or andesite composition formed in th
te have been reported from potassic ultramafic	magmas on Malaita Island on the Ontong Java Plateau S
Granitic	magmas provide additional examples of how melts of ge
usive eruptions occur when hot, (1200°C) runny	magmas reach the surface of the Earth's crust.
re earth elements (HREE) are Eu - Lu. Rocks or	magmas rich, or only slightly depleted in light rare
cause of the release of latent heat of fusion,	magmas that crystallise by decompression can actually
Mechanisms by which the calc-alkaline	magmas then evolve may include fractional crystalliza
Silicic is the group of silicate	magmas which will eventually crystallise a relatively
ct metasomatism created by Hercynian tonalitic	magmas, which make up the “Zentralgneis", although th

共起表現

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「MAGMAS」の共起表現一覧(1語右で並び替え)