Noun:

ସାଧନ, ଅସ୍ତ୍ରଶସ୍ତ୍ର,

agmas's Usage Examples:

Quickly after the lunar crust formed, or even as it was forming, different types of magmas that would give rise to the Mg-suite norites and troctolites began to form, although the exact depths at which this occurred are not known precisely.

magma chambers where basaltic magmas differentiate into granites, or of cumulates produced by mafic crystals settling out of the magma.

It appears that the final KREEP-rich magmas of the magma ocean eventually became concentrated within the region of Oceanus Procellarum and the Imbrium basin, a unique geologic province that is now known as the Procellarum KREEP Terrane.

between igneous differentiation of mafic magmas and felsic or silica crust meltings.

More specifically, two different magmas with compositions akin.

Felsic magmas are thought to form by addition of heat or water vapor to rock of.

the category of medial magmas, also known as the medial category, and denoted Med, is the category whose objects are medial magmas (that is, sets with a.

Magma mixing between felsic rhyolitic and mafic basaltic magmas in a magma reservoir Partial melting of metasomatized.

backarc magmas of the Neuquén Basin: Geochemical consequences of slab shallowing and the westward drift of South America".

magnitude more viscous than basaltic magmas, making degassing and effusion more complicated.

mixing of different magmas, one of which in the case of Parinacota may be the Ajata magmas.

Effusive eruptions are most common in basaltic magmas, but they also occur in intermediate and felsic magmas.

When the parent magmas of basalts crystallize, they preferentially.