Adjective:

গ্রানাইটজাতীয়,

granitoid's Usage Examples:

A granitoid is a generic term for a diverse collection of coarse-grained igneous rocks that consist predominantly of quartz, plagioclase, and alkali feldspar.

The Kola-Belomorian gneiss and Karelian granitoid-greenstone terrane both formed during this time.

volcanic rocks, but also includes ultramafic rocks, mafic intrusions, granitoid rocks, and early and middle Precambrian sediments.

sand in the Llano Uplift, Texas, with granite outcrops Grus sand and the granitoid it’s derived from The central Australian inselberg Uluru (Ayers Rock).

6 Ga by the emplacement of major granitoid batholiths that thickened and stabilised the continental crust during.

The Spawning Lake Stock is an Archean age granitoid stock in Northeastern Ontario, Canada, located in Briggs Township and Chambers Township of Temagami.

orogeny is associated with intense igneous activity that produced large granitoid plutons.

Andesite – An intermediate volcanic rock Alkali feldspar granite – A granitoid in which at least 90% of the total feldspar is alkali feldspar Anorthosite –.

Chambers-Strathy Batholith, also called the Strathy-Chambers Batholith, is a large granitoid batholith complex in the Temagami region of Northeastern Ontario, Canada.

range is also known as the South Mountain Batholith, the largest body of granitoid rocks in the entire Appalachians and comprises both granite barrens and.

Paleoproterozoic domains made of greenstone belts, sedimentary basins, regional granitoid-tonalite-trondhjemite-granodiorite (TTG) plutons, and large shear zones.

of the Churchill Craton with many remnants of Archean supracrustal and granitoid rocks.

succession of volcanic and sedimentary rocks, surrounded on all sides by granitoid plutons which range in age from >3547 to <3225 Ma.

These rocks are chiefly granitoids and migmatitic gneiss.

Vaasa granite is a migmatitic Paleoproterozoic garnet-bearing granitoid with variable amounts of gneissose enclaves.

it is part of the Mercantour-Argentera massif, and is mostly formed by granitoid gneiss.

A large magmatic, granitoid forming event during the orogeny produced rocks with unusually similar.

It is one of the three separate granitoid intrusions that constitute the Temagami Greenstone Belt, consisting of.

The topography of the land is rough and hilly, featuring large granitoid tors and associated boulders.