plutonic rock sentence in Hindi
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- This section of the Churchill province was formerly called the Ennadai-Rankin greenstone belt and include the Kaminak, Yathkyed, MacQuoid and Rankin supracrustal belts, containing a wide range of intrusive Neoarchean plutonic rocks ranging in composition from gabbro to syenogranite.
- It is characteristic of the later volcanic rocks rich in alkalis, such as phonolite, nepheline-basalt, leucite basalt, etc ., and also of certain plutonic rocks of the nepheline syenite series, which are typically developed in southern Norway.
- An example of the mineral, which possesses strong magnetic properties is the mineral magnetite, lodestone, from Tortola, British Virgin Islands; found in igneous plutonic rocks formations, composed of several minerals, including quartz, plagicase, alkali feldspar, biotite and titanite.
- Formed at the initiative of the citizens of Rivi�re-?Pierre, interpretation center, which began operations in the summer of 2002, highlights the granite which is a plutonic rock composed of quartz, mica and feldspar crystallized in form of grains visible to the eye.
- "' Orbicular granite "'( also known as "'orbicular rock "'or "'orbiculite "') is an uncommon plutonic rock type which is usually spheroidal structures, probably formed through nucleation around a grain in a cooling magma chamber.
- Nearly all gabbros are found in plutonic bodies, but to restrict the term ( as the International Union of Geological Sciences, IUGS, suggests ) just to plutonic rocks is inappropriate, because gabbro may be found as a coarse-grained interior facies of certain thick lavas ( see, for example ).
- The term was originally defined by Stern et al . ( 1989 ) to refer to plutonic rocks containing between 55 and 60 weight percent SiO 2, with Mg # > 0.6, Ni > 100 ppm, Cr > 200 ppm, K 2 O > 1 weight percent, Rb / Sr 500 ppm, Sr > 500 ppm, enrichment in LEu anomalies.
- The Irumide Belt comprises deformed crystalline basement units dated at 2.7 Ga and between 2.05 and 1.93 Ga, unconformably and in places structurally overlain by a supracrustal sequence of shallow water quartzites and pelites, the Muva Supergroup, in which sparse volcanic tuffs have given ages of between 1.88 and 1.85 Ga . This complex is intruded by limited granitoids at ca . 1.66-1.55 Ga and an extensive suite of syn-orogenic plutonic rocks at between 1.05 and 1.00 Ga.
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