aplite sentence in Hindi
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- The essential components of aplites are quartz and alkali feldspar ( the latter usually orthoclase or microperthite ), microcline and albite.
- This may be seen in many granite intrusions where later aplite veins form a late-stage stockwork through earlier phases of the granite mass.
- These granitic rocks consist predominantly of quartz monzonite and granodiorite with local, minor, scattered bodies of granite, aplite, diorite and gabbro.
- If the pipe is volcanic, as some have suggested, then the rock filling it ( the " pseudo-aplite " ) is peculiar in the extreme.
- The occasional appearance of myrmekite ( mainly in the microgranites ) and the hematitization of the plagioclase in the aplites and in the red facies rocks points to metasomatic processes.
- These rocks consist of gneiss, and gneissic diorite and quartz diorite, intruded by irregular bodies of equigranular granitic rocks, predominantly quartz diorite and granodiorite, with accompanying pegmatite and aplite.
- Aplite and veins may intrude pegmatites and wall rocks adjacent to intrusions, creating a confused sequence of felsic intrusive apophyses ( thin branches or offshoots of igneous bodies ) within the aureole of some granites.
- Phenocrysts of feldspar occur occasionally and of quartz more seldom; but the relation of aplite to quartz-porphyry, granophyre and felsite is very close, as all these rocks have nearly the same chemical composition.
- Major port cargo include tobacco, tobacco products, textiles, newsprint, wastepaper, chemicals, steel, steel products, phosphates, forest products, machinery, project cargo, refractory, vehicles, pharmaceuticals, aplite and livestock.
- Located between the Chaparral Shear Zone on the south and the Mesa Butte Shear Zone on the north, there are light-colored granites ( Aplite to Granodiorite ), Diorite, Gabbro, Gneisses, Schists, Metasedimentary and Metavolcanic rocks.
- The remainder of the Early Paleoproterozoic granites, granitic pegmatites, aplites, and granodiorites & ndash; are parts of either younger plutons or dike swarms, that have intruded the Granite Gorge Metamorphic Suite, either contemporaneously with, or after they were metamorphosed.
- The aplites of granite areas, for example, are the last part of the magma to crystallize, and correspond in composition to the quartzo-feldspathic aggregates that fill up the spaces between the early-formed minerals in the main body of the rock.
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