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greenschist facies वाक्य

"greenschist facies" हिंदी मेंgreenschist facies in a sentence
उदाहरण वाक्यमोबाइल
  • All these minerals were altered during the greenschist facies retromorphism.
  • The slates are highly cleaved and metamorphosed as high as lower greenschist facies.
  • They consist of interlayered sedimentary and volcanic flow rocks metamorphosed to low greenschist facies.
  • In greater detail the greenschist facies is subdivided into subgreenschist, lower and upper greenschist.
  • The greenstone belts of the various archean cratons are commonly altered to the greenschist facies.
  • These rocks therefore underwent chlorite ( chloritization ) indicating retrograde metamorphism under greenschist facies conditions.
  • The chloritization of the biotite is a clear sign for retrograde metamorphic overprinting under greenschist facies conditions.
  • The ophiolites of the Zermatt-Saas zone are mostly ultramafic rocks with greenschist facies mineralogy : serpentinites.
  • Regional metamorphism has converted the shale to a low greenschist facies, where clay is converted to chlorite.
  • The sedimentary rocks that were laid down in the basin are often weakly metamorphic ( greenschist facies ).
  • The metapelites are of granulite facies and the ultramafics are of greenschist facies and the enclosing gneisses represent amphibolites facies.
  • Illite crystallinity can be used to trace the low grade metamorphic transition from zeolite facies to greenschist facies ( diagenetic zone to epizone ).
  • It is often found in minute micaceous aggregates ( with individual plates barely visible ), as a major component of chromium rich greenschist facies.
  • If the illite crystallinity values fall in the 0-0.25 ?? range, it corresponds with a metamorphic epizone or greenschist facies.
  • Thus, metamorphic assemblages of ultramafic rocks containing anthophyllite are indicative of at least greenschist facies metamorphism in the presence of carbon dioxide bearing metamorphic fluids.
  • If burial continues along Barrovian Sequence metamorphic trajectories, greenschist facies gives rise to amphibolite facies assemblages, dominated by amphibole and eventually to granulite facies.
  • In the east side of the Cullarin Block, in the east-pointing finger of the ACT, the Tabberabberan Orogeny also reached the upper greenschist facies again.
  • Tremolite occurs as a result of contact metamorphism of calcium and magnesium rich siliceous sedimentary rocks and in greenschist facies metamorphic rocks derived from ultramafic or magnesium carbonate bearing rocks.
  • The original 20 30 m thick Homestake Formation, has been deformed and metamorphosed, resulting in upper greenschist facies of siderite-phyllite, and lower amphibolite facies of grunerite schists.
  • The deposits show evidence of an Early Cretaceous, amphibolite facies event and a younger, mid-Cretaceous lower greenschist facies event which resulted from the accretion of the Yukon-Tanana Terrane.
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