greenschist वाक्य
उदाहरण वाक्य
मोबाइल
- All these minerals were altered during the greenschist facies retromorphism.
- The greenschist, whose colour comes from harbour wall, are now closed.
- 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.
- Incorporated at the base of the greenschist are limestone lenses containing upper Silurian conodonts.
- A shield is that part of the metamorphosed greenschist, amphibolite, and granulite facies.
- Oligoclase is also found in metamorphic rocks formed under transitional greenschist to amphibolite facies conditions.
- In greater detail the greenschist facies is subdivided into subgreenschist, lower and upper greenschist.
- 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.
- Oceanic basalts in the vicinity of mid-ocean ridges typically exhibit sub-greenschist alteration.
- Greenstone artefacts may be made of greenschist, chlorastrolite, chlorite, hornblende, or epidote.
- Marialite occurs in regional and contact metamorphism : marble, calcareous gneiss, granulite and greenschist.
- The Changchun Schist being mostly Greenschist is found on the western side and forms thick beds.
- Greenschist alteration is in keeping with the regional metamorphism that is characteristic of Welsh Neoproterozoic rocks.
- The Metasedimentary Belt is predominantly sedimentary and volcanic rocks which have undergone greenschist to granulite facies metamorphism.
- Gold is associated with silicic, kaolinitic, and pyritic alteration of greenschist-grade felsic metavolcanics.
- 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.
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