prehnite sentence in Hindi
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- Associated minerals are other zeolites, prehnite, calcite and quartz.
- It is an indicator mineral of the prehnite-pumpellyite metamorphic facies.
- Prehnite pseudomorphs after laumontite ( epimorphs ) have been found in India.
- Associated minerals include prehnite, scolecite and mesolite.
- Prehnite-pumpellyite facies to mid-amphibolite facies have been produced by metamorphism.
- Semi precious stones extracted are amethyst, epidote, garnet, prehnite, and quartz.
- It also occurs as cavity and vesicle fillings associated with prehnite, calcite, and zeolites.
- Mineral assemblages include kaolinite and montmorillonite with laumontite, wairakite, prehnite, calcite and chlorite.
- Less common minerals can include biotite, garnet, actinolite, epidote, chalcedony, prehnite, and wodginite.
- Extensive deposits of gem quality prehnite occur in the basalt tableland surrounding Wave Hill Station in the central Northern Territory, of Australia.
- Lower temperatures are transitional with and overlap the prehnite-pumpellyite facies and higher temperatures overlap with and include sub-amphibolite facies.
- High-ultrahigh pressure metamorphic path through the zeolite, prehnite-pumpellyite, blueschist, and eclogite facies stability zones of subducted oceanic crust.
- Zeolite and prehnite-pumpellyite facies assemblages may or may not be present, thus the onset of metamorphism may only be marked by blueschist facies conditions.
- If the illite crystallinity values fall in the 0.25-0.30 ?? range, it corresponds with a metamorphic high anchizone or prehnite-pumpellyite facies.
- If the illite crystallinity values fall in the 0.30-0.42 ?? range, it corresponds with a metamorphic low anchizone or prehnite-pumpellyite facies.
- It occurs as a primary mineral in nepheline syenites, within hydrothermal cavities in basalts and diabase and in serpentinites in association with zeolites, datolite, prehnite, calcite and serpentine.
- Typical glasses, notably formation of spherulites, of perlite, lithophysae, and low-temperature prehnite-pumpellyite facies sub-seafloor alteration is ubiquitous though often overprinted by later metamorphic events.
- They are found in serpentine and, especially where the lavas contain nepheline or leucite, are often rich in zeolites, such as analcite, prehnite, natrolite, scolecite, chabazite, heulandite, etc.
- As the rock enters the submetamorphic field, generally Zeolite facies metamorphism, clay minerals begin to recrystallize into low-temperature metamorphic phyllite minerals such as chlorite, prehnite, pumpellyite, glauconite and so forth.
- The sequence has been affected by very low grade metamorphism in the pumpellyite actinolite facies, with the development of the assemblage pumpellyite + actinolite + chlorite + sericite + albite + carbonate ?clinozoisite ?prehnite in the basic volcanics.
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