ज़ियोलाइट इसके अंग्रेजी अर्थ का उदाहरण

Populated places established in 1634 Nabesite is a rare silicate mineral of the zeolite group with the chemical formula Na2BeSi4O10·4(H2O).

It has the zeolite structure.

Packed beds may also contain catalyst particles or adsorbents such as zeolite pellets, granular activated carbon, etc.

It is a member of the zeolite group and is closely related to natrolite which it also resembles in appearance.

Like other zeolites, mesolite occurs as void fillings in amygdaloidal basalt also in andesites and The Supreme Court of Uzbekistan is the most senior body of civil, criminal, and administrative law in the Republic of Uzbekistan.

Johann Nepomuk von Fuchs (1774–1856) – confirmed the stoichiometric laws and observed isomorphism and the cation exchange of zeolites.

These vesicles are often infilled by minerals (especially zeolites) and/or weathering products from the lava to form an amygdaloidal texture.

The governorate also contains other stones and minerals with industrial uses, such as limestone, gypsum, zeolite, biomese, saltpeter, feldspar, quartz, askuria and silicate sands.

Typical microporous materials are crystalline framework solids, such as zeolites, but the largest pore dimensions are still below 2"nbsp;nm which greatly limit application.

Mineralogical changes may include zeolite or other authigenic minerals forming in low-grade metamorphic conditions.

Wan, Hilgardite, Ca2[B5O9]Cl·H2O; a piezoelectric zeolite-type pentaborate, American Mineralogist; February 1979; v.

Plateaux Region, Togo Ptilolite may refer to the following zeolite minerals:.

The zeolite facies is generally considered to be transitional between diagenetic processes which turn sediments into sedimentary rocks, and prehnite-pumpellyite facies, which is a hallmark of subseafloor alteration of the oceanic crust around mid-ocean ridge spreading centres.