wulfenite sentence in Hindi
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- Secondary minerals consist of lead minerals like anglesite, cerussite, pyromorphite and wulfenite, and of iron sulfides like marcasite and pyrite.
- Associated secondary minerals include cerussite, phoenicochroite, vauquelinite, willemite, wulfenite, galena, sphalerite, pyrite, tennantite and chalcopyrite.
- The region is known for striking combinations of cerussite, fluorite, vanadinite, wulfenite, barite, and mimetite, as well as galenite and anglesite.
- A number of small mining districts are located in the hills around Villa Ahumada, and the area is noted for its crystal specimens of wulfenite and other minerals.
- Lesser known localities of wulfenite include : Sherman Tunnel, St . Peter s Dome, Tincup-Tomichi-Moncarch mining districts, Pride of America mine and Bandora mine in Colorado.
- When massicot is found in a natural environment, some other minerals that may be found with it may include cerussite, litharge, minium, wulfenite, oxides of antimony and limonite.
- It occurs in the oxidized zone of ore deposits and is associated with dioptase, wulfenite, hemihedrite, phoenicochroite, duftite, mimetite, shattuckite, chrysocolla, hemimorphite, willemite and fluorite.
- The structure of the wulfenite-" I " 4 1 / a system can be described as a close packing of tetrahedral MoO 4 2 " anions and Pb 2 + cations.
- The correct nomenclature of the 90 : 10 solid state is wulfenite-" I " 4 1 / a and the 64 : 36 solid state is wulfenite-" I " 4.
- The correct nomenclature of the 90 : 10 solid state is wulfenite-" I " 4 1 / a and the 64 : 36 solid state is wulfenite-" I " 4.
- The wulfenite found in this area is similar in properties ( paragenetic sequence, low silver and antimony contents of the galenas and absence of pyromorphite ) to the wulfenites of the Alps and may be similar in origin.
- The wulfenite found in this area is similar in properties ( paragenetic sequence, low silver and antimony contents of the galenas and absence of pyromorphite ) to the wulfenites of the Alps and may be similar in origin.
- The structure of wulfenite-" I " 4 is also very similar to that of wulfenite-" I " 4 1 / a but has an unequal distribution of tungsten and molybdenum which may explain the observed hemihedrism.
- The structure of wulfenite-" I " 4 is also very similar to that of wulfenite-" I " 4 1 / a but has an unequal distribution of tungsten and molybdenum which may explain the observed hemihedrism.
- An extensive solid solution exists between the two end members wulfenite and stolzite ( PbWO 4 ), such that tungstenian-wulfenite compositions range from 90 % wulfenite and 10 % stolzite to chillagite ( 64 % wulfenite, 36 % stolzite ) and so on.
- An extensive solid solution exists between the two end members wulfenite and stolzite ( PbWO 4 ), such that tungstenian-wulfenite compositions range from 90 % wulfenite and 10 % stolzite to chillagite ( 64 % wulfenite, 36 % stolzite ) and so on.
- An extensive solid solution exists between the two end members wulfenite and stolzite ( PbWO 4 ), such that tungstenian-wulfenite compositions range from 90 % wulfenite and 10 % stolzite to chillagite ( 64 % wulfenite, 36 % stolzite ) and so on.
- An extensive solid solution exists between the two end members wulfenite and stolzite ( PbWO 4 ), such that tungstenian-wulfenite compositions range from 90 % wulfenite and 10 % stolzite to chillagite ( 64 % wulfenite, 36 % stolzite ) and so on.
- Molybdenum can be extracted from wulfenite by crushing the ore to 60-80 mesh, mixing the ore with NaNO 3 or NaOH, heating the mixture to about 700 �C ( decomposing ), leaching with water, filtering, collecting the insoluble residues which may include Union Carbide and Carbon Corp.
- It is argued that no miscibility gap exists in the wulfenite-stolzite solid solution at room temperature due to the almost identical size and shape of the MoO 4 2 " and WO 4 2 " ions, however, arguments have been made for the existence of a miscibility gap at higher temperatures.
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