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- Q1070902 subject Q7174074.
- Q1070902 subject Q7174859.
- Q1070902 subject Q7215190.
- Q1070902 subject Q8445686.
- Q1070902 abstract "Buddingtonite is an ammonium feldspar with formula: NH4AlSi3O8 (note: some sources add 0.5H2O to the formula). It forms by hydrothermal alteration of primary feldspar minerals. It is an indicator of possible gold and silver deposits, as they can become concentrated by hydrothermal processes. It crystallizes in the monoclinic crystal system and is colorless to white with a vitreous luster. Its structure is analogous to that of high sanidine (KAlSi3O8). Buddingtonite has a hardness of 5.5 and a specific gravity of 2.32. Buddingtonite was discovered in 1964 at the Sulfur Bank mine near Clear Lake in Lake County, California (Erd et al., 1964). Clear Lake is at the north end of The Geysers geothermal area. It also occurs in the Tonopah, Nevada (Felzer et al., 1994) area and in hydrothermal areas in New Zealand (Yang et al., 2001) and Japan. It has also been reported from the sedimentary Phosphoria Formation in Idaho (Gulbrandsen, 1974), South Dakota (Solomon & Rossman, 1988), Wyoming, and Montana. It occurs in the oil shale deposit, near Proserpine, Queensland, Australia (Loughan, et al., 1983).It was named for Arthur Francis Buddington (1890–1980), a petrologist at Princeton University.".
- Q1070902 wikiPageWikiLink Q1090.
- Q1070902 wikiPageWikiLink Q10972285.
- Q1070902 wikiPageWikiLink Q1099503.
- Q1070902 wikiPageWikiLink Q11998326.
- Q1070902 wikiPageWikiLink Q1211.
- Q1070902 wikiPageWikiLink Q1212.
- Q1070902 wikiPageWikiLink Q1214.
- Q1070902 wikiPageWikiLink Q1221.
- Q1070902 wikiPageWikiLink Q156361.
- Q1070902 wikiPageWikiLink Q163082.
- Q1070902 wikiPageWikiLink Q17.
- Q1070902 wikiPageWikiLink Q170258.
- Q1070902 wikiPageWikiLink Q178977.
- Q1070902 wikiPageWikiLink Q190901.
- Q1070902 wikiPageWikiLink Q1987070.
- Q1070902 wikiPageWikiLink Q21578.
- Q1070902 wikiPageWikiLink Q221378.
- Q1070902 wikiPageWikiLink Q222814.
- Q1070902 wikiPageWikiLink Q36074.
- Q1070902 wikiPageWikiLink Q408.
- Q1070902 wikiPageWikiLink Q41472.
- Q1070902 wikiPageWikiLink Q426723.
- Q1070902 wikiPageWikiLink Q44497.
- Q1070902 wikiPageWikiLink Q624543.
- Q1070902 wikiPageWikiLink Q636340.
- Q1070902 wikiPageWikiLink Q664.
- Q1070902 wikiPageWikiLink Q709386.
- Q1070902 wikiPageWikiLink Q7174074.
- Q1070902 wikiPageWikiLink Q7174859.
- Q1070902 wikiPageWikiLink Q7215190.
- Q1070902 wikiPageWikiLink Q82480.
- Q1070902 wikiPageWikiLink Q8445686.
- Q1070902 wikiPageWikiLink Q897.
- Q1070902 wikiPageWikiLink Q898786.
- Q1070902 wikiPageWikiLink Q988827.
- Q1070902 name "Buddingtonite".
- Q1070902 type ChemicalSubstance.
- Q1070902 type Mineral.
- Q1070902 type ChemicalObject.
- Q1070902 type Thing.
- Q1070902 type Q7946.
- Q1070902 comment "Buddingtonite is an ammonium feldspar with formula: NH4AlSi3O8 (note: some sources add 0.5H2O to the formula). It forms by hydrothermal alteration of primary feldspar minerals. It is an indicator of possible gold and silver deposits, as they can become concentrated by hydrothermal processes. It crystallizes in the monoclinic crystal system and is colorless to white with a vitreous luster. Its structure is analogous to that of high sanidine (KAlSi3O8).".
- Q1070902 label "Buddingtonite".
- Q1070902 name "Buddingtonite".