| 词条 | Raspite |
| 释义 |
| name = Raspite | boxwidth = | boxbgcolor = | image = Raspite-130810.jpg | imagesize = 260px | alt = | caption = | category = Oxide minerals | formula = PbWO4 | molweight = | strunz = 4.DG.20 | dana = | system = Monoclinic | class = Prismatic (2/m) (same H-M symbol) | symmetry = P21/b | unit cell = | color = | colour = | habit = | twinning = | cleavage = | fracture = | tenacity = | mohs = | luster = | streak = | diaphaneity = | gravity = | density = | polish = | opticalprop = | refractive = | birefringence = | pleochroism = | 2V = | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = | alteration = | other = | prop1 = | prop1text = | references = }}Raspite is a mineral, a lead tungstate; with the formula PbWO4. It forms yellow to yellowish brown monoclinic crystals.[1] It is the low temperature monoclinic dimorph of the tetragonal stolzite.[1][2] It was discovered in 1897 at Broken Hill, New South Wales, Australia, it was named for Charles Rasp (1846–1907), German-Australian prospector, discoverer of the Broken Hill ore deposit.[3] See also
References1. ^1 Handbook of Mineralogy {{Tungsten minerals}}{{Mineral-stub}}2. ^Mindat entry 3. ^{{citation | url = http://webmineral.com/data/Raspite.shtml | title = Raspite Mineral Data | work = Webmineral.com | accessdate = September 12, 2010}} 3 : Lead minerals|Tungstate minerals|Monoclinic minerals |
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