首页> 外文期刊>Journal of mineralogical and petrological sciences >Rhabdophane-(Y), YPO4·H2O, a new mineral in alkali olivine basalt from Hinodematsu, Genkai-cho, Saga Prefecture, Japan
【24h】

Rhabdophane-(Y), YPO4·H2O, a new mineral in alkali olivine basalt from Hinodematsu, Genkai-cho, Saga Prefecture, Japan

机译:日本佐贺县玄海町日出松的碱性橄榄石玄武岩中的新型矿物Rhabdophane-(Y),YPO 4 ·H 2 O

获取原文
       

摘要

Rhabdophane-(Y), ideal formulaYPO_(4)·H_(2)O, occurs in a druse of the Higashimatsuura basalt at Hinodematsu, Genkai-cho, Saga Prefecture, Japan. It occurs as short rod-like crystals and forms radial aggregates. Rhabdophane-(Y) is hexagonal, P 6_(2)22, a = 6.959(2) ?, c = 6.384(2) ?, V = 267.7(1) ?~(3), Z = 3. It is yellowish white to yellowish brown in color with a silky to dull luster. The density is 4.54 g/cm~(3) (calc.). The strongest lines in the X-ray powder diffraction pattern are [d (I /I _(0)) hkl ] 2.821 (100) 102, 3.013 (77) 200, 6.026 (76) 100, 4.385 (47) 101, 3.480 (44) 110, 2.127 (28) 003, and 1.854 (26) 212.
机译:Rhabdophane-(Y),理想的化学式YPO_(4)·H_(2)O,发生在日本佐贺县玄海町日松市的Hatsushimatsuura玄武岩中。它以短棒状晶体的形式出现并形成放射状聚集体。 Rhabdophane-(Y)是六角形的,P 6_(2)22,a = 6.959(2)α,c = 6.384(2)α,V = 267.7(1)α。 〜(3),Z = 3。其颜色为黄白色至黄棕色,具有丝般至暗淡的光泽。密度为4.54 g / cm〜(3)(计算)。 X射线粉末衍射图中最强的线是[d(i / I _(0))hkl] 2.821(100)102,3.013(77)200,6.026 (76)100、4.385(47)101、3.480(44)110、2.127(28)003和1.854(26)212。

著录项

相似文献

  • 外文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号