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首页> 外文期刊>Mineralogical Magazine >Paratooite-(La), a new lanthanum-dominant rare-earth copper carbonate from Paratoo, South Australia
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Paratooite-(La), a new lanthanum-dominant rare-earth copper carbonate from Paratoo, South Australia

机译:Paratooite-(La),一种来自南澳大利亚州Paratoo的新型镧为主的稀土碳酸铜

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Paratooite-(La) is a new lanthanum-dominant rare-earth copper carbonate from the Paratoo copper mine, near Yunta, Olary district, South Australia. Paratooite-(La) occurs as sheaves and radiating sprays of blade-like to tabular pale blue crystals in thin fissures in a slaty country rock. Individual crystals are typically 50-200 mu n in maximum dimension but < 5 mu m thick. Associated minerals include donnayite-(Y), kamphaugite-(Y), and bastnasite-(La). Electron microprobe and CHN analyses gave: La_2O_3 26.47; Pr_2O_3 7.74; Nd_2O_3 8.15; Sm_2O_3 0.66; Gd_2O_3 0.85; Y_2O_3 0.72; CaO 7.57; SrO 3.15; Na_2O 3.3; CuO 5.77; F 0.24; CO_2 32.05; NO_2 1.12; -O=F -0.10; sum 100.03, yielding an empirical formula of (La_(3.54)Ca_(2.94)Na_(2.32)Nd_(1.05)Pr_(1.03)Sr_(o.66)Y_(0.14)Gd_(0.10)Sm_(0.08))_(SIGMA 11.86)Cu_(1.58)(C_(15.84)N_(0.53))O_(47.76)F_(o 24) The simplified formula is (REE,Ca,Na,Sr)_6Cu(CO_3)_8 or possibly REE_3(Ca,Sr)_2NaCu(CO_3)_8. The mineral is pale turquoise-blue to pale blue in colour, transparent, with a pearly to vitreous lustre and a pale blue streak. No cleavage was observed but the morphology and TEM studies indicate a cleavage parallel to {100}. The Mohs hardness is estimated to be 4. The strongest lines in the X-ray powder pattern are [d_(obs) (I_(obs)) (hkl)]: 5.047 (53) (200); 4.786 (49) (021); 3.957 (43) (220); 3.468 (43) (012, 221); 2.927 (100) (202); 2.530 (52) (241); 2.344 (22) (420,103); 2.232 (20) (421). A synchrotron powder diffraction pattern was indexed on a primitive orthorhombic cell with a = 10.0862(5), b = 12.8088(6), c = 7.2360(4) A, V= 934.8(1) A~3 and Z= 2. The crystal structure of the new mineral could not be determined but powder diffraction data indicate the space group is probably P222, Pmmm, P222_1 or Pmm2. The measured density is 3.68(3) g/cm~3 and the calculated density is 3.78 g/cm~3. Paratooite-(La) is biaxial negative with a = 1.605(3), beta = 1.696(3) and gamma = 1.752(2); pleochroism is medium strong; X very pale bluish, Y and Z bluish (with greenish tint) with absorption Z approx = Y X. Paratooite-(La) is a supergene mineral which precipitated from mildly basic carbonated groundwaters. The mineral is named for the type locality.
机译:Paratooite-(La)是来自Paratoo铜矿的一种新的以镧为主的稀土碳酸铜,位于南澳大利亚Olary区Yunta附近。滑石-(La)发生在片状乡村岩石的细裂缝中,呈滑轮状并辐射出叶片状至片状淡蓝色晶体的放射状喷雾。单个晶体的最大尺寸通常为50-200微米,但厚度小于5微米。伴生矿物包括方铅矿-(Y),坎普陶土-(Y)和矿渣-(La)。电子探针和CHN分析得出:La_2O_3 26.47; Pr_2O_3 7.74; Nd_2O_3 8.15; Sm_2O_3 0.66; Gd_2O_3 0.85; Y_2O_3 0.72;氧化钙7.57; SrO 3.15; Na_2O 3.3;氧化铜5.77; F 0.24; CO_2 32.05; NO_2 1.12; -O = F -0.10;总和为100.03,得出(La_(3.54)Ca_(2.94)Na_(2.32)Nd_(1.05)Pr_(1.03)Sr_(o.66)Y_(0.14)Gd_(0.10)Sm_(0.08)_(( SIGMA 11.86)Cu_(1.58)(C_(15.84)N_(0.53))O_(47.76)F_(o 24)的简化公式是(REE,Ca,Na,Sr)_6Cu(CO_3)_8或可能是REE_3(Ca, Sr)_2NaCu(CO_3)_8。矿物为浅蓝绿色至浅蓝色,透明,具有珍珠色至玻璃光泽和淡蓝色条纹。没有观察到卵裂,但是形态和TEM研究表明与{100}平行的卵裂。莫氏硬度估计为4。X射线粉末图案中最强的线为[d_(obs)(I_(obs))(hkl)]:5.047(53)(200); 4.786(49)(021); 3.957(43)(220); 3.468(43)(012,221); 2.927(100)(202); 2.530(52)(241); 2.344(22)(420,103); 2.232(20)(421)。同步加速器粉末衍射图在原始斜方晶格上的索引为a = 10.0862(5),b = 12.8088(6),c = 7.2360(4)A,V = 934.8(1)A〜3和Z = 2。无法确定新矿物的晶体结构,但粉末衍射数据表明该空间群可能是P222,Pmmm,P222_1或Pmm2。实测密度为3.68(3)g / cm〜3,计算密度为3.78 g / cm〜3。 Paratooite-(La)是双轴负离子,a = 1.605(3),β= 1.696(3),γ= 1.752(2);多色性中等强; X呈淡蓝色,Y和Z呈蓝色(具有绿色),吸收率Z约等于Y X。滑石-(La)是一种超基因矿物,从温和碱性的碳酸盐地下水中析出。矿物以类型的局部性来命名。

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