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首页> 外文期刊>The American mineralogist >Edgrewite Ca _9(SiO _4) _4F _2- hydroxyledgrewite Ca _9(SiO _4) _4(OH) _2, a new series of calcium humite-group minerals from altered xenoliths in the ignimbrite of Upper Chegem caldera, Northern Caucasus, Kabardino-Balkaria, Russia
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Edgrewite Ca _9(SiO _4) _4F _2- hydroxyledgrewite Ca _9(SiO _4) _4(OH) _2, a new series of calcium humite-group minerals from altered xenoliths in the ignimbrite of Upper Chegem caldera, Northern Caucasus, Kabardino-Balkaria, Russia

机译:钙铁矿Ca _9(SiO _4)_4F _2-羟基钙铁矿Ca _9(SiO _4)_4(OH)_2,这是一系列新的钙蒙脱石族矿物,其来自上Chegem破火山口,北高加索,卡巴尔达诺-巴尔卡尔里亚的火成岩中蚀变的异质岩中的钙腐殖质俄国

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Members of the edgrewite Ca _9(SiO _4) _4F _2-hydroxyledgrewite Ca9(SiO _4) _4(OH) _2 series, structural analogues of clinohumite-hydroxylclinohumite series, Mg _9(SiO _4) _4(F,OH) _2, were discovered in xenoliths of carbonate-silicate rock altered to skarn within ignimbrites of the Upper Chegem volcanic structure, Kabardino-Balkaria, Northern Caucasus, Russia. The new minerals occur sparingly in zones containing bultfonteinite, hillebrandite, jennite, and chegemite, as well as rare relics of larnite and rondorfite enclosed in a matrix of hydroxylellestadite. Edgrewite and hydroxyledgrewite are largely altered to jennite in places with admixed zeophyllite and trabzonite, and are preserved as elongate relics mostly 0.1-0.4 mm long in the central part of atoll-like pseudomorphs. The new minerals form a solid-solution series Ca9(SiO _4)4(F,OH)2, in which the content of the edgrewite end-member Ca 9_(SiO _4) _4F _2 ranges from 74% (F = 3.64 wt%) to 31% (F = 1.52 wt%). Structure refinement of crystals containing 51% and 37% of the edgrewite end-member gave, respectively, R _1 = 3.03%, space group P 2 _1/b11(no. 14), Z = 2, a = 5.06870(10), b = 11.35790(10), c = 15.4004(2) ?, α = 100.5980(10)°, V = 871.47(3) ?3; and R _1 = 1.61%, space group P2 1/b 11 (no. 14), Z = 2, a = 5.06720(10), b = 11.35450(10), c = 15.3941(2) ?, α = 100.5870(10)°, and V = 870.63(2) ? ~3. Minerals of the edgrewite-hydroxyledgrewite series are colorless, optically biaxial (+), 2V _(meas) = 80(5)°; 2V _(alc) = 78.7°; dispersion r > v, medium; orientation: Z = a, X ∧ c = 12(2)°; edgrewite: α = 1.621(2), β = 1.625(2),γ= 1.631(2); hydroxyledgrewite: α= 1.625(2),β= 1.629(2),γ= 1.635(2) (589 nm). The micro-hardness VHN _(50) = 352-366 kg/mm ~2 corresponds to the Mohs scale of 5.5-6. 5. FTIR spectra of edgrewite and hydroxyledgrewite show resolved bands at (edgrewite/ hydroxyledgrewite, cm ~(-1)):3558 and 3551 and 3543/3554, absent/3486, 1075/1075, 996/996, 980/982, 934/933, 917/918, 904/903, 890/884, 864/864, 842/842, 818/820. Raman spectra are characterized by the following bands (edgrewite/hydroxyledgrewite, cm ~(-1)) at: 921/923, 889/890, 839/840, and 815/814 (SiO _4 stretching), at: 556/559, 527/527, 423/419, 406/404, and 394/394 (SiO _4 bending), 309/295, 269/256, and 163/166 (CaO _6). In the OH stretching region three bands are noted at 3554, 3547, and 3540 cm~(-1) for edgrewite and two - 3550 and 3475 cm ~(-1) for hydroxyledgrewite confirming the corresponding IR spectra. The major difference in Raman and IR spectra of edgrewite and hydroxyledgrewite is the presence of two resolved peaks in the OH stretching region at ca. 3550 and 3480 cm ~(-1) for hydroxyledgrewite.
机译:发现了钙长辉石Ca _9(SiO _4)_4F _2-羟基ledgrewite Ca9(SiO _4)_4(OH)_2系列的成员,斜长石-羟基轻质斜长石系列的结构类似物Mg _9(SiO _4)_4(F,OH)_2。在俄罗斯北部高加索地区,上切格姆火山结构的火成岩中,碳酸盐-硅酸盐岩石的异岩中的矽卡岩变成了矽卡岩。新矿物很少出现在以下区域:含有方黄铁矿,山坡铁矿,软陶矿和白铁矿,以及被包裹在羟基硬石中的稀有的褐铁矿和锂铁矿遗迹。在混有沸石叶绿石和斜方岩的地方,辉绿岩和羟基辉绿岩在很大程度上被转变为菱镁矿,并被保存为长形文物,在环礁状假晶形的中央部分长约0.1-0.4毫米。新的矿物形成固溶体系列Ca9(SiO _4)4(F,OH)2,其中辉绿岩端基Ca 9_(SiO _4)_4F _2的含量为74%(F = 3.64 wt% )至31%(F = 1.52 wt%)。含有51%和37%的钙矾石端基的晶体的结构细化分别得出R _1 = 3.03%,空间群P 2 _1 / b11(编号14),Z = 2,a = 5.06870(10), b = 11.35790(10),c = 15.4004(2)θ,α= 100.5980(10)°,V = 871.47(3)θ3;和。并且R _1 = 1.61%,空间组P2 1 / b 11(编号14),Z = 2,a = 5.06720(10),b = 11.35450(10),c = 15.3941(2)α,α= 100.5870( 10)°,且V = 870.63(2)? 〜3。镁橄榄石-羟基ledgrewite系列的矿物是无色的,光学双轴(+),2V _(meas)= 80(5)°; 2V _(alc)= 78.7°;色散r> v,中等;方向:Z = a,X = c = 12(2)°;钙矾石:α= 1.621(2),β= 1.625(2),γ= 1.631(2);羟基水硬钙石:α= 1.625(2),β= 1.629(2),γ= 1.635(2)(589 nm)。显微硬度VHN _(50)= 352-366 kg / mm〜2对应于5.5-6的莫氏硬度。 5.褐铁矿和羟基褐铁矿的FTIR谱显示分辨的谱带为(褐铁矿/羟基灰石,cm〜(-1)):3558和3551和3543/3554,不存在/ 3486、1075 / 1075、996 / 996、980 / 982、934 / 933、917 / 918、904 / 903、890 / 884、864 / 864、842 / 842、818 / 820。拉曼光谱的特征是以下谱带(钙铝榴石/羟基水银榴石,cm〜(-1))位于:921 / 923、889 / 890、839 / 840和815/814(SiO_4拉伸),位于:556/559, 527 / 527、423 / 419、406 / 404和394/394(SiO _4弯曲),309 / 295、269 / 256和163/166(CaO _6)。在OH拉伸区域中,对于钙榴石,在3554、3547和3540 cm〜(-1)处观察到三个谱带,对于羟基榴石,在3550和3475 cm〜(-1)处看到三个谱带,从而确认了相应的红外光谱。钙铁矿和羟基钙铁矿在拉曼光谱和红外光谱上的主要区别在于,OH拉伸区中大约有两个解析峰存在。 3550和3480 cm〜(-1)用于羟基水铝石。

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