Mineralogy Database

X-Ray Diffraction Table

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Minerals Arranged by X-Ray Powder Diffraction

See Help on X-Ray Diffraction.

Powder X-ray Diffraction (XRD) is one of the primary techniques used by mineralogists and solid state chemists to examine the physico-chemical make-up of unknown materials. This data is represented in a collection of single-phase X-ray powder diffraction patterns for the three most intense D values in the form of tables of interplanar spacings (D), relative intensities (I/Io), mineral name and chemical formulae

The XRD technique takes a sample of the material and places a powdered sample in a holder, then the sample is illuminated with x-rays of a fixed wave-length and the intensity of the reflected radiation is recorded using a goniometer. This data is then analyzed for the reflection angle to calculate the inter-atomic spacing (D value in Angstrom units - 10-8 cm). The intensity(I) is measured to discriminate (using I ratios) the various D spacings and the results are compared to this table to identify possible matches. Note: 2 theta (Θ) angle calculated from the Bragg Equation, 2 Θ = 2(arcsin(n λ/(2d)) where n=1

For more information about this technique, see X-Ray Analysis of a Solid or take an internet course at Birkbeck College On-line Courses.  Many thanks to Frederic Biret for these data.

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Found 32 Records, Sorted by D1 using 1.54056 - CuKa1 for 2θ WHERE (d1 > 3.56916 AND d1 < 3.71484)
D1
Å (2θ)
I1
%)
D2
Å (2θ)
I2
(%)
D3
Å (2θ)
I3
(%)
Mineral Formula
3.582(24.84) 160 4.640(19.11) 160 3.488(25.52) 160 Felbertalite Cu2Pb6Bi8S19
3.592(24.77) 200 5.104(17.36) 160 5.746(15.41) 160 Ribbeite (Mn++,Mg)5(SiO4)2(OH)2
3.594(24.75) 200 2.650(33.80) 160 4.444(19.96) 160 Zoubekite AgPb4Sb4S10
3.596(24.74) 200 3.992(22.25) 160 6.886(12.85) 40 Ertixiite Na2Si4O9
3.598(24.72) 200 5.720(15.48) 160 5.196(17.05) 120 Alleghanyite Mn5(SiO4)2(OH)2
3.600(24.71) 200 4.040(21.98) 200 5.400(16.40) 200 Wilkmanite Ni3Se4
3.600(24.71) 200 3.550(25.06) 180 3.490(25.50) 160 Vincentite (Pd,Pt)3(As,Sb,Te)
3.602(24.70) 200 2.296(39.20) 140 5.960(14.85) 120 Sperrylite PtAs2
3.602(24.70) 200 5.890(15.03) 200 3.074(29.02) 180 Calzirtite CaZr3TiO9
3.608(24.65) 200 5.784(15.31) 200 7.414(11.93) 120 Nordenskioldine CaSnB2O6
3.612(24.63) 200 5.754(15.39) 180 5.368(16.50) 160 Leucophoenicite Mn7(SiO4)3(OH)2
3.612(24.63) 200 5.114(17.33) 200 5.738(15.43) 156 Jerrygibbsite (Mn,Zn)9(SiO4)4(OH)2
3.620(24.57) 200 6.540(13.53) 200 6.320(14.00) 180 Nasonite Pb6Ca4Si6O21Cl2
3.622(24.56) 200 5.288(16.75) 200 7.038(12.57) 200 Chernovite-(Y) YAsO4
3.626(24.53) 200 2.292(39.28) 180 5.980(14.80) 180 Tolovkite IrSbS
3.636(24.46) 200 6.240(14.18) 160 8.340(10.60) 160 Tungusite [Ca14(OH)8](Si8020)(Si8020)2[Fe++9(OH)14]
3.638(24.45) 200 4.480(19.80) 200 6.340(13.96) 200 Argentite Ag2S
3.640(24.43) 200 6.890(12.84) 178 3.976(22.34) 164 Rambergite MnS
3.656(24.33) 200 5.970(14.83) 140 4.744(18.69) 120 Djerfisherite K6Na(Fe,Cu,Ni)25S26Cl
3.660(24.30) 200 5.620(15.76) 200 6.180(14.32) 200 Plombierite Ca5H2Si6O18·6H2O
3.660(24.30) 200 5.780(15.32) 180 3.320(26.83) 160 Heazlewoodite Ni3S2
3.664(24.27) 200 5.860(15.11) 180 6.160(14.37) 160 Betekhtinite Cu10(Fe,Pb)S6
3.668(24.24) 200 4.386(20.23) 200 6.522(13.57) 180 Chukhrovite-(Y) Ca3(Y,Ce)Al2(SO4)F13·10(H2O)
3.670(24.23) 200 4.756(18.64) 180 5.992(14.77) 180 Owensite (Ba,Pb)6(Cu,Fe,Ni)25S27
3.676(24.19) 200 2.344(38.37) 190 1.858(48.99) 180 Kalungaite PdAsSe
3.678(24.18) 200 15.340(5.76) 200 4.680(18.95) 180 Chlormagaluminite (Mg,Fe++)4Al2(OH)12(Cl2,CO3)·2(H2O)
3.684(24.14) 200 5.274(16.80) 180 5.138(17.24) 160 Zirsinalite Na6(Ca,Mn,Fe++)Zr[Si6O18]
3.688(24.11) 200 6.120(14.46) 160 3.778(23.53) 120 Luobusaite Fe0.83Si2
3.698(24.05) 200 6.180(14.32) 160 9.200(9.61) 160 Caledonite Pb5Cu2(CO3)(SO4)3(OH)6
3.700(24.03) 200 5.260(16.84) 160 5.380(16.46) 160 Glaucochroite CaMnSiO4
3.708(23.98) 200 5.654(15.66) 200 6.028(14.68) 200 Saryarkite-(Y) Ca(Y,Th)Al5(SiO4)2(PO4,SO4)2(OH)7·6(H2O)
3.712(23.95) 200 5.600(15.81) 200 7.000(12.64) 200 Plattnerite PbO2

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