1666:
1591:
2057:
1624:
2370:), the structure is more ordered, resulting in a higher degree of crystallinity and purer cookeite. However, this direct relationship between pressure and structure has been called into question by the discovery of several samples of different crystallinity in the same sample from a low-pressure zone. Cookeites from high pressure always exhibit a high degree of crystallinity, but ordered cookeites can also be found at low pressure. The low-crystallinity crystals assumed to be characteristic of low pressures simply haven't yet reached the
1940:
length of 1.66 Ă…. There are two T-O'-T layers in the r-cookeite: the first is located at the edge of the cell, around the (x, y, z=0) coordinate plane, and the second is located in the center of the cell, around the (x, y, z=1/2) coordinate plane. These two layers are identical and equivalent through the translatory mirror c with coordinates (x, y, z=1/4). Since the O' layer has only one vacant site in the cell, when the layers are stacked, the vacant sites of the two layers are shifted in the (
3808:
2120:
1775:
35:
1497:, cookeite is found in the phyllosilicate class (class 71), whose silicate layers are formed by six-membered rings with alternating 2:1 layers (two layers of T tetrahedra around a layer of O octahedra) and 1:1 layers (isolated layer of octahedra) (71.04), and more precisely in the chlorite group (71.04.01).
2015:
The cell parameter of cookeite IIa is half that of r-cookeite: the difference between these two structures is due to the stacking of the O and T-O'-T layers. Within the layers themselves, there is no notable structural difference between this cookeite and the r-cookeite. However, the dioctahedral O'
1939:
layers have a mixed occupancy of silicon and aluminum. The Al cations in the O' layers are symmetrically distributed over two non-equivalent sites, with an average Al-O bond length of 1.92 Ă…. The cations (Si,Al) layers are distributed over four non-equivalent sites, with an average (Si,Al)-O bond
1883:
connected by their edges. All octahedra are of mixed aluminum and lithium occupancy. O-layer cations are distributed over three non-equivalent sites by symmetry. Two-thirds of the sites are preferentially occupied by Al Ă 91 % (orange octahedrons in the figure opposite), a third of the sites
2390:
Since a perfect crystal is considered an ordered, infinite stack of atoms, the layers contain an infinite number of sites. However, these sites can be grouped into "symmetry-equivalent sites", i.e. the application of symmetry operations of the crystal space group on a particular site of the
1686:
of finding a certain chemical species there. For example, the trioctahedral O layer of r-cookeite shown above has three different sites, two of which are predominantly occupied by aluminum (orange octahedra) and the third by lithium (green octahedra). Similarly, the tetrahedral sites of the
460:
Cookeite is a white mineral with green, brown, golden, or pinkish hues of varying intensity. It occurs as pseudo-hexagonal crystals, spherules, radiated or fibrous aggregates. It has a pearly or silky sheen, and is transparent to translucent. It is flexible but inelastic, with perfect
1582:
a less dense layer of O' octahedra, only two-thirds of whose sites are occupied (dioctahedral layer). Unoccupied octahedral sites are called "vacant sites". This layer is surrounded by two layers of six-membered rings of aluminosilicate tetrahedra, noted T, to form T-O'-T
2365:
Pressure seems to have the greatest influence on the degree of crystallinity and composition of the cookeite. At low pressures, the stacking of layers is not very regular and the cookeite may contain many substitutional impurities. At higher pressures (above 10
2362:, tourmaline, and fluorite. It occurs at relatively low temperatures (between 150°C and 200°C) under hydrothermal conditions, after other minerals have formed in the breccia. The lithium in cookeite is the result of hydrothermal transport of magmatic fluids.
2016:
layers of cookeite IIa are all identical and ordered so as to have the vacant sites one above the other in the stacking direction of the layers, whereas in r-cookeite, due to the translatory mirror c, the vacant sites of the O' layers do not overlap.
1778:
Structure of the r-cookeite, projected along the b-direction (perspective view). Yellow: Si, orange: Al, green: Li, blue: O, grey: H. The six-membered ring structure of the T layers is particularly visible in the left-hand
1681:
to cell in a non-periodic fashion. For this reason, octahedral sites are referred to as "mixed occupancy" sites. The occupancy of a site by different chemical species is described by its occupancy percentages, i.e. by the
1676:
The O layer contains the metal cations Al and Li. The distribution of these cations is not ordered in the structure: octahedral sites can host either Al or Li, but the occupation of the sites by these cations varies from
1575:
There are two types of octahedral layers, denoted O and O', which differ in their degree of filling. Cookeites belong to the "di, trioctahedral" chlorites, i.e. they possess:
2909:
M. P. Mata, D. R. Peacor et al., "Polytypism of cookeite in low-grade metapelites of the
Cameros Basin, Spain: Lack of correlation of well-ordered polytypes with pressure",
3109:
1665:
1553:
or hydroxyl (OH) groups. The aluminosilicate layers contain an octahedrally coordinated aluminum layer and two aluminosilicate layers formed by six-membered (Si,Al)
3084:
2851:
J. Sejkora, P. Ondruš et al., "Supergene minerals at the Huber stock and Schnöd stock deposits, Krásno ore district, the
SlavkovskĂ˝ les area, Czech Republic",
3099:
1623:
3311:
2875:
S. K. Ren, R. A. Eggleton et al., "The formation of hydrothermal cookeite in the breccia pipes of the ardlethan tin field, New South Wales, Australia",
1590:
3244:
3089:
3778:
3707:
3475:
3334:
3264:
3783:
3548:
3505:
3194:
3149:
3139:
3064:
3044:
3588:
3583:
3573:
3490:
3219:
3164:
3750:
3745:
3722:
3495:
3437:
3422:
3392:
3292:
3254:
3124:
3094:
3059:
3029:
2892:
B. Goffé, J. M. Azañon et al., "Metamorphic cookeite in Alpine metapelites from Rif, northern
Morocco, and the Betic Chain, southern Spain",
3543:
3480:
3462:
3239:
3184:
3179:
3169:
3049:
2004:(Z = 2 form units per cell), with cell parameters = 5.14 Å, = 8.90 Å, = 14.15 Å, α = 90.55°, β = 96.2° and γ = 90° (cell volume V = 643.49
1757:
The stacking of layers is not identical in all cookeites: there are several polytypes, distinguished by the length of the stacking period (
3684:
3510:
3234:
3074:
2264:
3520:
3500:
3427:
3259:
3189:
3485:
3114:
2984:
2956:
2048:) plane with respect to the primitive conventional cell, makes it easier to compare its structure with that of monoclinic cookeites.
2914:
2668:
ICSD No. 203 212; L. Desgranges, G. Calvarin et al., "Interlayer interactions in M(OH)2: a neutron diffraction study of Mg(OH)2",
2754:
2716:
2948:
S. W. Bailey et J. S. Lister, "Structures, compositions, and X-ray diffraction identification of dioctahedral chlorites",
2593:
ICSD No. 9 368 ; V. A. Aleksandrova, V. A. Drits et al., "Structural features of dioctahedral one-packet chlorite",
2631:
Z. V. Vrublevskaja, I. S. Delitsin et al., "Cookeite with a perfect regular structure, formed by bauxite alteration",
2518:
2374:
equilibrium of ordered crystals, due to other factors such as deformation of the medium or the chemical environment.
2272:
2616:
685:
353:
109:
1856:
Its structure consists of an alternating stack of two types of layers, noted O and T-O'-T, parallel to the plane (
483:. It is also not very dense, with a measured density ranging from 2.58 to 2.69. Cookeite has a pale green to pink
2977:
2522:
3839:
1750:
layers. In cookeite, Li and Al cations take the place of Mg cations in brucite-type layers (O layers) and
2391:
asymmetric unit of the conventional lattice allows all other equivalent sites in the crystal to be found.
515:, has a molecular mass of 522.16 u, or 8.67 Ă— 10 kg. It is therefore composed of the following elements:
1494:
119:
3844:
2651:
B. E. Brown and S. W. Bailey, "Chlorite polytypism: I. Regular and semi-random one-layer structure",
134:
2332:
Cookeite is a product of silicate alteration. In low-grade metamorphic zones, it is associated with
3834:
2970:
2172:
357:
16:
Mineral species of the silicate group and the phyllosilicate subgroup, part of the chlorite family.
487:
along the X and Y axes, and is colorless to pale yellow along the Z axis. It has a white line and
2312:
2192:
2073:
Cookeite is often a product of the hydrothermal alteration of lithium-bearing minerals, such as
440:
2292:
1542:
473:
202:
192:
2863:
1888:
length is 1.95 Ă… for octahedra containing predominantly aluminum and 2.11 Ă… for the others.
1579:
a layer of O octahedra, with all sites occupied by metallic elements (trioctahedral layer);
389:
2152:
8:
3369:
2244:
385:
212:
2787:, vol. 32, no 5, september-october 2001, p. 413, 416-421 (ISSN 0026-4628, read online).
2611:
ICSD No. 83 765; H. Zheng et S. W. Bailey, "Refinement of the cookeite 'r' structure",
462:
397:
182:
2688:
ICSD No. 100 682; B. Perdikatsis and H. Burzlaff, "Strukturverfeinerung am Talk Mg3",
3154:
3009:
2897:
2750:
2712:
2697:
2575:
2514:
1534:
2350:
field in
Australia showed that cookeite forms in the porous interstices of granitic
1919:
containing exclusively aluminium, surrounded by two T layers of tetrahedrons (Si,Al)
2856:
2693:
2673:
2636:
2086:
1758:
689:
232:
172:
58:
2953:
2656:
2308:
3812:
3773:
3553:
2677:
436:
2729:
3598:
3229:
3214:
2993:
2484:
2371:
2288:
2216:
1511:
479:
Cookeite is a soft mineral, as its hardness only ranges from 2.5 to 3.5 on the
301:
129:
20:
2825:
Didier
Descouens, "La Cookéite: une chlorite rare, dans la Haute-Garonne", in
3828:
3788:
3760:
3249:
2268:
2144:
1885:
1569:
533:
429:
405:
253:
141:
2635:, vol. 60, nos 11-12, november-december 1975, p. 1041-1046 (ISSN 0003-004X,
2534:
John W. Anthony, Richard A. Bideaux, Kenneth W. Bladh and Monte C. Nichols,
2336:. In high-grade metamorphic zones, it is formed mainly by the alteration of
2056:
1671:
Aluminosilicate layer T-O'-T. The black circle indicates six-membered rings.
3768:
3611:
3606:
3407:
3316:
3302:
3282:
3129:
2938:, 1837–1868, John Wiley & Sons, New York (NY), 6th ed., 1134 p., p. 625
2615:, vol. 82, nos 9-10, september-october 1997, p. 1007-1013 (ISSN 0003-004X,
2333:
2316:
2240:
2148:
2012:. Its structure is noted as IIa in the nomenclature of chlorite polytypes.
1997:
488:
466:
417:
278:
2771:
1695:
rings are of mixed silicon and aluminum occupancy (yellow in the figure).
665:
The silicon in the silicate layers may be partly substituted by aluminum,
3702:
3674:
3621:
3578:
3534:
3412:
3397:
3387:
3349:
2880:
2766:
J. Hyrsl and A. Petrov, "Famous
Mineral Localities: Llallagua, Bolivia",
2359:
2196:
2028:
1683:
1565:
1515:
484:
444:
275:
265:
3442:
2860:
2796:
M. Jensen, "Mineralogy of the
Yaogangxian Mine, Hunan Province, China",
3730:
3646:
3631:
3558:
3417:
3402:
3382:
3344:
3224:
3209:
3199:
3144:
3119:
3104:
3069:
3054:
3024:
2800:, vol. 25, no 4, april 2009, p. 1-11, 14 (ISSN 0885-4327, read online).
2783:
J. A. Mandarino, "Abstracts of New
Mineral Descriptions (Department)",
2367:
2101:
2097:
2078:
2074:
1774:
1546:
480:
382:
2840:Étude minéralogique des pegmatites du champ de la Sahatany, Madagascar
2709:
2553:
688:, it belongs to the class of silicates (IX), more precisely micaceous
3735:
3712:
3694:
3679:
3669:
3661:
3636:
3616:
3568:
3515:
3470:
3452:
3432:
3354:
3326:
3174:
3159:
2344:
2168:
2113:
2082:
1811:, with Z=4 form units per conventional cell. Its cell parameters are
1678:
823:
670:
659:
647:
643:
576:
401:
361:
2842:, doctoral thesis from the Université Paul-Sabatier, Toulouse, 1986.
2424:=1) coordinate plane is part of the neighboring cell in the crystal.
2176:
3740:
3563:
3530:
3204:
3079:
3014:
2220:
2200:
2105:
592:
297:
2962:
1884:
contain 82 % of Li (green octahedra). The average (Al,Li)-OH
3651:
3447:
3377:
3359:
3339:
3039:
3034:
2355:
2351:
2337:
2320:
2140:
1993:
1846:
1699:
1698:
The structure of cookeite can be seen as an alternating stack of
651:
560:
544:
393:
321:
293:
222:
2060:
A thin layer of cookeite encircles a green elbaite at the base,
1783:
Cookeite "r" is a rare lithium-rich cookeite with the formula Al
3641:
3134:
3019:
2770:, vol. 37, no 2, march-april 2006, p. 117-162 (ISSN 0026-4628,
2711:, Th. Hahn, Kluwer Academic Publishers, 2005 (repr.), 5th ed. (
2109:
2093:
655:
608:
421:
2809:
2655:, vol. 47, 7-8, july-august 1962, p. 819-850 (ISSN 0003-004X,
2127:
2580:
2483:., vol. 10, no 4, December 1970, p. 636–647 (ISSN 0008-4476,
2248:
2224:
2061:
1538:
692:(9.E) composed of tetrahedral and octahedral lattices (9.EC)
666:
425:
2692:., vol. 156, 3-4, january 1981, p. 177-186 (ISSN 0044-2968,
2119:
3801:
Structural groups mainly; based on rruff.info/ima, modified
3287:
3274:
3001:
2814:. Maine Geological Survey, Dept. of Conservation (Augusta).
2287:
Tsarafara Sud, Sahatany valley, Sahatany pegmatite fields,
1751:
639:
470:
34:
2672:, vol. 52, no 1, february 1996, p. 82-86 (ISSN 0108-7681,
2019:
Note: there are two space groups in the triclinic system:
416:
The topotype deposit is located in the Mount Mica Quarry,
2347:
1702:-type layers and talc-type layers. Indeed, brucite Mg(OH)
1550:
320:. This soft, low-density mineral of variable color has a
2952:, vol. 37, no 3, June 1989, p. 193-202 (ISSN 0009-8604,
2896:, vol. 8, no 2, april 1996, p. 335-348 (ISSN 0935-1221,
2558:
2913:, vol. 89, no 10, 2004, p. 1510-1515 (ISSN 0003-004X,
1927:, structured in the form of six-membered rings (Si,Al)
270:
x = y: pale green to pink, z: colorless to pale yellow
2943:
Rock-forming minerals, vol. 3 : Sheet silicates
2941:
William
Alexander Deer, R. A. Howie and J. Zussman,
2092:
It is often associated with the following minerals:
364:. It forms at relatively low temperatures (below 200
2068:
2879:, vol. 26, june 1988, p. 407-412 (ISSN 0008-4476,
2479:P. ÄŚernĂ˝, "Compositional variations in cookeite",
2445:) creates its image by symmetry with coordinates (
1510:Cookeite generally crystallizes in the monoclinic
698:Members of micaceous phyllosilicate group 9.EC.55
39:Cookeite on quartz, Paris, Maine, topotype deposit
2855:, vol. 51, 1-2, 2006, p. 57-101 (ISSN 1210-8197,
2433:This mirror applied to a point with coordinates (
3826:
2749:, Munich, Christian Weise Verlag, 1992, 336 p. (
2036:, inducing an artificially doubled cell in the (
2400:Since a cell is defined by the coordinates 0 ≤
2123:Specimen from Couledoux, Haute-Garonne, France.
1911:, are made up of an O' layer of octahedrons AlO
1629:Dioctahedral layer O', of chemical composition
1596:Trioctahedral layer O, of chemical composition
450:
2978:
2936:The System of Mineralogy of James Dwight Dana
2597:, vol. 17, 1972, p. 456-461 (ISSN 0038-5638).
2536:The Handbook of Mineralogy: Silica, Silicates
2500:, vol. 41, 1866, p. 246-248 (ISSN 0002-9599).
1841:and β = 96,6° (unit cell volume V = 1 305,41
673:, with a fairly constant (Al,B,Be)/Si ratio.
300:and the phyllosilicate subgroup, part of the
2496:G. J. Brush, "On cookeite and jefferisite",
2475:
2473:
2008:). It has a volumetric mass density of 2,69
2000:has been described in triclinic space group
324:structure made up of alternating layers LiAl
2513:, Van Nostrand Reinhold Co., 1979, 229 p. (
2509:Richard Scott Mitchell, John Reese Henley,
2128:Productive deposits of remarkable specimens
638:Impurities often found in cookeite include
2985:
2971:
2945:, John Wiley & Sons, 1963, p. 131-163.
2570:
2568:
392:(1827-1894), an American mineralogist and
356:. Cookeite is often found as a product of
33:
2810:Vandall T. King; Eugene E. Foord (1994).
2538:, vol. II, Mineral Data Publishing, 1995.
2470:
1541:elements and aluminosilicate layers. The
1537:consists of a stack of layers containing
455:
376:
2647:
2645:
2548:
2546:
2544:
2118:
2055:
1891:The T-O'-T layers, with a composition Al
1879:, are made up of octahedrons (Al,Li)(OH)
1773:
2829:, no. 54, 1983, p. 31, (ISSN 0153-9167)
2565:
494:
3827:
476:(formation of thin sheets or flakes).
2966:
2886:
2642:
2627:
2625:
2541:
2412:< 1, the T-O'-T layer around the (
1871:The O layers, with a composition LiAl
1807:. It crystallizes in the space group
676:
2903:
2607:
2605:
2603:
2343:A study of samples collected in the
681:Cookeite is a polytype of chlorite.
521:Chemical composition of the mineral
2992:
2051:
2023:. The symmetry of this cookeite is
13:
2622:
1955:
1935:in which the tetrahedrons (Si,Al)O
1500:
381:Cookeite was described in 1866 by
14:
3856:
2600:
2511:Mineral names: what do they mean?
2327:
167:white, green, brown, golden, pink
3806:
2747:Die Mineralien des Schwarzwaldes
2143:mine in the Krunkelbach valley,
2069:Gîtology and associated minerals
1664:
1622:
1589:
491:creamy-yellow fairly regularly.
2928:
2869:
2845:
2832:
2819:
2803:
2790:
2777:
2760:
2739:
2722:
2702:
2682:
2662:
2427:
2394:
2384:
1960:A cookeite with the formula (Al
1545:of the metallic elements is an
499:Cookeite, with the formula LiAl
2698:10.1524/zkri.1981.156.3-4.177)
2587:
2528:
2503:
2490:
1568:. The layers are connected by
435:Type samples are deposited at
1:
2934:Edward Salisbury Dana (1892)
2464:
1769:
2736:(Retrieved July 20th, 2011).
2562:(Retrieved July 20th, 2011).
2552:Jolyon Ralph and Ida Chau, "
368:°C) and variable pressures.
7:
2923:
2584:(Retrieved July 1st, 2011).
1766:for monoclinic cookeites).
1505:
451:Physico-chemical properties
411:
360:alteration of silicates in
10:
3861:
3110:Fluorotetraferriphlogopite
2678:10.1107/S0108768195008275)
2595:Soviet. Phys. Crystallogr.
2581:http://euromin.w3sites.net
2029:unconventional space group
1495:Dana Classification System
371:
258:biaxial (+), 0,0170–0,0240
18:
3797:
3759:
3721:
3693:
3660:
3597:
3529:
3461:
3368:
3325:
3301:
3273:
3000:
2670:Acta Crystallogr. Sect. B
2027:; its description in the
711:
708:
705:
702:
697:
626:Total : 35 elements
520:
274:
264:
252:
231:
221:
211:
201:
191:
181:
171:
163:
158:
140:
128:
118:
108:
57:
49:
44:
32:
27:
2377:
2167:Siglo Veinte (XX) mine,
2085:, and can also occur in
632:Total : 100 %
1847:volumetric mass density
1549:, whose vertices are O
1543:coordination polyhedron
686:Strunz's classification
304:, with the formula LiAl
3085:Ferroaluminoceladonite
2574:The EUROMIN project, "
2124:
2089:in the primary state.
2065:
1780:
629:Total : 522,16 u
456:Determination criteria
377:Inventor and etymology
2730:Cookeite Mineral Data
2559:http://www.mindat.org
2307:Huber Stock, Krásno,
2293:Antananarivo province
2122:
2059:
1777:
110:Strunz classification
2064:-colored at the top.
1687:six-membered (Si,Al)
539:% of molecular mass
495:Chemical composition
447:, USA (No. 2.3728).
390:Josiah Parsons Cooke
3840:Monoclinic minerals
3813:Minerals portal
3100:Fluorokinoshitalite
2853:J. Czech Geol. Soc.
2812:Mineralogy of Maine
2734:Mineralogy Database
2354:containing quartz,
2239:Mount Mica quarry,
1714:layers, and talc Mg
1258:(Fe,Mg,Al,Fe,Ti,Mn)
1049:Franklinfurnaceite
386:George Jarvis Brush
120:Dana classification
2358:(such as pyrite),
2215:Yaogangxian Mine,
2125:
2087:hydrothermal veins
2066:
1781:
677:Crystallochemistry
398:Harvard University
187:perfect over {001}
3822:
3821:
3312:Ferripyrophyllite
3155:Manganiceladonite
3010:Aluminoceladonite
2861:10.3190/JCGS.989,
2827:Monde et minéraux
2755:978-3-921656-24-2
2717:978-0-470-68908-0
2153:Baden-WĂĽrttemberg
1992:from the Djalair
1759:lattice parameter
1561:rings of (Si,Al)O
1491:
1490:
1354:pseudo-hexagonal
1185:pseudo-hexagonal
636:
635:
529:Number (formula)
388:and dedicated to
287:
286:
283:cream yellow (SW)
227:from 2.58 to 2.69
3852:
3845:Lithium minerals
3811:
3810:
3809:
3245:Tetraferriannite
3105:Fluorophlogopite
2987:
2980:
2973:
2964:
2963:
2918:
2907:
2901:
2894:Eur. J. Mineral.
2890:
2884:
2873:
2867:
2849:
2843:
2836:
2830:
2823:
2817:
2815:
2807:
2801:
2794:
2788:
2781:
2775:
2764:
2758:
2743:
2737:
2726:
2720:
2706:
2700:
2686:
2680:
2666:
2660:
2649:
2640:
2629:
2620:
2609:
2598:
2591:
2585:
2572:
2563:
2550:
2539:
2532:
2526:
2507:
2501:
2498:Amer. Jour. Sci.
2494:
2488:
2477:
2458:
2431:
2425:
2408:< 1, and 0 ≤
2398:
2392:
2388:
2052:Mineral deposits
2011:
2007:
1852:
1844:
1840:
1830:
1820:
1668:
1658:
1657:
1656:
1648:
1647:
1639:
1638:
1626:
1616:
1615:
1614:
1606:
1605:
1593:
1526:(monoclinic) or
1472:
1471:
1470:
1462:
1461:
1453:
1452:
1444:
1443:
1435:
1434:
1403:
1402:
1401:
1393:
1392:
1384:
1383:
1375:
1374:
1349:
1348:
1347:
1339:
1338:
1330:
1329:
1321:
1320:
1294:
1293:
1292:
1284:
1283:
1275:
1274:
1266:
1265:
1234:
1233:
1232:
1224:
1223:
1215:
1214:
1206:
1205:
1180:
1179:
1178:
1170:
1169:
1144:
1142:
1141:
1133:
1132:
1124:
1123:
1098:
1097:
1096:
1088:
1087:
1079:
1078:
1070:
1069:
1061:
1060:
1029:
1028:
1027:
1019:
1018:
987:
986:
985:
977:
976:
968:
967:
959:
958:
925:
924:
923:
915:
914:
906:
905:
897:
896:
865:
864:
863:
855:
854:
846:
845:
837:
836:
802:
801:
800:
792:
791:
783:
782:
774:
773:
765:
764:
739:
738:
737:
729:
728:
695:
694:
518:
517:
367:
233:Refractive index
104:
103:
102:
94:
93:
85:
84:
76:
75:
64:
63:(repeating unit)
37:
25:
24:
3860:
3859:
3855:
3854:
3853:
3851:
3850:
3849:
3835:Phyllosilicates
3825:
3824:
3823:
3818:
3807:
3805:
3793:
3774:Franklinphilite
3755:
3717:
3689:
3656:
3593:
3554:Montmorillonite
3525:
3457:
3364:
3321:
3297:
3269:
3090:Ferroceladonite
2996:
2994:Phyllosilicates
2991:
2950:Clays Clay Min.
2931:
2926:
2921:
2908:
2904:
2891:
2887:
2874:
2870:
2850:
2846:
2837:
2833:
2824:
2820:
2808:
2804:
2795:
2791:
2782:
2778:
2765:
2761:
2744:
2740:
2727:
2723:
2707:
2703:
2687:
2683:
2667:
2663:
2650:
2643:
2630:
2623:
2610:
2601:
2592:
2588:
2573:
2566:
2551:
2542:
2533:
2529:
2508:
2504:
2495:
2491:
2478:
2471:
2467:
2462:
2461:
2432:
2428:
2399:
2395:
2389:
2385:
2380:
2330:
2217:Xian de Yizhang
2173:Rafael Bustillo
2130:
2116:and tourmaline.
2071:
2054:
2009:
2005:
1991:
1987:
1983:
1979:
1975:
1971:
1967:
1963:
1958:
1956:Other cookeites
1938:
1934:
1930:
1926:
1922:
1918:
1914:
1910:
1906:
1902:
1898:
1894:
1882:
1878:
1874:
1850:
1842:
1838:
1828:
1818:
1806:
1802:
1798:
1794:
1790:
1786:
1772:
1749:
1745:
1741:
1737:
1733:
1729:
1725:
1721:
1717:
1713:
1709:
1705:
1694:
1690:
1672:
1669:
1660:
1655:
1652:
1651:
1650:
1646:
1643:
1642:
1641:
1637:
1634:
1633:
1632:
1630:
1627:
1618:
1613:
1610:
1609:
1608:
1604:
1601:
1600:
1599:
1597:
1594:
1564:
1560:
1556:
1508:
1503:
1501:Crystallography
1469:
1466:
1465:
1464:
1460:
1457:
1456:
1455:
1451:
1448:
1447:
1446:
1442:
1439:
1438:
1437:
1433:
1430:
1429:
1428:
1426:
1400:
1397:
1396:
1395:
1391:
1388:
1387:
1386:
1382:
1379:
1378:
1377:
1373:
1370:
1369:
1368:
1366:
1346:
1343:
1342:
1341:
1337:
1334:
1333:
1332:
1328:
1325:
1324:
1323:
1319:
1316:
1315:
1314:
1312:
1309:Orthochamosite
1291:
1288:
1287:
1286:
1282:
1279:
1278:
1277:
1273:
1270:
1269:
1268:
1264:
1261:
1260:
1259:
1257:
1231:
1228:
1227:
1226:
1222:
1219:
1218:
1217:
1213:
1210:
1209:
1208:
1204:
1201:
1200:
1199:
1197:
1177:
1174:
1173:
1172:
1168:
1165:
1164:
1163:
1161:
1140:
1137:
1136:
1135:
1131:
1128:
1127:
1126:
1122:
1119:
1118:
1117:
1115:
1095:
1092:
1091:
1090:
1086:
1083:
1082:
1081:
1077:
1074:
1073:
1072:
1068:
1065:
1064:
1063:
1059:
1056:
1055:
1054:
1052:
1026:
1023:
1022:
1021:
1017:
1014:
1013:
1012:
1010:
984:
981:
980:
979:
975:
972:
971:
970:
966:
963:
962:
961:
957:
954:
953:
952:
950:
922:
919:
918:
917:
913:
910:
909:
908:
904:
901:
900:
899:
895:
892:
891:
890:
888:
862:
859:
858:
857:
853:
850:
849:
848:
844:
841:
840:
839:
835:
832:
831:
830:
828:
799:
796:
795:
794:
790:
787:
786:
785:
781:
778:
777:
776:
772:
769:
768:
767:
763:
760:
759:
758:
756:
736:
733:
732:
731:
727:
724:
723:
722:
720:
690:phyllosilicates
679:
514:
510:
506:
502:
497:
458:
453:
437:Yale University
414:
379:
374:
365:
352:having several
351:
347:
343:
339:
335:
331:
327:
319:
315:
311:
307:
302:chlorite family
296:species of the
259:
244:= 1,579–1,584,
240:= 1,572–1,576,
147:
101:
98:
97:
96:
92:
89:
88:
87:
83:
80:
79:
78:
74:
71:
70:
69:
67:
62:
61:
40:
23:
17:
12:
11:
5:
3858:
3848:
3847:
3842:
3837:
3820:
3819:
3817:
3816:
3802:
3798:
3795:
3794:
3792:
3791:
3786:
3781:
3779:Lennilenapeite
3776:
3771:
3765:
3763:
3761:Stilpnomelanes
3757:
3756:
3754:
3753:
3748:
3743:
3738:
3733:
3727:
3725:
3719:
3718:
3716:
3715:
3710:
3708:Ferrisepiolite
3705:
3699:
3697:
3691:
3690:
3688:
3687:
3682:
3677:
3672:
3666:
3664:
3658:
3657:
3655:
3654:
3649:
3644:
3639:
3634:
3629:
3624:
3619:
3614:
3609:
3603:
3601:
3595:
3594:
3592:
3591:
3586:
3581:
3576:
3571:
3566:
3561:
3556:
3551:
3546:
3540:
3538:
3527:
3526:
3524:
3523:
3518:
3513:
3508:
3503:
3498:
3493:
3488:
3483:
3478:
3476:Brinrobertsite
3473:
3467:
3465:
3459:
3458:
3456:
3455:
3450:
3445:
3440:
3435:
3430:
3425:
3420:
3415:
3410:
3405:
3400:
3395:
3390:
3385:
3380:
3374:
3372:
3366:
3365:
3363:
3362:
3357:
3352:
3347:
3342:
3337:
3335:Bismutoferrite
3331:
3329:
3323:
3322:
3320:
3319:
3314:
3308:
3306:
3299:
3298:
3296:
3295:
3290:
3285:
3279:
3277:
3271:
3270:
3268:
3267:
3265:Yangzhumingite
3262:
3257:
3252:
3247:
3242:
3237:
3232:
3230:Siderophyllite
3227:
3222:
3217:
3215:Polylithionite
3212:
3207:
3202:
3197:
3192:
3187:
3182:
3177:
3172:
3167:
3162:
3157:
3152:
3147:
3142:
3137:
3132:
3127:
3122:
3117:
3112:
3107:
3102:
3097:
3092:
3087:
3082:
3077:
3072:
3067:
3062:
3057:
3052:
3047:
3042:
3037:
3032:
3027:
3022:
3017:
3012:
3006:
3004:
2998:
2997:
2990:
2989:
2982:
2975:
2967:
2961:
2960:
2946:
2939:
2930:
2927:
2925:
2922:
2920:
2919:
2902:
2885:
2868:
2844:
2838:N. Ranorosoa,
2831:
2818:
2802:
2789:
2776:
2759:
2745:Kurt Walenta,
2738:
2721:
2701:
2681:
2661:
2641:
2621:
2599:
2586:
2564:
2540:
2527:
2502:
2489:
2468:
2466:
2463:
2460:
2459:
2426:
2393:
2382:
2381:
2379:
2376:
2329:
2328:Mineral growth
2326:
2325:
2324:
2311:, district de
2304:
2303:
2301:Czech Republic
2297:
2296:
2289:Vakinankaratra
2284:
2283:
2277:
2276:
2260:
2259:
2253:
2252:
2236:
2235:
2229:
2228:
2212:
2211:
2205:
2204:
2188:
2187:
2181:
2180:
2164:
2163:
2157:
2156:
2137:
2136:
2129:
2126:
2070:
2067:
2053:
2050:
1989:
1985:
1981:
1977:
1973:
1969:
1965:
1961:
1957:
1954:
1936:
1932:
1928:
1924:
1920:
1916:
1912:
1908:
1904:
1900:
1896:
1892:
1880:
1876:
1872:
1804:
1800:
1796:
1792:
1788:
1784:
1771:
1768:
1747:
1743:
1739:
1735:
1731:
1730:consists of Mg
1727:
1723:
1719:
1715:
1711:
1707:
1706:consists of Mg
1703:
1692:
1688:
1674:
1673:
1670:
1663:
1661:
1653:
1644:
1635:
1628:
1621:
1619:
1611:
1602:
1595:
1588:
1585:
1584:
1580:
1570:hydrogen bonds
1562:
1558:
1554:
1512:crystal system
1507:
1504:
1502:
1499:
1489:
1488:
1479:
1473:
1467:
1458:
1449:
1440:
1431:
1424:
1420:
1419:
1410:
1404:
1398:
1389:
1380:
1371:
1364:
1360:
1359:
1356:
1350:
1344:
1335:
1326:
1317:
1310:
1306:
1305:
1300:
1295:
1289:
1280:
1271:
1262:
1255:
1251:
1250:
1241:
1235:
1229:
1220:
1211:
1202:
1195:
1191:
1190:
1187:
1181:
1175:
1166:
1159:
1155:
1154:
1148:
1145:
1138:
1129:
1120:
1113:
1109:
1108:
1102:
1099:
1093:
1084:
1075:
1066:
1057:
1050:
1046:
1045:
1036:
1030:
1024:
1015:
1008:
1004:
1003:
994:
988:
982:
973:
964:
955:
948:
942:
941:
932:
926:
920:
911:
902:
893:
886:
882:
881:
872:
866:
860:
851:
842:
833:
826:
820:
819:
810:
804:
797:
788:
779:
770:
761:
754:
750:
749:
743:
740:
734:
725:
718:
714:
713:
710:
707:
704:
700:
699:
678:
675:
634:
633:
630:
627:
624:
621:
620:
617:
614:
611:
605:
604:
601:
598:
595:
589:
588:
585:
582:
579:
573:
572:
569:
566:
563:
557:
556:
553:
550:
547:
541:
540:
537:
530:
527:
523:
522:
512:
508:
504:
500:
496:
493:
457:
454:
452:
449:
413:
410:
378:
375:
373:
370:
349:
345:
341:
337:
333:
329:
325:
317:
313:
309:
305:
298:silicate group
285:
284:
281:
272:
271:
268:
262:
261:
260:2V = 35 to 60°
256:
250:
249:
235:
229:
228:
225:
219:
218:
215:
209:
208:
205:
199:
198:
195:
189:
188:
185:
179:
178:
175:
169:
168:
165:
161:
160:
159:Identification
156:
155:
144:
138:
137:
132:
130:Crystal system
126:
125:
122:
116:
115:
112:
106:
105:
99:
90:
81:
72:
65:
55:
54:
51:
47:
46:
42:
41:
38:
30:
29:
21:Chlorite group
19:Main article:
15:
9:
6:
4:
3:
2:
3857:
3846:
3843:
3841:
3838:
3836:
3833:
3832:
3830:
3815:
3814:
3803:
3800:
3799:
3796:
3790:
3789:Stilpnomelane
3787:
3785:
3784:Parsettensite
3782:
3780:
3777:
3775:
3772:
3770:
3767:
3766:
3764:
3762:
3758:
3752:
3749:
3747:
3744:
3742:
3739:
3737:
3734:
3732:
3729:
3728:
3726:
3724:
3720:
3714:
3711:
3709:
3706:
3704:
3701:
3700:
3698:
3696:
3692:
3686:
3683:
3681:
3678:
3676:
3673:
3671:
3668:
3667:
3665:
3663:
3659:
3653:
3650:
3648:
3645:
3643:
3640:
3638:
3635:
3633:
3630:
3628:
3625:
3623:
3620:
3618:
3615:
3613:
3610:
3608:
3605:
3604:
3602:
3600:
3596:
3590:
3587:
3585:
3582:
3580:
3577:
3575:
3572:
3570:
3567:
3565:
3562:
3560:
3557:
3555:
3552:
3550:
3549:Ferrosaponite
3547:
3545:
3542:
3541:
3539:
3536:
3532:
3528:
3522:
3519:
3517:
3514:
3512:
3509:
3507:
3506:Lunijianlaite
3504:
3502:
3499:
3497:
3494:
3492:
3489:
3487:
3484:
3482:
3479:
3477:
3474:
3472:
3469:
3468:
3466:
3464:
3460:
3454:
3451:
3449:
3446:
3444:
3441:
3439:
3436:
3434:
3431:
3429:
3426:
3424:
3421:
3419:
3416:
3414:
3411:
3409:
3406:
3404:
3401:
3399:
3396:
3394:
3391:
3389:
3386:
3384:
3381:
3379:
3376:
3375:
3373:
3371:
3367:
3361:
3358:
3356:
3353:
3351:
3348:
3346:
3343:
3341:
3338:
3336:
3333:
3332:
3330:
3328:
3324:
3318:
3315:
3313:
3310:
3309:
3307:
3304:
3300:
3294:
3291:
3289:
3286:
3284:
3281:
3280:
3278:
3276:
3272:
3266:
3263:
3261:
3258:
3256:
3253:
3251:
3250:Trilithionite
3248:
3246:
3243:
3241:
3238:
3236:
3233:
3231:
3228:
3226:
3223:
3221:
3218:
3216:
3213:
3211:
3208:
3206:
3203:
3201:
3198:
3196:
3195:Oxyphlogopite
3193:
3191:
3188:
3186:
3183:
3181:
3178:
3176:
3173:
3171:
3168:
3166:
3163:
3161:
3158:
3156:
3153:
3151:
3150:Luanshiweiite
3148:
3146:
3143:
3141:
3140:Kinoshitalite
3138:
3136:
3133:
3131:
3128:
3126:
3123:
3121:
3118:
3116:
3113:
3111:
3108:
3106:
3103:
3101:
3098:
3096:
3093:
3091:
3088:
3086:
3083:
3081:
3078:
3076:
3073:
3071:
3068:
3066:
3065:Chromphyllite
3063:
3061:
3058:
3056:
3053:
3051:
3048:
3046:
3045:Boromuscovite
3043:
3041:
3038:
3036:
3033:
3031:
3028:
3026:
3023:
3021:
3018:
3016:
3013:
3011:
3008:
3007:
3005:
3003:
2999:
2995:
2988:
2983:
2981:
2976:
2974:
2969:
2968:
2965:
2958:
2955:
2951:
2947:
2944:
2940:
2937:
2933:
2932:
2916:
2912:
2906:
2899:
2895:
2889:
2882:
2878:
2877:Can. Mineral.
2872:
2865:
2862:
2858:
2854:
2848:
2841:
2835:
2828:
2822:
2813:
2806:
2799:
2793:
2786:
2780:
2773:
2769:
2763:
2756:
2752:
2748:
2742:
2735:
2731:
2725:
2718:
2714:
2710:
2705:
2699:
2695:
2691:
2685:
2679:
2675:
2671:
2665:
2658:
2654:
2648:
2646:
2638:
2634:
2628:
2626:
2618:
2614:
2608:
2606:
2604:
2596:
2590:
2583:
2582:
2577:
2571:
2569:
2561:
2560:
2555:
2549:
2547:
2545:
2537:
2531:
2524:
2520:
2519:0-442-24593-9
2516:
2512:
2506:
2499:
2493:
2486:
2482:
2476:
2474:
2469:
2456:
2452:
2448:
2444:
2440:
2436:
2430:
2423:
2419:
2415:
2411:
2407:
2403:
2397:
2387:
2383:
2375:
2373:
2372:thermodynamic
2369:
2363:
2361:
2357:
2353:
2349:
2346:
2341:
2339:
2335:
2322:
2318:
2314:
2310:
2309:HornĂ Slavkov
2306:
2305:
2302:
2299:
2298:
2294:
2290:
2286:
2285:
2282:
2279:
2278:
2274:
2270:
2269:Haute-Garonne
2266:
2262:
2261:
2258:
2255:
2254:
2250:
2246:
2242:
2238:
2237:
2234:
2233:United States
2231:
2230:
2226:
2222:
2218:
2214:
2213:
2210:
2207:
2206:
2202:
2198:
2194:
2193:Lac-du-Bonnet
2190:
2189:
2186:
2183:
2182:
2178:
2174:
2170:
2166:
2165:
2162:
2159:
2158:
2154:
2150:
2146:
2145:Menzenschwand
2142:
2139:
2138:
2135:
2132:
2131:
2121:
2117:
2115:
2111:
2107:
2103:
2099:
2095:
2090:
2088:
2084:
2080:
2076:
2063:
2058:
2049:
2047:
2046:
2041:
2040:
2035:
2034:
2030:
2026:
2022:
2017:
2013:
2003:
1999:
1995:
1953:
1951:
1950:
1945:
1944:
1889:
1887:
1869:
1867:
1866:
1861:
1860:
1854:
1848:
1836:
1835:
1826:
1825:
1816:
1815:
1810:
1776:
1767:
1765:
1764:
1760:
1755:
1754:(O' layers).
1753:
1701:
1696:
1685:
1680:
1667:
1662:
1625:
1620:
1592:
1587:
1586:
1581:
1578:
1577:
1576:
1573:
1571:
1567:
1552:
1548:
1544:
1540:
1536:
1531:
1530:(triclinic).
1529:
1525:
1521:
1517:
1513:
1498:
1496:
1493:According to
1487:
1483:
1480:
1478:
1474:
1425:
1422:
1421:
1418:
1414:
1411:
1409:
1405:
1365:
1362:
1361:
1357:
1355:
1352:orthorhombic
1351:
1311:
1308:
1307:
1304:
1301:
1299:
1296:
1256:
1253:
1252:
1249:
1245:
1242:
1240:
1236:
1196:
1193:
1192:
1188:
1186:
1183:orthorhombic
1182:
1160:
1157:
1156:
1152:
1149:
1146:
1114:
1111:
1110:
1106:
1103:
1100:
1051:
1048:
1047:
1044:
1040:
1037:
1035:
1031:
1009:
1006:
1005:
1002:
998:
995:
993:
989:
949:
947:
944:
943:
940:
936:
933:
931:
927:
887:
884:
883:
880:
876:
873:
871:
867:
827:
825:
822:
821:
818:
814:
811:
809:
805:
755:
753:Borocookeite
752:
751:
747:
744:
741:
719:
717:Baileychlore
716:
715:
701:
696:
693:
691:
687:
684:According to
682:
674:
672:
668:
663:
661:
657:
653:
649:
645:
641:
631:
628:
625:
623:
622:
619:55,15 %
618:
615:
612:
610:
607:
606:
602:
599:
596:
594:
591:
590:
587:25,84 %
586:
583:
580:
578:
575:
574:
571:16,14 %
570:
567:
564:
562:
559:
558:
555:1, 33 %
554:
551:
548:
546:
543:
542:
538:
535:
532:Atomic mass (
531:
528:
525:
524:
519:
516:
492:
490:
486:
482:
477:
475:
472:
468:
464:
448:
446:
442:
438:
433:
431:
427:
423:
419:
409:
407:
406:Massachusetts
403:
399:
395:
391:
387:
384:
369:
363:
359:
355:
323:
303:
299:
295:
291:
282:
280:
277:
273:
269:
267:
263:
257:
255:
254:Birefringence
251:
247:
243:
239:
236:
234:
230:
226:
224:
220:
217:pearly; silky
216:
214:
210:
206:
204:
200:
196:
194:
190:
186:
184:
180:
176:
174:
170:
166:
162:
157:
154:
150:
145:
143:
142:Crystal class
139:
136:
133:
131:
127:
123:
121:
117:
113:
111:
107:
66:
60:
56:
52:
48:
43:
36:
31:
26:
22:
3804:
3769:Bannisterite
3723:Pyrosmalites
3626:
3612:Borocookeite
3607:Baileychlore
3589:Yakhontovite
3584:Volkonskoite
3574:Swinefordite
3491:Hydrobiotite
3408:Cronstedtite
3317:Pyrophyllite
3303:Pyrophyllite
3283:Minnesotaite
3220:Preiswerkite
3165:Masutomilite
3130:Hendricksite
2949:
2942:
2935:
2929:Bibliography
2911:Am. Mineral.
2910:
2905:
2893:
2888:
2876:
2871:
2852:
2847:
2839:
2834:
2826:
2821:
2811:
2805:
2798:Mineral News
2797:
2792:
2784:
2779:
2767:
2762:
2746:
2741:
2733:
2724:
2708:
2704:
2689:
2684:
2669:
2664:
2653:Am. Mineral.
2652:
2633:Am. Mineral.
2632:
2613:Am. Mineral.
2612:
2594:
2589:
2579:
2557:
2535:
2530:
2510:
2505:
2497:
2492:
2481:Can. Mineral
2480:
2454:
2450:
2446:
2442:
2438:
2434:
2429:
2421:
2417:
2413:
2409:
2405:
2404:< 1, 0 ≤
2401:
2396:
2386:
2364:
2348:stanniferous
2342:
2334:pyrophyllite
2331:
2317:Karlovy Vary
2315:, région de
2300:
2280:
2256:
2232:
2208:
2191:Tanco Mine,
2184:
2160:
2149:Black Forest
2133:
2091:
2072:
2044:
2043:
2038:
2037:
2032:
2031:
2024:
2020:
2018:
2014:
2001:
1998:Central Asia
1959:
1948:
1947:
1942:
1941:
1890:
1870:
1864:
1863:
1858:
1857:
1855:
1833:
1832:
1823:
1822:
1813:
1812:
1808:
1782:
1762:
1761:
1756:
1697:
1675:
1574:
1532:
1527:
1523:
1519:
1509:
1492:
1485:
1481:
1476:
1416:
1412:
1407:
1353:
1302:
1297:
1247:
1243:
1238:
1184:
1150:
1112:Glagolevite
1104:
1042:
1038:
1033:
1000:
996:
991:
945:
938:
934:
929:
885:Clinochlore
878:
874:
869:
816:
812:
807:
745:
712:Space group
709:Point group
683:
680:
664:
637:
603:1,54 %
498:
478:
459:
434:
415:
383:mineralogist
380:
358:hydrothermal
289:
288:
279:fluorescence
245:
241:
237:
152:
148:
3751:Schallerite
3746:Pyrosmalite
3703:Falcondoite
3675:Chrysocolla
3622:Clinochlore
3579:Vermiculite
3535:vermiculite
3496:Karpinskite
3463:Corrensites
3438:Manandonite
3423:Guidottiite
3413:Fraipontite
3398:Caryopilite
3393:Brindleyite
3388:Berthierine
3370:Serpentines
3350:Hisingerite
3293:Willemseite
3255:Voloshinite
3125:Gorbunovite
3095:Fluorannite
3060:Chernykhite
3030:Balestraite
2954:read online
2915:read online
2898:read online
2881:read online
2864:read online
2772:read online
2690:Z. Kristall
2657:read online
2637:read online
2617:read online
2523:read online
2485:read online
2360:cassiterite
2263:Goutasson,
2197:Bernic Lake
2179:department.
2079:tourmalines
2077:or certain
1996:deposit in
1684:probability
1516:space group
1363:Pennantite
1053:Ca(Fe,Al)Mn
1007:Donbassite
803:(x ≤ 0,33)
485:pleochroism
467:{001} plane
445:Connecticut
322:crystalline
276:Ultraviolet
266:Pleochroism
248:= 1,589–1,6
124:71.04.01.02
3829:Categories
3731:Friedelite
3695:Sepiolites
3662:Allophanes
3647:Pennantite
3632:Donbassite
3559:Nontronite
3544:Beidellite
3481:Corrensite
3418:Greenalite
3403:Chrysotile
3383:Antigorite
3345:Halloysite
3327:Kaolinites
3240:Tainiolite
3225:Roscoelite
3210:Phlogopite
3200:Paragonite
3185:Norrishite
3180:Nanpingite
3170:Montdorite
3145:Lepidolite
3120:Glauconite
3070:Clintonite
3055:Celadonite
3050:Bramallite
3025:Aspidolite
2465:References
2453:+1/2, 1/2-
2281:Madagascar
2251:(topotype)
2175:province,
2102:microcline
2098:lepidolite
2083:pegmatites
2075:lepidolite
1845:) and its
1770:Cookeite r
1566:tetrahedra
1547:octahedron
1313:(Fe,Mg,Fe)
1198:(Ni,Mg,Fe)
1158:Gonyerite
829:(Fe,Mg,Fe)
489:fluoresces
481:Mohs scale
362:pegmatites
146:prismatic;
135:monoclinic
3736:Mcgillite
3713:Sepiolite
3685:Neotocite
3680:Imogolite
3670:Allophane
3637:Gonyerite
3617:Chamosite
3599:Chlorites
3569:Sauconite
3531:Smectites
3516:Saliotite
3511:Rectorite
3471:Aliettite
3453:Pecoraite
3433:Lizardite
3355:Kaolinite
3235:Suhailite
3175:Muscovite
3160:Margarite
3075:Eastonite
2785:Min. Rec.
2768:Min. Rec.
2525:), p. 15.
2345:Ardlethan
2273:Occitania
2265:Couledoux
2169:Llallagua
2114:spodumene
1837:= 28,498
1535:structure
824:Chamosite
671:beryllium
660:potassium
648:magnesium
644:manganese
577:Aluminium
471:micaceous
441:New Haven
402:Cambridge
354:polytypes
3741:Nelenite
3627:Cookeite
3564:Saponite
3521:Tosudite
3501:Kulkeite
3443:NĂ©pouite
3428:Kellyite
3260:Wonesite
3205:Phengite
3190:Orlovite
3080:Ephesite
3015:Anandite
2924:Appendix
2576:Cookeite
2554:Cookeite
2356:sulfides
2352:breccias
2247:County,
2221:Chenzhou
2201:Manitoba
2106:petalite
1849:is 2,66
1827:= 8,940
1817:= 5,158
1539:metallic
1506:Overview
1423:Sudoite
1358:unknown
1254:Odinite
1189:unknown
946:Cookeite
706:Formula
703:Mineral
593:Hydrogen
561:Silicium
526:Element
474:fracture
463:cleavage
424:County,
412:Topotype
290:Cookeite
203:Tenacity
197:flexible
193:Fracture
183:Cleavage
173:Twinning
114:09.EC.55
50:Category
28:Cookeite
3652:Sudoite
3486:Dozyite
3448:Odinite
3378:Amesite
3360:Nacrite
3340:Dickite
3115:Garmite
3040:Biotite
3035:Bityite
2957:archive
2338:kyanite
2321:Bohemia
2313:Sokolov
2161:Bolivia
2141:Uranium
2134:Germany
1994:bauxite
1700:brucite
1583:layers.
1518:can be
1436:(Al,Fe)
1267:(Si,Al)
1194:Nimite
990:2 or 2/
889:(Mg,Fe)
721:(Zn,Al)
652:calcium
616:287,99
584:134,91
545:Lithium
465:on the
394:chemist
372:History
294:mineral
223:Density
177:around
59:Formula
45:General
3642:Nimite
3537:family
3305:series
3135:Illite
3020:Annite
2753:
2732:", in
2715:
2578:", in
2556:", in
2517:
2449:+1/2,
2257:France
2245:Oxford
2185:Canada
2177:PotosĂ
2110:quartz
2094:albite
1791:Li)(Si
1779:layer.
1551:anions
1514:. Its
1340:(OH,O)
1171:(OH,O)
1125:(OH,O)
997:C1, C2
856:(OH,O)
793:(OH,F)
658:, and
656:sodium
609:Oxygen
568:84,26
422:Oxford
366:
332:and Al
213:Luster
3275:Talcs
3002:Micas
2378:Notes
2249:Maine
2241:Paris
2225:Hunan
2209:China
2081:, in
2062:mauve
1986:10,35
1726:)(OH)
1376:Al(Si
1322:Al(Si
1207:Al(Si
898:Al(Si
838:Al(Si
667:boron
600:8,06
552:6,94
426:Maine
418:Paris
292:is a
164:Color
151:2 or
3533:and
3288:Talc
2751:ISBN
2713:ISBN
2515:ISBN
2010:g/cm
1990:7,65
1988:(OH)
1976:)(Si
1974:1,96
1970:0,65
1968:)(Li
1966:0,13
1962:1,85
1915:(OH)
1899:(OH)
1886:bond
1875:(OH)
1851:g/cm
1803:(OH)
1797:0,96
1793:3,04
1752:talc
1738:(OH)
1679:cell
1649:(OH)
1607:(OH)
1598:LiAl
1533:Its
1463:(OH)
1394:(OH)
1385:Al)O
1331:Al)O
1285:(OH)
1225:(OH)
1216:Al)O
1116:NaMg
1089:(OH)
1020:(OH)
978:(OH)
969:Al)O
951:LiAl
916:(OH)
907:Al)O
847:Al)O
775:(BSi
762:1+3x
730:(OH)
640:iron
511:(OH)
507:Al)O
469:and
340:(OH)
328:(OH)
316:(OH)
312:Al)O
95:(OH)
86:Al)O
68:LiAl
2857:doi
2694:doi
2674:doi
2368:bar
2199:),
1982:0,6
1978:3,4
1952:).
1868:).
1787:(Al
1718:(Si
1454:AlO
1263:2,5
999:or
960:(Si
771:4-x
669:or
613:18
503:(Si
430:USA
396:at
308:(Si
207:2,5
77:(Si
3831::
2959:).
2917:).
2900:).
2883:).
2866:).
2774:).
2757:).
2659:).
2644:^
2639:).
2624:^
2619:).
2602:^
2567:^
2543:^
2521:,
2487:).
2472:^
2457:).
2441:,
2437:,
2420:,
2416:,
2340:.
2319:,
2291:,
2271:,
2267:,
2243:,
2223:,
2219:,
2171:,
2151:,
2147:,
2112:,
2108:,
2104:,
2100:,
2096:,
2042:,
2033:C1
2025:P1
2021:P1
2002:C1
1984:)O
1980:Al
1972:Al
1964:Fe
1946:,
1933:18
1925:10
1909:12
1903:Si
1862:,
1853:.
1831:,
1821:,
1809:Cc
1801:10
1799:)O
1795:Al
1748:12
1742:Si
1724:10
1710:OH
1693:18
1631:Al
1572:.
1559:18
1528:C1
1524:Cc
1522:,
1520:C2
1484:2/
1475:2/
1459:10
1445:Si
1427:Mg
1415:2/
1406:2/
1390:10
1367:Mn
1336:10
1303:Cm
1246:2/
1237:2/
1221:10
1162:Mn
1153:1
1147:1
1134:·H
1107:2
1101:2
1085:10
1071:Si
1062:Zn
1041:2/
1032:2/
1011:Al
1001:Cc
974:10
937:2/
928:2/
912:10
877:2/
868:2/
852:10
815:2/
806:2/
789:10
784:)O
766:Al
757:Li
748:1
742:1
662:.
654:,
650:,
646:,
642:,
597:8
581:5
565:3
549:1
536:)
509:10
443:,
439:,
432:.
428:,
420:,
408:.
404:,
400:,
350:12
344:Si
314:10
153:Cc
91:10
53:IX
2986:e
2979:t
2972:v
2859::
2816:.
2728:"
2719:)
2696::
2676::
2455:z
2451:y
2447:x
2443:z
2439:y
2435:x
2422:z
2418:y
2414:x
2410:z
2406:y
2402:x
2366:k
2323:.
2295:.
2275:.
2227:.
2203:.
2195:(
2155:.
2045:b
2039:É‘
2006:Ă…
1949:b
1943:a
1937:4
1931:O
1929:6
1923:O
1921:4
1917:2
1913:4
1907:O
1905:8
1901:2
1897:4
1895:O
1893:2
1881:6
1877:6
1873:2
1865:b
1859:É‘
1843:Ă…
1839:Ă…
1834:c
1829:Ă…
1824:b
1819:Ă…
1814:É‘
1805:8
1789:2
1785:2
1763:c
1746:O
1744:8
1740:2
1736:4
1734:O
1732:2
1728:2
1722:O
1720:4
1716:3
1712:6
1708:3
1704:2
1691:O
1689:6
1659:.
1654:2
1645:4
1640:O
1636:2
1617:.
1612:6
1603:2
1563:4
1557:O
1555:6
1486:m
1482:C
1477:m
1468:8
1450:3
1441:3
1432:2
1417:m
1413:C
1408:m
1399:8
1381:3
1372:5
1345:8
1327:3
1318:5
1298:m
1290:4
1281:5
1276:O
1272:2
1248:m
1244:C
1239:m
1230:8
1212:3
1203:5
1176:8
1167:3
1151:C
1143:O
1139:2
1130:8
1121:6
1105:C
1094:8
1080:O
1076:2
1067:2
1058:4
1043:m
1039:C
1034:m
1025:8
1016:2
992:m
983:8
965:3
956:4
939:m
935:C
930:m
921:8
903:3
894:5
879:m
875:C
870:m
861:8
843:3
834:5
817:m
813:C
808:m
798:8
780:3
746:C
735:8
726:3
534:u
513:8
505:3
501:4
348:O
346:8
342:2
338:4
336:O
334:2
330:6
326:2
318:8
310:3
306:4
246:Îł
242:β
238:α
149:C
100:8
82:3
73:4
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