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Sillimanite

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refractories or 55–60% alumina bricks. However, it has mostly been replaced by the other aluminosilicate polymorphs, andalusite and kyanite, for this purpose. As of 1998, sillimanite was just 2% of all aluminosilicate mineral production in the western world.
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Colourless or white to grey, also brown, yellow, yellow-green, grey-green, blue-green, blue; colourless in thin section
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Whitney, D.L. (2002). "Coexisting andalusite, kyanite, and sillimanite: Sequential formation of three Al
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or even by the naked eye. Both the fibrous and traditional forms of sillimanite are common in
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polymorphs during progressive metamorphism near the triple point, Sivrihisar, Turkey".
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indicating high temperature but variable pressure. Example rocks include
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Delaware State Mineral, Sillimanite, Delaware Geological Survey
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Gilchrist, J.D. (1977). "Alumino-Silicate Refractories".
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http://rruff.geo.arizona.edu/doclib/hom/sillimanite.pdf
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Natural sillimanite is used in the manufacture of high
812:"Delaware State Mineral – Delaware Geological Survey" 731:. Essex: Longman Scientific & Technical. p.  420:. Sillimanite is named after the American chemist 722: 902: 790:Klein, Cornelis and Cornelius S. Hurlbut, Jr., 727:Atlas of rock-forming minerals in thin section 451:. A common variety of sillimanite is known as 691: 689: 364: 27: 836: 649: 436:Sillimanite or fibrolite is one of three 706: 704: 755: 723:MacKenzie, W. S.; Guilford, C. (1980). 686: 903: 478:. It occurs with andalusite, kyanite, 355: 348: 341: 869: 701: 518:are similar mineral species found in 175:Prismatic crystals, fibrous, acicular 879:Geological Survey of Norway Bulletin 784: 626:"IMA–CNMNC approved mineral symbols" 623: 711:http://www.mindat.org/min-3662.html 599:List of minerals named after people 13: 847:10.1016/B978-0-08-020430-7.50027-X 606:, which is also called "fibrolite" 308:Colourless to pale brown to yellow 14: 947: 839:Fuels, Furnaces and Refractories 575: 560: 334: 228:Vitreous to subadamantine, silky 152:c = 5.75 Å; Z = 4 863: 830: 804: 749: 716: 666: 617: 535:Delaware Mineralogical Society 525:Sillimanite has been found in 1: 794:1985, Wiley 20th ed., p. 380 610: 431: 7: 587: 531:New Castle County, Delaware 10: 952: 926:Minerals in space group 62 553: 248:Transparent to translucent 322: 312: 302: 292: 270: 262: 252: 242: 232: 222: 209: 199: 189: 179: 169: 161: 156: 140: 128: 113: 101: 91: 81: 71: 50: 40: 35: 26: 21: 870:Ihlen, Peter M. (2000). 567:Silimanite crystal from 540: 698:Handbook of Mineralogy 630:Mineralogical Magazine 443:, the other two being 921:Orthorhombic minerals 792:Manual of Mineralogy, 766:American Mineralogist 83:Strunz classification 778:10.2138/am-2002-0404 582:Fibrolite micrograph 426:Chester, Connecticut 16:Nesosilicate mineral 936:Symbols of Delaware 931:Industrial minerals 651:10.1180/mgm.2021.43 642:2021MinM...85..291W 624:Warr, L.N. (2021). 506:and also rarely in 376:Phase diagram of Al 93:Dana classification 911:Aluminium minerals 674:"WebMineral entry" 527:Brandywine Springs 480:potassium feldspar 263:Optical properties 150:, b = 7.66 Å 119:Dipyramidal (mmm) 464:sedimentary rocks 422:Benjamin Silliman 329: 328: 298:δ = 0.020 – 0.022 284:= 1.654 – 1.670 n 280:= 1.653 – 1.661 n 943: 895: 894: 892: 890: 876: 867: 861: 860: 834: 828: 826: 824: 823: 814:. Archived from 808: 802: 788: 782: 781: 753: 747: 746: 730: 720: 714: 708: 699: 693: 684: 683: 681: 680: 670: 664: 663: 653: 621: 594:List of minerals 579: 564: 410:chemical formula 387:aluminosilicates 368: 360: 353: 346: 338: 272:Refractive index 254:Specific gravity 215: 57: 56:(repeating unit) 31: 19: 18: 951: 950: 946: 945: 944: 942: 941: 940: 901: 900: 899: 898: 888: 886: 874: 868: 864: 857: 835: 831: 821: 819: 810: 809: 805: 789: 785: 763: 759: 754: 750: 743: 721: 717: 709: 702: 694: 687: 678: 676: 672: 671: 667: 622: 618: 613: 604:Asbestos cement 590: 583: 580: 571: 565: 556: 543: 438:aluminosilicate 434: 419: 415: 403:aluminosilicate 392: 391: 390: 384: 383: 379: 375: 370: 369: 362: 361: 356: 354: 349: 347: 342: 339: 288:= 1.669 – 1.684 287: 283: 279: 213: 151: 124:: (2/m 2/m 2/m) 120: 67: 63: 55: 54: 17: 12: 11: 5: 949: 939: 938: 933: 928: 923: 918: 913: 897: 896: 862: 855: 829: 803: 783: 772:(4): 405–416. 761: 757: 748: 741: 715: 700: 685: 665: 636:(3): 291–320. 615: 614: 612: 609: 608: 607: 601: 596: 589: 586: 585: 584: 581: 574: 572: 566: 559: 555: 552: 542: 539: 433: 430: 417: 413: 381: 377: 372: 371: 363: 340: 333: 332: 331: 330: 327: 326: 324: 320: 319: 316: 310: 309: 306: 300: 299: 296: 290: 289: 285: 281: 277: 274: 268: 267: 264: 260: 259: 256: 250: 249: 246: 240: 239: 236: 230: 229: 226: 220: 219: 216: 207: 206: 203: 197: 196: 193: 187: 186: 183: 177: 176: 173: 167: 166: 163: 159: 158: 157:Identification 154: 153: 146:a = 7.47  144: 138: 137: 132: 126: 125: 117: 111: 110: 105: 103:Crystal system 99: 98: 95: 89: 88: 85: 79: 78: 75: 69: 68: 65: 61: 58: 48: 47: 42: 38: 37: 33: 32: 24: 23: 15: 9: 6: 4: 3: 2: 948: 937: 934: 932: 929: 927: 924: 922: 919: 917: 916:Nesosilicates 914: 912: 909: 908: 906: 884: 880: 873: 866: 858: 856:9780080204307 852: 848: 844: 840: 833: 818:on 2010-06-10 817: 813: 807: 801: 800:0-471-80580-7 797: 793: 787: 779: 775: 771: 767: 752: 744: 742:0-582-45591-X 738: 734: 729: 728: 719: 712: 707: 705: 697: 692: 690: 675: 669: 661: 657: 652: 647: 643: 639: 635: 631: 627: 620: 616: 605: 602: 600: 597: 595: 592: 591: 578: 573: 570: 563: 558: 557: 551: 548: 538: 536: 532: 528: 523: 521: 517: 513: 509: 505: 501: 497: 493: 489: 485: 481: 477: 473: 469: 468:index mineral 465: 462: 461:metamorphosed 458: 454: 450: 446: 442: 439: 429: 427: 423: 411: 407: 404: 400: 396: 388: 374: 367: 359: 352: 345: 337: 325: 321: 317: 315: 311: 307: 305: 301: 297: 295: 294:Birefringence 291: 275: 273: 269: 265: 261: 257: 255: 251: 247: 245: 241: 237: 235: 231: 227: 225: 221: 217: 212: 208: 204: 202: 198: 194: 192: 188: 185:{010} perfect 184: 182: 178: 174: 172: 171:Crystal habit 168: 164: 160: 155: 149: 145: 143: 139: 136: 133: 131: 127: 123: 118: 116: 115:Crystal class 112: 109: 106: 104: 100: 96: 94: 90: 86: 84: 80: 76: 74: 70: 59: 53: 49: 46: 43: 39: 34: 30: 25: 20: 887:. Retrieved 882: 878: 865: 838: 832: 820:. Retrieved 816:the original 806: 791: 786: 769: 765: 751: 726: 718: 677:. Retrieved 668: 633: 629: 619: 544: 524: 512:Dumortierite 457:thin section 452: 435: 398: 394: 393: 357: 134: 108:Orthorhombic 97:52.02.02a.01 45:Nesosilicate 841:: 258–272. 466:. It is an 395:Sillimanite 358:Sillimanite 304:Pleochroism 266:Biaxial (+) 244:Diaphaneity 130:Space group 22:Sillimanite 905:Categories 822:2009-12-19 713:Mindat.org 679:2009-12-19 611:References 508:pegmatites 502:, gneiss, 488:cordierite 445:andalusite 441:polymorphs 432:Occurrence 351:Andalusite 323:References 211:Mohs scale 122:H-M symbol 73:IMA symbol 660:235729616 569:Sri Lanka 520:porcelain 484:almandine 476:granulite 453:fibrolite 408:with the 399:fibrolite 195:Splintery 142:Unit cell 889:14 March 588:See also 504:hornfels 314:2V angle 214:hardness 201:Tenacity 191:Fracture 181:Cleavage 41:Category 638:Bibcode 554:Gallery 547:alumina 516:mullite 492:biotite 449:kyanite 406:mineral 344:Kyanite 87:9.AF.05 52:Formula 36:General 853:  798:  739:  658:  500:schist 496:quartz 472:gneiss 401:is an 318:21–30° 234:Streak 224:Luster 885:: 113 875:(PDF) 656:S2CID 238:White 205:Tough 162:Color 891:2022 851:ISBN 796:ISBN 737:ISBN 541:Uses 514:and 494:and 474:and 447:and 258:3.24 135:Pbnm 883:436 843:doi 774:doi 760:SiO 646:doi 498:in 416:SiO 397:or 380:SiO 77:Sil 64:SiO 907:: 881:. 877:. 849:. 770:87 768:. 735:. 733:10 703:^ 688:^ 654:. 644:. 634:85 632:. 628:. 537:. 529:, 522:. 510:. 490:, 486:, 482:, 428:. 412:Al 389:). 60:Al 893:. 859:. 845:: 825:. 780:. 776:: 762:5 758:2 745:. 682:. 662:. 648:: 640:: 418:5 414:2 385:( 382:5 378:2 286:γ 282:β 278:α 276:n 218:7 148:Å 66:5 62:2

Index


Nesosilicate
Formula
IMA symbol
Strunz classification
Dana classification
Crystal system
Orthorhombic
Crystal class
H-M symbol
Space group
Unit cell
Å
Crystal habit
Cleavage
Fracture
Tenacity
Mohs scale
Luster
Streak
Diaphaneity
Specific gravity
Refractive index
Birefringence
Pleochroism
2V angle

Kyanite
Andalusite
Sillimanite

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