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Andalusite

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Abs-Wurmbach, I.; Langer, K.; Seifert, F.; Tillmanns, Ε. (1 October 1981). "The crystal chemistry of (Mn 3+ , Fe 3+ )-substituted andalusites (viridines and kanonaite), (Al 1-x-y Mn x 3+ Fe 3+ y ) 2 (O|SiO 4 ): crystal structure refinements, Mössbauer, and polarized optical absorption spectra".
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of andalusite, each occurring under different temperature-pressure regimes and are therefore rarely found together in the same rock. Because of this the three minerals are a useful tool to help identify the pressure-temperature paths of the host rock in which they are found. It is particularly
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pattern when shown in cross-section. This stone was known at least from the sixteenth century, being taken to many European countries, as a souvenir, by pilgrims returning from Santiago de Compostela.
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Whitney, D.L. (2002). "Coexisting andalusite, kyanite, and sillimanite: Sequential formation of three Al2SiO5 polymorphs during progressive metamorphism near the triple point, Sivrihisar, Turkey".
391:, being the lower pressure mid temperature polymorph. At higher temperatures and pressures, andalusite may convert to sillimanite. Thus, as with its other polymorphs, andalusite is an 522:
A clear variety found in Brazil and Sri-Lanka can be cut into a gemstone. Faceted andalusite stones give a play of red, green, and yellow colors that resembles a muted form of
376:, Spain. It soon became clear that it was a locality error, and that the specimens studied were actually from El Cardoso de la Sierra, in the Spanish province of 768:
Calvo, Miguel (2016). "El "lapis crucifer", "piedra de cruz de Compostela": un elemento importante de los patrimonios geológico y cultural del NW de España".
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Vrána, S.; Rieder, M.; Podlaha, J. (1978). "Kanonaite, (Mn 0.76 3+ Al0.23Fe 0.02 3+ )Al, a new mineral isotypic with andalusite".
674: 402: 912: 1082: 961: 622: 669:. Madrid, Spain: Escuela TĂ©cnica Superior de Ingenieros de Minas de Madrid. FundaciĂłn GĂłmez Pardo. pp. 91–94. 610: 551: 85: 1077: 440: 203: 236: 1087: 168:
As euhedral crystals or columnar aggregates having nearly square cross sections; fibrous compact to massive
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Whitney, D.L. (2002). "Coexisting andalusite, kyanite, and sillimanite: Sequential formation of three Al
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index mineral, providing clues to depth and pressures involved in producing the host rock.
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is a greenish-black mineral related to andalusite and having the approximate composition
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polymorphs during progressive metamorphism near the triple point, Sivrihisar, Turkey".
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Pink, violet, yellow, green, white, gray; in thin section, colorless to pink or green
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mineral which forms under low pressure and low to high temperatures. The minerals
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3+ substitutes for aluminium, the same change is also responsible for the colour.
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possesses by far the largest portion of the world's known andalusite deposits.
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Delamétherie, Jean Claude (1798). "Sur une pierre de l'Andalousie".
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Journal of the Southern African Institute of Mining and Metallurgy
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commonly contains dark inclusions of carbon or clay which form a
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Journal de Physique, de Chimie d'Histoire Naturelle et des Arts
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Zeitschrift fĂĽr Kristallographie - Crystalline Materials
956:. New York: Oxford University Press. pp. 314–318. 979:"Use Of Andalusite Refractories In Ferrous Metallurgy" 904: 634:
http://rruff.geo.arizona.edu/doclib/hom/andalusite.pdf
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Fernandes, Shyamala; Choudhary, Gagan (Summer 2009).
575:in furnaces, kilns and other industrial processes. 910: 885:International Colored Gem Association: Anadalusite 846: 977:Dubreuil, P.; Sobolev, V. M.; Filari, E. (1999). 1059: 667:Minerales y Minas de España. Vol. IX. Silicatos 689: 645: 241:Transparent to nearly opaque with inclusions 431: 945: 849:Contributions to Mineralogy and Petrology 1022: 460: 732: 627: 1060: 422: 415: 408: 951: 767: 664: 606: 604: 259:double refractive, biaxial negative; 983:Refractories and Industrial Ceramics 913:"Gem-quality andalusite from Brazil" 13: 601: 145:c = 5.5566 Ă…; Z = 4 14: 1104: 263:has anomalous aggregate reaction. 824:"Minerals Colored by Metal Ions" 611:Gemological Institute of America 401: 27: 1023:Overbeek, P. W. (1 June 1989). 1016: 970: 875: 840: 492:variety of andalusite in which 816: 780: 761: 726: 683: 658: 639: 383:Andalusite is trimorphic with 16:Aluminium nesosilicate mineral 1: 594: 533: 1025:"Andalusite in South Africa" 469: 364:with the chemical formula Al 188:Good on {110}, poor on {100} 7: 802:10.1524/zkri.1981.155.14.81 582: 10: 1109: 1083:Minerals in space group 58 954:Introduction to mineralogy 952:Nesse, William D. (2000). 559:metamorphic rocks such as 342: 329: 319: 309: 299: 289: 267: 255: 245: 235: 225: 215: 202: 192: 182: 172: 162: 154: 149: 133: 121: 106: 94: 84: 74: 53: 43: 38: 26: 21: 828:minerals.gps.caltech.edu 571:Andalusite is used as a 465:Round faceted andalusite 615:GIA Gem Reference Guide 566: 538:Andalusite is a common 198:uneven to subconchoidal 1041:10520/AJA0038223X_1910 665:Calvo, Miguel (2018). 636:Handbook of Mineralogy 466: 1078:Orthorhombic minerals 932:10.5741/GEMS.45.2.120 743:American Mineralogist 692:American Mineralogist 464: 86:Strunz classification 755:10.2138/am-2002-0404 712:10.2138/am-2002-0404 143:, b = 7.9031 Ă… 1088:Industrial minerals 920:Gems & Gemology 704:2002AmMin..87..405W 443:Phase diagram of Al 1068:Aluminium minerals 995:10.1007/BF02762295 861:10.1007/BF00373417 467: 305:strongly trichroic 256:Optical properties 112:Dipyramidal (mmm) 676:978-84-8321-883-9 380:, not Andalusia. 349: 348: 295:δ = 0.009 – 0.010 281:= 1.633 – 1.644 n 277:= 1.629 – 1.640 n 1100: 1052: 1051: 1049: 1047: 1020: 1014: 1013: 1011: 1009: 989:(5–6): 252–259. 974: 968: 967: 949: 943: 942: 940: 938: 917: 908: 902: 901: 899: 898: 889:. Archived from 879: 873: 872: 844: 838: 837: 835: 834: 820: 814: 813: 784: 778: 777: 765: 759: 758: 730: 724: 723: 687: 681: 680: 662: 656: 655: 643: 637: 631: 625: 608: 589:List of minerals 555:associated with 518: 454:aluminosilicates 435: 427: 420: 413: 405: 269:Refractive index 247:Specific gravity 208: 139:a = 7.7980  60: 59:(repeating unit) 31: 19: 18: 1108: 1107: 1103: 1102: 1101: 1099: 1098: 1097: 1058: 1057: 1056: 1055: 1045: 1043: 1021: 1017: 1007: 1005: 975: 971: 964: 950: 946: 936: 934: 915: 909: 905: 896: 894: 881: 880: 876: 845: 841: 832: 830: 822: 821: 817: 796:(1–4): 81–114. 785: 781: 770:De Re Metallica 766: 762: 740: 736: 731: 727: 688: 684: 677: 663: 659: 644: 640: 632: 628: 609: 602: 597: 585: 569: 536: 517: 513: 509: 505: 501: 472: 459: 458: 457: 451: 450: 446: 442: 437: 436: 429: 428: 423: 421: 416: 414: 409: 406: 393:aluminosilicate 371: 367: 338:non-fluorescent 325:r < v strong 285:= 1.638 – 1.650 284: 280: 276: 206: 144: 117:: (2/m 2/m 2/m) 113: 70: 66: 58: 57: 34: 17: 12: 11: 5: 1106: 1096: 1095: 1090: 1085: 1080: 1075: 1070: 1054: 1053: 1035:(6): 157–171. 1015: 969: 962: 944: 926:(2): 120–129. 903: 874: 855:(3): 325–332. 839: 815: 779: 760: 749:(4): 405–416. 738: 734: 725: 698:(4): 405–416. 682: 675: 657: 638: 626: 599: 598: 596: 593: 592: 591: 584: 581: 568: 565: 535: 532: 515: 511: 507: 503: 471: 468: 448: 444: 439: 438: 430: 407: 400: 399: 398: 397: 369: 365: 347: 346: 344: 340: 339: 336: 327: 326: 323: 317: 316: 313: 307: 306: 303: 297: 296: 293: 287: 286: 282: 278: 274: 271: 265: 264: 257: 253: 252: 249: 243: 242: 239: 233: 232: 229: 223: 222: 219: 213: 212: 209: 200: 199: 196: 190: 189: 186: 180: 179: 178:On {101}, rare 176: 170: 169: 166: 160: 159: 156: 152: 151: 150:Identification 147: 146: 137: 131: 130: 125: 119: 118: 110: 104: 103: 98: 96:Crystal system 92: 91: 88: 82: 81: 78: 72: 71: 68: 64: 61: 51: 50: 45: 41: 40: 36: 35: 32: 24: 23: 15: 9: 6: 4: 3: 2: 1105: 1094: 1091: 1089: 1086: 1084: 1081: 1079: 1076: 1074: 1073:Nesosilicates 1071: 1069: 1066: 1065: 1063: 1042: 1038: 1034: 1030: 1026: 1019: 1004: 1000: 996: 992: 988: 984: 980: 973: 965: 963:9780195106916 959: 955: 948: 933: 929: 925: 921: 914: 907: 893:on 2006-07-17 892: 888: 886: 878: 870: 866: 862: 858: 854: 850: 843: 829: 825: 819: 811: 807: 803: 799: 795: 791: 783: 775: 771: 764: 756: 752: 748: 744: 729: 721: 717: 713: 709: 705: 701: 697: 693: 686: 678: 672: 668: 661: 653: 649: 642: 635: 630: 624: 623:0-87311-019-6 620: 616: 612: 607: 605: 600: 590: 587: 586: 580: 578: 574: 564: 562: 558: 553: 549: 545: 541: 531: 529: 525: 520: 499: 495: 491: 487: 483: 481: 477: 463: 455: 441: 434: 426: 419: 412: 404: 396: 394: 390: 386: 381: 379: 375: 363: 360: 357: 353: 345: 341: 337: 335: 332: 328: 324: 322: 318: 314: 312: 308: 304: 302: 298: 294: 292: 291:Birefringence 288: 272: 270: 266: 262: 258: 254: 250: 248: 244: 240: 238: 234: 230: 228: 224: 220: 218: 214: 210: 205: 201: 197: 195: 191: 187: 185: 181: 177: 175: 171: 167: 165: 164:Crystal habit 161: 157: 153: 148: 142: 138: 136: 132: 129: 126: 124: 120: 116: 111: 109: 108:Crystal class 105: 102: 99: 97: 93: 89: 87: 83: 79: 77: 73: 62: 56: 52: 49: 48:Nesosilicates 46: 42: 37: 30: 25: 20: 1044:. Retrieved 1032: 1028: 1018: 1006:. Retrieved 986: 982: 972: 953: 947: 935:. Retrieved 923: 919: 906: 895:. Retrieved 891:the original 884: 877: 852: 848: 842: 831:. Retrieved 827: 818: 793: 789: 782: 773: 769: 763: 746: 742: 728: 695: 691: 685: 666: 660: 651: 647: 641: 629: 614: 577:South Africa 570: 537: 521: 497: 485: 484: 474:The variety 473: 417: 382: 359:nesosilicate 351: 350: 334:fluorescence 260: 251:3.17 (± .04) 127: 101:Orthorhombic 561:mica schist 548:sillimanite 540:metamorphic 528:pleochroism 524:iridescence 476:chiastolite 425:Sillimanite 389:sillimanite 378:Guadalajara 331:Ultraviolet 301:Pleochroism 261:chiastolite 237:Diaphaneity 123:Space group 1062:Categories 1046:25 October 1008:25 October 937:30 October 897:2006-07-13 833:2023-03-01 654:: 386–387. 595:References 573:refractory 552:polymorphs 534:Occurrence 418:Andalusite 352:Andalusite 343:References 321:Dispersion 204:Mohs scale 115:H-M symbol 76:IMA symbol 33:Andalusite 22:Andalusite 1093:Gemstones 1003:136482381 810:201671728 720:131616262 498:Kanonaite 494:manganese 480:cruciform 470:Varieties 374:Andalusia 356:aluminium 135:Unit cell 869:95925117 776:: 67–79. 583:See also 486:Viridine 311:2V angle 221:Vitreous 207:hardness 194:Fracture 184:Cleavage 174:Twinning 44:Category 700:Bibcode 557:pelitic 544:kyanite 411:Kyanite 385:kyanite 362:mineral 211:6.5–7.5 90:9.AF.10 55:Formula 39:General 1001:  960:  867:  808:  718:  673:  621:  617:1995, 514:)AlSiO 354:is an 315:71–86° 227:Streak 217:Luster 999:S2CID 916:(PDF) 865:S2CID 806:S2CID 716:S2CID 490:green 488:is a 231:White 155:Color 1048:2021 1010:2021 958:ISBN 939:2021 671:ISBN 619:ISBN 567:Uses 550:are 546:and 512:0.02 508:0.23 504:0.76 387:and 128:Pnnm 1037:hdl 991:doi 928:doi 857:doi 798:doi 794:155 751:doi 737:SiO 708:doi 502:(Mn 447:SiO 368:SiO 80:And 67:SiO 1064:: 1033:89 1031:. 1027:. 997:. 987:40 985:. 981:. 924:45 922:. 918:. 863:. 853:66 851:. 826:. 804:. 792:. 772:. 747:87 745:. 714:. 706:. 696:87 694:. 652:46 650:. 613:, 603:^ 563:. 530:. 519:. 510:Fe 506:Al 456:). 63:Al 1050:. 1039:: 1012:. 993:: 966:. 941:. 930:: 900:. 887:" 883:" 871:. 859:: 836:. 812:. 800:: 774:6 757:. 753:: 739:5 735:2 722:. 710:: 702:: 679:. 516:5 452:( 449:5 445:2 370:5 366:2 283:Îł 279:β 275:α 273:n 141:Ă… 69:5 65:2

Index


Nesosilicates
Formula
IMA symbol
Strunz classification
Crystal system
Orthorhombic
Crystal class
H-M symbol
Space group
Unit cell
Ă…
Crystal habit
Twinning
Cleavage
Fracture
Mohs scale
Luster
Streak
Diaphaneity
Specific gravity
Refractive index
Birefringence
Pleochroism
2V angle
Dispersion
Ultraviolet
fluorescence
aluminium
nesosilicate

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