26:
977:
801:
472:
1018:
25:
1062:
1011:
891:
962:
99:
1067:
1004:
241:
274:
1057:
1052:
109:
796:{\displaystyle {\ce {4CaAl2Si2O8(H2O)2 + NaAlSi2O6 <=> 2Ca2Al3Si3O12(OH) + NaAl3Si3O10(OH)2 + SiO2 + 6H2O}}}
1047:
89:
1042:
1037:
430:
231:
221:
832:
434:
264:
254:
850:
211:
958:
166:
988:
984:
898:
840:
302:
284:
201:
55:
976:
404:
bearing variety with a pinkish hue due to substitution of Mn(III) in the aluminium site.
836:
386:
119:
1031:
854:
324:
191:
131:
48:
44:
362:
957:
Nesse, William D., "Introduction to
Mineralogy," (c)2000 Oxford University Press
921:
442:
149:
876:
456:
438:
420:
408:
140:
124:
460:
401:
359:
393:
by substitution of iron(III) in the aluminium (m3 site) and is also called
452:
334:
845:
820:
932:
448:
416:
412:
390:
356:
872:
464:
429:
It occurs in rocks which have undergone low to medium grade
196:
Elongated primatic crystals, striated; granular to fibrous
786:
766:
750:
729:
716:
703:
676:
663:
650:
637:
580:
567:
551:
535:
517:
504:
491:
992:
186:
Colorless, green, gray, light green, yellow green, pink
604:
475:
437:
of high calcium sedimentary rocks. It also occurs in
343:
333:
323:
301:
293:
283:
273:
263:
253:
240:
230:
220:
210:
200:
190:
182:
177:
165:
148:
130:
118:
108:
98:
88:
54:
40:
35:
18:
795:
612:
611:
594:
593:
415:, and is so-named because of its resemblance to
173:c = 10.155 ; β = 115.50°; Z = 2
1012:
8:
948:. Geological Society of London. p. 477.
892:"Clinozoisite in the Handbook of Mineralogy"
1019:
1005:
844:
785:
780:
775:
765:
760:
749:
744:
733:
728:
723:
715:
710:
702:
697:
679:
675:
670:
662:
657:
649:
644:
636:
631:
626:
613:
606:
605:
603:
595:
588:
586:
585:
583:
579:
574:
566:
561:
550:
545:
534:
529:
521:
516:
511:
503:
498:
490:
485:
480:
476:
474:
455:minerals have suggested clinozoisite and
868:
866:
864:
407:It was originally discovered in 1896 in
811:
587:
467:and water via the following reaction:
15:
886:
884:
7:
973:
971:
821:"IMA–CNMNC approved mineral symbols"
991:. You can help Knowledge (XXG) by
14:
946:Single-chain Silicates, Volume 2A
975:
459:are associated and derived from
24:
922:Clinozoisite data on Webmineral
983:This article about a specific
740:
734:
686:
680:
614:
589:
541:
522:
385:)O(OH). It forms a continuous
1:
1084:
1063:Minerals in space group 11
970:
279:Transparent to translucent
206:Lamellar on {100} uncommon
944:Deer, William A. (1997).
23:
365:mineral with formula: Ca
1068:Silicate mineral stubs
933:Clinothulite on Mindat
825:Mineralogical Magazine
797:
798:
431:regional metamorphism
171:a = 8.879, b = 5.583
100:Strunz classification
473:
435:contact metamorphism
426:crystal structure.
1058:Monoclinic minerals
846:10.1180/mgm.2021.43
837:2021MinM...85..291W
819:Warr, L.N. (2021).
788:
768:
752:
731:
718:
705:
678:
665:
652:
639:
600:
582:
569:
553:
537:
519:
506:
493:
110:Dana classification
1053:Aluminium minerals
793:
776:
756:
732:
719:
706:
693:
666:
653:
640:
627:
619:
570:
557:
525:
520:
507:
494:
481:
400:Clinothulite is a
339:14 to 90° measured
294:Optical properties
1000:
999:
791:
779:
759:
739:
722:
709:
696:
685:
669:
656:
643:
630:
621:
573:
560:
540:
528:
510:
497:
484:
395:aluminium epidote
350:
349:
329:δ = 0.006 – 0.011
315:= 1.708 – 1.729 n
311:= 1.706 – 1.724 n
144:
1075:
1048:Calcium minerals
1021:
1014:
1007:
985:silicate mineral
979:
972:
950:
949:
941:
935:
930:
924:
919:
913:
912:
910:
909:
903:
897:. Archived from
896:
888:
879:
870:
859:
858:
848:
816:
802:
800:
799:
794:
792:
789:
787:
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767:
764:
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751:
748:
743:
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730:
727:
720:
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714:
707:
704:
701:
694:
689:
683:
677:
674:
667:
664:
661:
654:
651:
648:
641:
638:
635:
628:
622:
620:
618:
617:
610:
602:
601:
599:
592:
584:
581:
578:
571:
568:
565:
558:
552:
549:
544:
538:
536:
533:
526:
518:
515:
508:
505:
502:
495:
492:
489:
482:
303:Refractive index
285:Specific gravity
246:
226:Irregular/uneven
216:Perfect on {001}
138:
136:Prismatic (2/m)
61:
60:(repeating unit)
28:
16:
1083:
1082:
1078:
1077:
1076:
1074:
1073:
1072:
1028:
1027:
1026:
1025:
968:
954:
953:
943:
942:
938:
931:
927:
920:
916:
907:
905:
901:
894:
890:
889:
882:
871:
862:
818:
817:
813:
808:
471:
470:
384:
380:
376:
372:
368:
319:= 1.712 – 1.735
318:
314:
310:
244:
172:
160:
137:
83:
79:
75:
71:
67:
59:
58:
47:
31:
12:
11:
5:
1081:
1079:
1071:
1070:
1065:
1060:
1055:
1050:
1045:
1040:
1030:
1029:
1024:
1023:
1016:
1009:
1001:
998:
997:
980:
966:
965:
952:
951:
936:
925:
914:
880:
860:
831:(3): 291–320.
810:
809:
807:
804:
783:
774:
771:
763:
755:
747:
742:
736:
726:
713:
700:
692:
688:
682:
673:
660:
647:
634:
625:
616:
609:
598:
591:
577:
564:
556:
548:
543:
532:
524:
514:
501:
488:
479:
441:alteration of
387:solid solution
382:
378:
374:
370:
366:
348:
347:
345:
341:
340:
337:
331:
330:
327:
321:
320:
316:
312:
308:
305:
299:
298:
295:
291:
290:
287:
281:
280:
277:
271:
270:
267:
261:
260:
257:
251:
250:
247:
238:
237:
234:
228:
227:
224:
218:
217:
214:
208:
207:
204:
198:
197:
194:
188:
187:
184:
180:
179:
178:Identification
175:
174:
169:
163:
162:
158:
152:
146:
145:
134:
128:
127:
122:
120:Crystal system
116:
115:
112:
106:
105:
102:
96:
95:
92:
86:
85:
81:
77:
73:
69:
65:
62:
52:
51:
42:
38:
37:
33:
32:
29:
21:
20:
13:
10:
9:
6:
4:
3:
2:
1080:
1069:
1066:
1064:
1061:
1059:
1056:
1054:
1051:
1049:
1046:
1044:
1043:Epidote group
1041:
1039:
1038:Sorosilicates
1036:
1035:
1033:
1022:
1017:
1015:
1010:
1008:
1003:
1002:
996:
994:
990:
986:
981:
978:
974:
969:
964:
963:0-19-510691-1
960:
956:
955:
947:
940:
937:
934:
929:
926:
923:
918:
915:
904:on 2015-09-24
900:
893:
887:
885:
881:
878:
874:
869:
867:
865:
861:
856:
852:
847:
842:
838:
834:
830:
826:
822:
815:
812:
805:
803:
781:
772:
769:
761:
753:
745:
724:
711:
698:
690:
671:
658:
645:
632:
623:
607:
596:
575:
562:
554:
546:
530:
512:
499:
486:
477:
468:
466:
462:
458:
454:
450:
446:
444:
440:
436:
432:
427:
425:
424:
418:
414:
410:
405:
403:
398:
396:
392:
388:
364:
361:
358:
355:is a complex
354:
346:
342:
338:
336:
332:
328:
326:
325:Birefringence
322:
306:
304:
300:
296:
292:
288:
286:
282:
278:
276:
272:
269:Grayish white
268:
266:
262:
258:
256:
252:
248:
243:
239:
235:
233:
229:
225:
223:
219:
215:
213:
209:
205:
203:
199:
195:
193:
192:Crystal habit
189:
185:
181:
176:
170:
168:
164:
156:
153:
151:
147:
142:
135:
133:
132:Crystal class
129:
126:
123:
121:
117:
113:
111:
107:
103:
101:
97:
93:
91:
87:
63:
57:
53:
50:
49:Epidote group
46:
45:Sorosilicates
43:
39:
34:
27:
22:
17:
993:expanding it
982:
967:
945:
939:
928:
917:
906:. Retrieved
899:the original
873:Clinozoisite
828:
824:
814:
469:
447:
428:
422:
406:
399:
394:
389:series with
363:sorosilicate
353:Clinozoisite
352:
351:
154:
30:Clinozoisite
19:Clinozoisite
443:plagioclase
297:Biaxial (+)
275:Diaphaneity
150:Space group
1032:Categories
908:2014-03-24
877:Mindat.org
806:References
463:releasing
457:paragonite
439:saussurite
409:East Tyrol
344:References
242:Mohs scale
141:H-M symbol
125:Monoclinic
90:IMA symbol
855:235729616
615:⇀
608:−
597:−
590:↽
461:lawsonite
402:manganese
360:aluminium
167:Unit cell
114:58.2.1a.4
453:pyroxene
451:bearing
419:and its
335:2V angle
259:Vitreous
245:hardness
232:Tenacity
222:Fracture
212:Cleavage
202:Twinning
104:9.BG.05a
41:Category
833:Bibcode
449:Jadeite
433:and in
417:zoisite
413:Austria
391:epidote
357:calcium
289:3.3–3.4
236:Brittle
56:Formula
36:General
961:
853:
559:NaAlSi
465:quartz
423:clinic
265:Streak
255:Luster
139:(same
84:)O(OH)
987:is a
902:(PDF)
895:(PDF)
851:S2CID
381:)(SiO
183:Color
80:)(SiO
989:stub
959:ISBN
695:NaAl
483:CaAl
421:mono
875:on
841:doi
758:SiO
373:(Si
249:6–7
94:Czo
72:(Si
1034::
883:^
863:^
849:.
839:.
829:85
827:.
823:.
738:OH
725:10
708:Si
684:OH
672:12
655:Si
642:Al
629:Ca
496:Si
445:.
411:,
397:.
369:Al
161:/m
68:Al
64:Ca
1020:e
1013:t
1006:v
995:.
911:.
857:.
843::
835::
790:O
782:2
778:H
773:6
770:+
762:2
754:+
746:2
741:)
735:(
721:O
712:3
699:3
691:+
687:)
681:(
668:O
659:3
646:3
633:2
624:2
576:6
572:O
563:2
555:+
547:2
542:)
539:O
531:2
527:H
523:(
513:8
509:O
500:2
487:2
478:4
383:4
379:7
377:O
375:2
371:3
367:2
317:γ
313:β
309:α
307:n
159:1
157:2
155:P
143:)
82:4
78:7
76:O
74:2
70:3
66:2
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