29:
591:
336:. The mineral's name is derived from the person who first described it, an Australian mineral collector named Charles W. Marsh. Marsh drew attention to native copper iodide (Marshite) in the 1800s emphasizing its natural occurrence, it is not to be confused with
725:
Pekov, I.V., Lykova, I.S., Bryzgalov, I.A., Ksenofontov, D.A., Zyryanova, L.A., and
Litvinov, N.D. (2010) âExtremely rich iodide mineralization at the Rubtsovskoe base metal deposit (North West Altay, Russia) and its genesisâ,
613:
The System of
Mineralogy of James Dwight Dana and Edward Salisbury Dana Yale University 1837-1892, Volume II: Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates,
441:, Russia marshite is found associated with other iodine-rich halide minerals such as miersite in a base metal deposit. Marshite is found in the silver deposit mined at the Albert Silver Mine in
684:
626:
567:
463:
705:
767:
Dana's System of
Mineralogy, Volume II: Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates, Etc. (Seventh Edition)"
33:
Exceptionally well crystallized specimen of the rare copper iodide marshite from the
Rubtsovskoe Deposit, Altaiskii Krai, Western Siberia, Russian Federation.
328:(Cu). Solid solution between the silver end-member miersite and the copper end-member marshite has been found in these minerals from deposits in
351:-red color. Another characteristic useful in identifying marshite is the dark red color it fluoresces under short-wave (SW) and long-wave (LW)
78:
216:
704:
Reich, M., Snyder, G.T., Ălvarez, F., PĂ©rez, A., Palacios, C., Vargas, G., Cameron, E.M., Muramatsu, Y. and Fehn, U. (2013)
666:
Marsh, C.W. and
Liversidge, A. (1892) "On Native Copper Iodide (Marshite) and other Minerals from Broken Hill, N.S. Wales",
706:âUSING IODINE ISOTOPES TO CONSTRAIN SUPERGENE FLUID SOURCES IN ARID REGIONS: INSIGHTS FROM THE CHUQUICAMATA OXIDE BLANKETâ
249:
740:
88:
783:
68:
406:
which are heavily mined for copper. Additional research on the rocks and minerals from this area show that
206:
196:
592:âThe identity of kilbrickenite with geocronite: And analyses of miersite, marshite, and copper-pyritesâ
475:
314:
103:
417:
In addition to multiple occurrences in
Australia and Chile, marshite has been found and reported in
434:
395:
239:
229:
343:
One of marshite's distinguishing features is that prior to exposure to air the mineral is a faint
627:âMarshite - miersite solid solution and iodargyrite from Broken Hill, New South Wales, Australiaâ
493:
186:
368:
337:
143:
483:
259:
176:
54:
372:
317:
47:
519:
479:
98:
777:
497:
376:
375:, Australia. Some of marshite's common mineral associations at this locality include
166:
110:
430:
399:
292:
616:
John Wiley and Sons, Inc., New York, 7th edition, revised and enlarged: pp. 20-22.
352:
329:
289:
127:
442:
438:
741:âThe Albert Silver Mine and Trippkeite Occurrence, Mpumalanga, South Africaâ
555:
388:
333:
414:
can be used to understand the processes that formed the supergene deposit.
380:
488:
422:
418:
384:
269:
539:
426:
407:
325:
321:
28:
403:
363:
The type locality of marshite is a metamorphosed Lead-Zinc-Silver
348:
344:
411:
668:
Journal and
Proceedings of the Royal Society of New South Wales
364:
445:, South Africa associated with various silver-rich minerals.
347:-yellow color, once exposed to the air however it becomes a
730:, Budapest, Hungary, August 21â27, CD of Abstracts, p. 416.
340:
a substance commonly synthesized in laboratory settings.
739:
Meulenbeld, P.M.P.B., Grote, W., and Verryn, S. (2014)
685:âMarshite and other minerals from Chuquicamata, Chileâ
769:
John Wiley and Sons, Inc., New York, pp. 20â22.
648:
Proceedings of the Royal
Society of New South Wales
301:
288:
280:
268:
258:
248:
238:
228:
215:
205:
195:
185:
175:
165:
157:
152:
142:
126:
109:
97:
87:
77:
67:
53:
43:
38:
21:
410:isotopes found in minerals, such as marshite, and
161:Honey-yellow, exposed to air pink-red to brick-red
765:Palache, P.; Berman H.; Frondel, C. (1960). "
611:Palache, C., Berman, H., Frondel, C. (1951) "
568:âA note on the crystal structure of marshiteâ
171:Tetrahedral crystals, cubo-octahedral, crusts
8:
551:
549:
547:
148:a = 6.05 Ă
(untwinned a = 6.6063(1) Ă
); Z=4
27:
728:20th General Meeting of the IMA (IMA2010)
662:
660:
566:Cooper, M.A., and Hawthorne, F.C. (1997)
487:
535:
533:
531:
529:
527:
586:
584:
454:
394:Marshite occurs naturally in geologic
18:
515:
513:
511:
509:
507:
7:
654:: 326â332 (as Native copper iodide).
464:"IMAâCNMNC approved mineral symbols"
14:
520:Handbook of Mineralogy - Marshite
313:(CuI) is a naturally occurring
1:
800:
572:The Canadian Mineralogist
26:
367:deposit at Broken Hill,
16:Isometric halide mineral
625:Millsteed, P.W. (1998)
631:Mineralogical Magazine
596:Mineralogical Magazine
468:Mineralogical Magazine
324:(Ag) substitution for
276:5.71 g/cm (calculated)
689:American Mineralogist
683:Jarrell, O.W. (1939)
556:Webmineral - Marshite
540:Mindat.org - Marshite
274:5.68 g/cm (measured),
79:Strunz classification
745:Rocks & Minerals
646:Marsh, C.W. (1892)
590:Prior, G.T. (1902)
489:10.1180/mgm.2021.43
480:2021MinM...85..291W
462:Warr, L.N. (2021).
359:Geologic occurrence
89:Dana classification
281:Optical properties
234:Adamantine, greasy
770:
383:, native copper,
369:Yancowinna County
338:copper (I) iodide
308:
307:
297:Dark red (SW, LW)
791:
764:
752:
737:
731:
723:
717:
710:Economic Geology
702:
696:
681:
675:
664:
655:
644:
638:
623:
617:
609:
603:
588:
579:
564:
558:
553:
542:
537:
522:
517:
502:
501:
491:
459:
320:with occasional
260:Specific gravity
221:
136:
119:
115:Hextetrahedral (
60:
59:(repeating unit)
31:
19:
799:
798:
794:
793:
792:
790:
789:
788:
784:Halide minerals
774:
773:
761:
756:
755:
738:
734:
724:
720:
703:
699:
682:
678:
665:
658:
645:
641:
624:
620:
610:
606:
589:
582:
565:
561:
554:
545:
538:
525:
518:
505:
461:
460:
456:
451:
373:New South Wales
361:
275:
219:
134:
117:
58:
57:
34:
17:
12:
11:
5:
797:
795:
787:
786:
776:
775:
772:
771:
760:
757:
754:
753:
732:
718:
697:
695:(10): 629â635.
676:
656:
639:
618:
604:
580:
559:
543:
523:
503:
474:(3): 291â320.
453:
452:
450:
447:
360:
357:
318:halide mineral
306:
305:
303:
299:
298:
295:
286:
285:
282:
278:
277:
272:
266:
265:
262:
256:
255:
252:
246:
245:
242:
236:
235:
232:
226:
225:
222:
213:
212:
209:
203:
202:
199:
193:
192:
189:
183:
182:
179:
173:
172:
169:
163:
162:
159:
155:
154:
153:Identification
150:
149:
146:
140:
139:
130:
124:
123:
113:
107:
106:
101:
99:Crystal system
95:
94:
91:
85:
84:
81:
75:
74:
71:
65:
64:
61:
51:
50:
48:Halide mineral
45:
41:
40:
36:
35:
32:
24:
23:
15:
13:
10:
9:
6:
4:
3:
2:
796:
785:
782:
781:
779:
768:
763:
762:
758:
750:
746:
742:
736:
733:
729:
722:
719:
716:(1): 163â171.
715:
711:
707:
701:
698:
694:
690:
686:
680:
677:
673:
669:
663:
661:
657:
653:
649:
643:
640:
637:(4): 471â475.
636:
632:
628:
622:
619:
615:
608:
605:
601:
597:
593:
587:
585:
581:
577:
573:
569:
563:
560:
557:
552:
550:
548:
544:
541:
536:
534:
532:
530:
528:
524:
521:
516:
514:
512:
510:
508:
504:
499:
495:
490:
485:
481:
477:
473:
469:
465:
458:
455:
448:
446:
444:
440:
436:
432:
428:
424:
420:
415:
413:
409:
405:
401:
397:
392:
390:
386:
382:
378:
374:
370:
366:
358:
356:
354:
350:
346:
341:
339:
335:
331:
327:
323:
319:
316:
312:
304:
300:
296:
294:
291:
287:
283:
279:
273:
271:
267:
263:
261:
257:
253:
251:
247:
243:
241:
237:
233:
231:
227:
223:
218:
214:
210:
208:
204:
200:
198:
194:
191:{011} perfect
190:
188:
184:
180:
178:
174:
170:
168:
167:Crystal habit
164:
160:
156:
151:
147:
145:
141:
138:
131:
129:
125:
121:
114:
112:
111:Crystal class
108:
105:
102:
100:
96:
92:
90:
86:
82:
80:
76:
72:
70:
66:
62:
56:
52:
49:
46:
42:
37:
30:
25:
20:
766:
759:Bibliography
748:
744:
735:
727:
721:
713:
709:
700:
692:
688:
679:
671:
667:
651:
647:
642:
634:
630:
621:
612:
607:
599:
595:
575:
571:
562:
471:
467:
457:
437:locality in
431:South Africa
416:
400:Chuquicamata
398:deposits at
393:
362:
342:
310:
309:
293:fluorescence
132:
116:
353:ultraviolet
330:Broken Hill
290:Ultraviolet
254:Transparent
250:Diaphaneity
128:Space group
751:: 416â423.
674:: 326â332.
602:: 186â190.
578:: 785â786.
449:References
443:Mpumalanga
439:Altai Krai
435:Rubtsovsky
302:References
217:Mohs scale
201:Conchoidal
69:IMA symbol
498:235729616
433:. At the
396:supergene
389:cerussite
334:Australia
315:isometric
284:Isotropic
144:Unit cell
104:Isometric
778:Category
381:limonite
311:Marshite
220:hardness
207:Tenacity
197:Fracture
187:Cleavage
181:On {111}
177:Twinning
44:Category
22:Marshite
476:Bibcode
423:Germany
419:Finland
385:cuprite
355:light.
270:Density
211:Brittle
93:9.1.7.3
83:3.AA.05
55:Formula
39:General
496:
429:, and
427:Russia
408:iodine
387:, and
326:copper
322:silver
244:Yellow
240:Streak
230:Luster
614:Etc."
494:S2CID
412:soils
404:Chile
349:brick
345:honey
158:Color
264:5.68
714:108
484:doi
377:wad
365:ore
224:2.5
73:Msh
63:CuI
780::
749:89
747:,
743:.
712:,
708:.
693:24
691:,
687:.
672:26
670:,
659:^
652:26
650:,
635:62
633:,
629:.
600:13
598:,
594:,
583:^
576:35
574:,
570:,
546:^
526:^
506:^
492:.
482:.
472:85
470:.
466:.
425:,
421:,
402:,
391:.
379:,
371:,
332:,
137:3m
120:3m
500:.
486::
478::
135:4
133:F
122:)
118:4
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
