43:
36:
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and thus relatively high efficiency. With the age of the deposit of 4.5 to 4.2 million years, the solar neutrino flux can be estimated over the last 4 million years provided it is possible to determine the amount of lead-205 in a lorandite sample. This reaction can be induced not only by neutrino but
547:
Boev, B., Šorša, A., Boev, I. (2016) Geochemical and mineralogical characteristics of the central part of the Alšar deposit (Republic of
Macedonia) with particular reference to investigations by X-ray diffraction. Geologica Macedonica, 30,
377:
other high energy cosmic particles, which all have different penetration depth in the crust. Therefore, a large volume of data is being accumulated during 2008–2010 from different depths of the deposit to produce reliable data.
620:
Pavicevic, M.; Elgoresy, A. (1988). "Crven Dol Tl deposit in
Allchar: Mineralogical investigation, chemical composition of Tl minerals and genetic implications".
35:
757:
561:
Cvetković, Lj.; Boronikhin, V. A.; Pavićević, M. K.; Krajnović, D.; Gržetić, I.; Libowitzky, E.; Giester, G.; Tillmanns, E. (1995). "Jankovićite, Tl
79:
255:
Crven Dol mine operated in the antimony-poor and arsenic- and thallium-rich layer of the orebody. The minerals making most of the orebody are
291:– is the main thallium mineral in the deposit. Several other thallium minerals have been discovered in the mine over the years, for example,
762:
468:
657:
Nuclear
Instruments and Methods in Physics Research Section A: Accelerators, Spectrometers, Detectors and Associated Equipment
622:
Nuclear
Instruments and Methods in Physics Research Section A: Accelerators, Spectrometers, Detectors and Associated Equipment
415:
Nuclear
Instruments and Methods in Physics Research Section A: Accelerators, Spectrometers, Detectors and Associated Equipment
216:. The area will be declared a protected site. In about 2010, several collectors without this permit were arrested by police."
271:. The deposit was mined extensively between 1880 and 1908. Antimony, arsenic and thallium were produced during that period.
225:
752:
499:
396:
742:
190:
747:
655:
Jankovic, S. (1988). "The
Allchar Tl–As–Sb Deposit, Yugoslavia and its specific metallogenic features".
737:
664:
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586:
514:
422:
213:
186:
229:
602:
530:
292:
330:
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283:, orpiment and realgar are the main minerals forming the ore. Lorandite – a thallium arsenic
197:. For some time, the thallium-rich part of the deposit was mined. The Crven Dol mine yielded
691:
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692:"Sedimentary-rock-hosted disseminated gold mineralization in the Alsar district, Macedonia"
194:
67:
668:
633:
590:
518:
426:
413:
Pavicevic, M (1988). "Lorandite from
Allchar — A low energy solar neutrino dosimeter".
357:
249:
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LORandite EXperiment (LOREX) is using lorandite from the ore deposit to determine the
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676:
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and the ore body still holds estimated amount of 500 t of thallium. The mineral
498:
Volkov, A. V.; Serafimovski, T.; Kochneva, N. T.; Tomson, I. N.; Tasev, G. (2006).
361:
168:
719:
526:
451:
Subotic, K. M.; Pavicevic, M. K. (1998). "Status of the LOREX: Geochemical".
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212:"Mineral collecting at Allchar is only allowed with permission from the
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500:"The Alshar epithermal Au-As-Sb-Tl deposit, southern Macedonia"
373:
485:"Allchar, Rožden, Kavadarci Municipality, North Macedonia"
372:,e)Pb process has a relatively low threshold energy of 52
364:
which undergoes a neutrino capturing reaction and yields
205:from this ore deposit can be used to determine the
142:
134:
129:
115:
110:
73:
63:
24:
577:, a new TI-sulfosalt from Allchar, Macedonia".
360:flux. This mineral contains large amounts of
8:
19:
18:
453:Exotic nuclei and atomic masses (ENAM 98)
391:
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321:
310:
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397:"Kozuf - untouched ecological nature"
248:started in the 15th century when the
7:
446:
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408:
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690:Perciva, T. J.; Radtke, AS (1994).
14:
228:, similar to those found in the
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34:
758:Geography of Macedonia (region)
1:
677:10.1016/0168-9002(88)90170-2
642:10.1016/0168-9002(88)90172-6
435:10.1016/0168-9002(88)90171-4
779:
763:Geological type localities
699:The Canadian Mineralogist
527:10.1134/S1075701506030020
29:
579:Mineralogy and Petrology
368:in the process. The Tl(ν
226:Carlin–type gold deposit
507:Geology of Ore Deposits
167:) is a low-temperature
155:(alternative spellings
191:Kavadarci Municipality
399:. Macedonia Timeless.
95:41.15694°N 21.94639°E
55:Location in Macedonia
455:. pp. 912–915.
214:University of Skopje
753:Mineral exploration
669:1988NIMPA.271..286J
634:1988NIMPA.271..297P
591:1995MinPe..53..125C
519:2006GeoOD..48..175V
427:1988NIMPA.271..287P
230:Carlin Unconformity
91: /
21:
599:10.1007/BF01171951
287:with formula TlAsS
100:41.15694; 21.94639
285:sulfosalt mineral
252:ruled this land.
224:The deposit is a
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16:Mine in Macedonia
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743:Mining in Europe
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421:(2): 287–296.
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358:solar neutrino
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250:Ottoman Empire
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207:solar neutrino
165:Alshar deposit
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748:Ore deposits
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169:hydrothermal
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152:
151:
738:Gold mining
293:jankovićite
98: /
74:Coordinates
732:Categories
720:mindat.org
705:: 649–665.
663:(2): 286.
628:(2): 297.
513:(3): 175.
381:References
331:bernardite
244:Mining of
111:Production
86:21°56′47″E
83:41°09′25″N
607:100802842
535:128807508
335:TI(Sb,As)
269:marcasite
203:lorandite
68:Macedonia
569:(As, Sb)
548:115-127.
366:lead-205
281:stibnite
279:Pyrite,
275:Minerals
261:orpiment
199:thallium
184:thallium
180:antimony
124:Thallium
116:Products
25:Location
665:Bibcode
630:Bibcode
587:Bibcode
515:Bibcode
423:Bibcode
346:vrbaite
316:fangite
305:(As,Sb)
257:realgar
246:Arsenic
220:Geology
187:deposit
176:arsenic
130:History
64:Country
605:
533:
467:
265:pyrite
240:Mining
234:Nevada
209:flux.
143:Closed
135:Opened
695:(PDF)
603:S2CID
531:S2CID
503:(PDF)
352:LOREX
465:ISBN
267:and
172:gold
146:1908
138:1880
120:Gold
717:at
673:doi
661:271
638:doi
626:271
595:doi
523:doi
457:doi
431:doi
419:271
374:keV
344:).
329:),
324:AsS
314:),
193:of
189:in
163:or
734::
703:32
701:.
697:.
671:.
659:.
636:.
624:.
601:.
593:.
583:53
581:.
575:22
565:Sb
553:^
529:.
521:.
511:48
509:.
505:.
463:.
443:^
429:.
417:.
405:^
388:^
348:.
320:Tl
311:22
301:Sb
297:Tl
259:,
236:.
232:,
159:,
122:,
679:.
675::
667::
644:.
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632::
609:.
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589::
573:S
571:4
567:9
563:5
537:.
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433::
425::
370:e
341:5
339:S
337:5
333:(
326:4
322:3
318:(
309:S
307:4
303:9
299:5
295:(
289:2
182:–
178:–
174:–
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