427:
561:
2315:
87:
36:
1148:
album diaphanum. Hoc simile quartzo durum, distinctum quod cum aqua forti non, nisi post aliquot minuta & fero, effervescens." In translation: "Slow marble - Marble, white and transparent with barely discernable particles. This is as hard as quartz, but it is different in that it does not, unless after a few minutes, effervesce with "aqua forti"".
753:
Vast deposits of dolomite are present in the geological record, but the mineral is relatively rare in modern environments. Reproducible, inorganic low-temperature syntheses of dolomite are yet to be performed. Usually, the initial inorganic precipitation of a metastable "precursor" (such as magnesium
1147:
Linnaeus, C. (1768): Systema naturae per regnum tria naturae, secundum classes, ordines, genera, species cum characteribus & differentiis. Tomus III. Laurentii Salvii, Holmiae, 236 p. On p.41 of this very book, Linnaeus stated (in Latin): "Marmor tardum - Marmor paticulis subimpalpabilibus
912:
In addition to being an industrial mineral, dolomite is highly valued by collectors and museums when it forms large, transparent crystals. The specimens that appear in the magnesite quarry exploited in Eugui, Esteribar, Navarra (Spain) are considered among the best in the world.
754:
calcite) can easily be achieved. The precursor phase will theoretically change gradually into a more stable phase (such as partially ordered dolomite) during periodical intervals of dissolution and re-precipitation. The general principle governing the course of this irreversible
618:
system. It forms white, tan, gray, or pink crystals. Dolomite is a double carbonate, having an alternating structural arrangement of calcium and magnesium ions. Unless it is in fine powder form, it does not rapidly dissolve or effervesce (fizz) in cold dilute
900:
under layers of dolomite to enable the detectors to detect the highest possible number of exotic particles. Because dolomite contains relatively minor quantities of radioactive materials, it can insulate against interference from
874:, dolomite and dolomitic limestone are added to soils and soilless potting mixes as a pH buffer and as a magnesium source. Pastures can be limed with dolomitic lime to raise their pH and where there is a magnesium deficiency.
653:. Small amounts of iron in the structure give the crystals a yellow to brown tint. Manganese substitutes in the structure also up to about three percent MnO. A high manganese content gives the crystals a rosy pink color.
1268:
Snyder, Glen T.; Matsumoto, Ryo; Suzuki, Yohey; Kouduka, Mariko; Kakizaki, Yoshihiro; Zhang, Naizhong; Tomaru, Hitoshi; Sano, Yuji; Takahata, Naoto; Tanaka, Kentaro; Bowden, Stephen A. (2020-02-05).
762:". High diagenetic temperatures, such as those of groundwater flowing along deeply rooted fault systems affecting some sedimentary successions or deeply buried limestone rocks allocate
1380:
Vasconcelos C.; McKenzie J. A.; Bernasconi S.; Grujic D.; Tien A. J. (1995). "Microbial mediation as a possible mechanism for natural dolomite formation at low temperatures".
1221:
Petrash, Daniel A.; Bialik, Or M.; Bontognali, Tomaso R.R.; Vasconcelos, Crisógono; Roberts, Jennifer A.; McKenzie, Judith A.; Konhauser, Kurt O. (2017-08-01).
1721:
57:
1601:
742:
have been also found to mediate in dolomite formation. In general, low-temperature dolomite may occur in natural supersaturated environments rich in
789:
proceeds in the presence of manganese(II). A still perplexing example of an organogenic origin is that of the reported formation of dolomite in the
1485:
446:
of a thin section in cross and plane polarised light: the brighter mineral grains in the picture are dolomite, and the darker grains are calcite.
2265:
730:, but also in sedimentary basins bearing gas hydrates and hypersaline lakes. It is often thought that dolomite nucleates with the help of
686:
Because dolomite can be dissolved by slightly acidic water, areas where dolomite is an abundant rock-forming mineral are important as
44:
2295:
1199:
1125:
1038:
2250:
405:
2374:
722:, namely, Lagoa Vermelha and Brejo do Espinho. There are many other localities where modern dolomite forms, notably along
2260:
1702:
1055:
778:
could play a key role in dolomitization, since diagenetic fluids of contrasting composition are mixed as a response to
877:
Dolomite is also used as the substrate in marine (saltwater) aquariums to help buffer changes in the pH of the water.
1184:
1119:
1023:
743:
2255:
1718:
146:
2285:
1081:
603:
580:
1779:
291:
2384:
2270:
2389:
1423:
Roberts, J. A.; Kenward, P. A.; Fowle, D. A.; Goldstein, R. H.; Gonzalez, L. A. & Moore, D. S. (1980).
1507:
1222:
595:
2354:
2349:
1334:
1482:
426:
2369:
2339:
1665:
Mansfield, Charles F. (1980). "A urolith of biogenic dolomite – another clue in the dolomite mystery".
746:
and microbial cell surfaces. This is likely result from complexation of both magnesium and calcium by
2344:
786:
731:
17:
1788:
1553:
Petrash, Daniel A.; Bialik, Or M.; Staudigel, Philip T.; Konhauser, Kurt O.; Budd, David A. (2021).
2364:
1757:
2359:
2280:
825:
703:
136:
49:
1138:
Saussure le fils, M. de (1792): Analyse de la dolomie. Journal de
Physique, vol.40, pp.161-173.
759:
665:
also can substitute in the structure for magnesium. The mineral dolomite is closely related to
598:(1750–1801), first in buildings of the old city of Rome, and later as samples collected in the
206:
2300:
2245:
281:
271:
1554:
1674:
1613:
1519:
1436:
1389:
1346:
1281:
1234:
979:
906:
739:
572:
564:
1270:"Evidence in the Japan Sea of microdolomite mineralization within gas hydrate microbiomes"
8:
2275:
1196:
940:
779:
526:
314:
304:
246:
Tabular crystals, often with curved faces, also columnar, stalactitic, granular, massive.
1678:
1617:
1523:
1440:
1422:
1393:
1350:
1285:
1238:
983:
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of iron and steel. Large quantities of processed dolomite are used in the production of
2379:
1772:
1647:
1582:
1459:
1424:
1405:
1310:
1269:
1035:
997:
785:
A recent biotic synthetic experiment claims to have precipitated ordered dolomite when
435:
261:
1531:
2019:
1686:
1651:
1639:
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1535:
1464:
1362:
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1019:
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897:
856:
620:
519:
400:
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108:
1555:"Biogeochemical reappraisal of the freshwater–seawater mixing-zone diagenetic model"
1246:
931: – Water-soluble mineral deposit formed by evaporation from an aqueous solution
1682:
1629:
1621:
1566:
1527:
1454:
1444:
1425:"Surface chemistry allows for abiotic precipitation of dolomite at low temperature"
1409:
1397:
1354:
1305:
1289:
1242:
987:
934:
628:
456:
342:
324:
251:
236:
White, grey to pink, reddish-white, brownish-white; colourless in transmitted light
115:
1379:
1335:"Lacustrine dolomite—an overview of modern, Holocene, and Pleistocene occurrences"
2319:
1725:
1706:
1489:
1203:
1109:
1042:
810:
806:
794:
790:
747:
707:
599:
588:
560:
552:). An alternative name sometimes used for the dolomitic rock type is dolostone.
549:
443:
1429:
Proceedings of the
National Academy of Sciences of the United States of America
1293:
922:
805:
Dolomite is used as an ornamental stone, a concrete aggregate, and a source of
775:
763:
715:
634:
545:
179:
156:
1699:
1158:
2333:
1765:
1643:
1578:
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1366:
1301:
1254:
946:
821:
770:
platforms never subjected to elevated temperatures. Under such conditions of
584:
366:
241:
168:
1449:
1059:
1990:
1468:
1319:
889:
871:
755:
727:
439:
396:
1719:
Short Sharp
Science: Particle quest: Hunting for Italian WIMPs underground
2290:
2074:
2050:
1817:
1634:
1508:"Dolomite: occurrence, evolution and economically important associations"
864:
650:
542:
191:
992:
967:
855:
is uncommon or too costly, dolomite is sometimes used in its place as a
2218:
2194:
2086:
2055:
2002:
1905:
1223:"Microbially catalyzed dolomite formation: From near-surface to burial"
902:
833:
771:
379:
1792:
1738:
Calvo M.; Sevillano, E. (1991). "The Eugui quarries, Navarra, Spain".
1570:
1085:
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2135:
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2123:
2116:
2103:
2026:
1966:
1954:
1929:
1917:
1910:
1893:
1857:
1625:
1401:
928:
852:
818:
814:
646:
592:
568:
516:
1602:"Formation of ordered dolomite in anaerobic photosynthetic biofilms"
2223:
2211:
2199:
2014:
1922:
1886:
1881:
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1850:
1834:
1829:
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86:
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1978:
1946:
1934:
1862:
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849:
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624:
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431:
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at high temperature. Particle physics researchers like to build
35:
2163:
2158:
2140:
2079:
2062:
2038:
2031:
2007:
1995:
1983:
1971:
1959:
1841:
1700:
A Review of the
Literature on Catalytic Biomass Tar Destruction
1552:
845:
723:
719:
711:
662:
2182:
1809:
691:
575:, Italy. The Dolomite Mountains were named after the mineral.
442:
can be etched and stained in order to identify the minerals.
1267:
766:. But the mineral is also volumetrically important in some
2091:
2067:
2043:
1898:
1874:
841:
837:
658:
654:
638:
587:
in 1768. In 1791, it was described as a rock by the French
507:
498:
483:
474:
92:
1045:. Handbook of Mineralogy. (PDF) . Retrieved on 2011-10-10.
465:
1822:
1800:
1728:. Newscientist.com (2011-09-05). Retrieved on 2011-10-10.
885:
829:
824:
rock, and serves as the host rock for large strata-bound
797:
dog, possibly as the result of an illness or infection.
702:
Modern dolomite formation has been found to occur under
606:
first named the mineral (after
Dolomieu) in March 1792.
1600:
Daye, Mirna; Higgins, John; Bosak, Tanja (2019-06-01).
1483:"Low-temperature nucleation of magnesite and dolomite"
1737:
1664:
583:
the mineral dolomite was probably first described by
477:
504:
495:
486:
468:
462:
492:
480:
459:
1108:Krauskopf, Konrad Bates; Bird, Dennis K. (1995).
2331:
1599:
937: – List of minerals with Knowledge articles
1014:Deer, W. A., R. A. Howie and J. Zussman (1966)
1175:Klein, Cornelis and Cornelius S. Hurlbut Jr.,
1773:
1107:
925: – Geological process producing dolomite
548:composed mostly of the mineral dolomite (see
1016:An Introduction to the Rock Forming Minerals
949: – Rock formation in the Alps of Europe
266:3 directions of cleavage not at right angles
943: – Suite of carbonate rocks in England
501:
471:
1780:
1766:
1206:. USGS Fact Sheet. Retrieved on 2013-9-10.
1633:
1458:
1448:
1309:
991:
614:The mineral dolomite crystallizes in the
1159:"Dolomite Mineral - Uses and Properties"
744:extracellular polymeric substances (EPS)
559:
425:
60:of all important aspects of the article.
1114:(3rd ed.). New York: McGraw-Hill.
14:
2332:
1505:
1098:. Mindat.org. Retrieved on 2011-10-10.
56:Please consider expanding the lead to
1761:
1709:National Renewable Energy Laboratory.
1216:
1214:
1212:
1169:
1332:
968:"IMA–CNMNC approved mineral symbols"
965:
880:Calcined dolomite is also used as a
29:
758:reaction has been coined "breaking
24:
2296:Volcanogenic massive sulfide (VMS)
1209:
25:
2401:
1753:
2313:
1128:from the original on 2017-02-26.
455:
85:
34:
2276:Magmatic nickel-copper-iron-PGE
2266:Kambalda-type komatiitic nickel
1731:
1712:
1693:
1667:Geochimica et Cosmochimica Acta
1658:
1593:
1546:
1499:
1475:
1416:
1373:
1333:Last, William M. (1990-05-01).
1326:
1261:
1247:10.1016/j.earscirev.2017.06.015
1189:
48:may be too short to adequately
2286:Sedimentary exhalative (SedEx)
1494:Neues Jahrbuch für Mineralogie
1151:
1141:
1132:
1101:
1074:
1048:
1029:
1008:
959:
774:the long-term activity of the
256:Common as simple contact twins
58:provide an accessible overview
27:Carbonate mineral - CaMg(CO₃)₂
13:
1:
2261:Iron oxide copper gold (IOCG)
1532:10.1016/S0012-8252(00)00022-2
953:
637:exists between dolomite, the
609:
413:values vary between 10 and 10
1687:10.1016/0016-7037(80)90264-1
1359:10.1016/0012-8252(90)90004-F
1179:Wiley, 20th ed., p. 339-340
1111:Introduction to geochemistry
1084:. mindat.org. Archived from
1058:. webmineral. Archived from
697:
604:Nicolas-Théodore de Saussure
581:Nicolas-Théodore de Saussure
541:The term is also used for a
7:
2375:Minerals in space group 148
1496:, Monatshefte, pp. 289–302.
916:
10:
2406:
2251:Carbonate-hosted lead-zinc
1294:10.1038/s41598-020-58723-y
736:Desulfovibrio brasiliensis
555:
2309:
2238:
2151:
2102:
1945:
1808:
1799:
1506:Warren, J. (2000-11-01).
787:anoxygenic photosynthesis
732:sulfate-reducing bacteria
596:Déodat Gratet de Dolomieu
417:
391:
384:Poorly soluble in dilute
378:
365:
341:
333:
323:
313:
303:
290:
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260:
250:
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232:
227:
205:
190:
167:
155:
145:
135:
114:
104:
99:
84:
79:
1740:The Mineralogical Record
1018:, Longman, pp. 489–493.
399:white to pink under UV;
1791:, mineral mixtures and
1450:10.1073/pnas.1305403110
826:Mississippi Valley-Type
800:
1481:Deelman, J.C. (1999):
972:Mineralogical Magazine
813:for the production of
576:
447:
2301:Orogenic gold deposit
2246:Banded iron formation
1512:Earth-Science Reviews
1339:Earth-Science Reviews
1227:Earth-Science Reviews
1177:Manual of Mineralogy,
817:. It is an important
740:microbial metabolisms
714:such as those at the
616:trigonal-rhombohedral
563:
434:look similar under a
429:
392:Other characteristics
147:Strunz classification
2385:Luminescent minerals
907:background radiation
809:, as well as in the
571:mountain range near
91:Dolomite (white) on
2390:Industrial minerals
2320:Minerals portal
2256:Heavy mineral sands
1679:1980GeCoA..44..829M
1618:2019Geo....47..509D
1524:2000ESRv...52....1W
1441:2013PNAS..11014540R
1394:1995Natur.377..220V
1351:1990ESRv...27..221L
1286:2020NatSR..10.1876S
1239:2017ESRv..171..558P
993:10.1180/mgm.2021.43
984:2021MinM...85..291W
966:Warr, L.N. (2021).
941:Magnesian Limestone
884:for destruction of
780:Milankovitch cycles
760:Ostwald's step rule
694:terrain formation.
527:magnesium carbonate
2355:Carbonate minerals
2350:Magnesium minerals
1724:2017-05-17 at the
1705:2015-02-04 at the
1488:2008-04-09 at the
1274:Scientific Reports
1202:2013-06-04 at the
1041:2008-04-09 at the
905:without adding to
898:particle detectors
690:and contribute to
577:
448:
334:Optical properties
309:Vitreous to pearly
109:Carbonate minerals
2370:Trigonal minerals
2340:Sedimentary rocks
2327:
2326:
2234:
2233:
1571:10.1111/sed.12849
1388:(6546): 220–222.
1195:Kaufmann, James.
621:hydrochloric acid
573:Cortina d'Ampezzo
520:carbonate mineral
424:
423:
75:
74:
16:(Redirected from
2397:
2345:Calcium minerals
2318:
2317:
2316:
2271:Lateritic nickel
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1565:(5): 1797–1830.
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1005:
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963:
935:List of minerals
750:comprising EPS.
748:carboxylic acids
682:
629:Crystal twinning
540:
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401:triboluminescent
343:Refractive index
325:Specific gravity
296:
219:= 16.002 ;
201:
185:
176:
121:
120:(repeating unit)
89:
77:
76:
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61:
38:
30:
21:
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2365:Dolomite (rock)
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1034:
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1013:
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919:
811:Pidgeon process
807:magnesium oxide
803:
791:urinary bladder
700:
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677:
673:
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612:
558:
550:Dolomite (rock)
538:
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43:This article's
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2360:Dolomite group
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2012:
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1754:External links
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1692:
1673:(6): 829–839.
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1612:(6): 509–512.
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1028:
1007:
978:(3): 291–320.
957:
955:
952:
951:
950:
944:
938:
932:
926:
923:Dolomitization
918:
915:
802:
799:
776:deep biosphere
764:dolomitization
716:Rio de Janeiro
708:supersaturated
706:conditions in
699:
696:
679:
675:
671:
635:Solid solution
611:
608:
557:
554:
546:carbonate rock
536:
532:
422:
421:
419:
415:
414:
409:
393:
389:
388:
382:
376:
375:
369:
363:
362:
358:
353:= 1.679–1.681
350:
345:
339:
338:
335:
331:
330:
327:
321:
320:
317:
311:
310:
307:
301:
300:
297:
288:
287:
284:
278:
277:
274:
268:
267:
264:
258:
257:
254:
248:
247:
244:
238:
237:
234:
230:
229:
228:Identification
225:
224:
223: = 3
209:
203:
202:
194:
188:
187:
173:Rhombohedral (
171:
165:
164:
159:
157:Crystal system
153:
152:
149:
143:
142:
139:
133:
132:
129:
125:
122:
112:
111:
106:
102:
101:
97:
96:
90:
82:
81:
73:
72:
52:the key points
42:
40:
33:
26:
9:
6:
4:
3:
2:
2402:
2391:
2388:
2386:
2383:
2381:
2378:
2376:
2373:
2371:
2368:
2366:
2363:
2361:
2358:
2356:
2353:
2351:
2348:
2346:
2343:
2341:
2338:
2337:
2335:
2322:
2321:
2308:
2302:
2299:
2297:
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2289:
2287:
2284:
2282:
2279:
2277:
2274:
2272:
2269:
2267:
2264:
2262:
2259:
2257:
2254:
2252:
2249:
2247:
2244:
2243:
2241:
2239:Deposit types
2237:
2225:
2220:
2217:
2213:
2208:
2205:
2201:
2196:
2193:
2189:
2184:
2181:
2177:
2172:
2169:
2165:
2160:
2157:
2156:
2154:
2150:
2142:
2137:
2134:
2130:
2125:
2122:
2118:
2113:
2110:
2109:
2107:
2105:
2101:
2093:
2088:
2085:
2081:
2076:
2073:
2069:
2064:
2061:
2057:
2052:
2049:
2045:
2040:
2037:
2033:
2028:
2025:
2021:
2016:
2013:
2009:
2004:
2001:
1997:
1992:
1989:
1985:
1980:
1977:
1973:
1968:
1965:
1961:
1956:
1953:
1952:
1950:
1948:
1944:
1936:
1931:
1928:
1924:
1919:
1916:
1912:
1907:
1904:
1900:
1895:
1892:
1888:
1883:
1880:
1876:
1871:
1868:
1864:
1859:
1856:
1852:
1848:
1843:
1840:
1836:
1831:
1828:
1824:
1819:
1816:
1815:
1813:
1811:
1807:
1804:
1802:
1798:
1794:
1790:
1783:
1778:
1776:
1771:
1769:
1764:
1763:
1760:
1745:
1741:
1734:
1727:
1723:
1720:
1715:
1708:
1704:
1701:
1696:
1688:
1684:
1680:
1676:
1672:
1668:
1661:
1653:
1649:
1645:
1641:
1636:
1635:1721.1/126802
1631:
1627:
1623:
1619:
1615:
1611:
1607:
1603:
1596:
1588:
1584:
1580:
1576:
1572:
1568:
1564:
1560:
1559:Sedimentology
1556:
1549:
1541:
1537:
1533:
1529:
1525:
1521:
1518:(1–3): 1–81.
1517:
1513:
1509:
1502:
1495:
1491:
1487:
1484:
1478:
1470:
1466:
1461:
1456:
1451:
1446:
1442:
1438:
1434:
1430:
1426:
1419:
1411:
1407:
1403:
1399:
1395:
1391:
1387:
1383:
1376:
1368:
1364:
1360:
1356:
1352:
1348:
1344:
1340:
1336:
1329:
1321:
1317:
1312:
1307:
1303:
1299:
1295:
1291:
1287:
1283:
1279:
1275:
1271:
1264:
1256:
1252:
1248:
1244:
1240:
1236:
1232:
1228:
1224:
1217:
1215:
1213:
1205:
1201:
1198:
1192:
1186:
1185:0-471-80580-7
1182:
1178:
1172:
1164:
1160:
1154:
1144:
1135:
1127:
1123:
1121:9780070358201
1117:
1113:
1112:
1104:
1088:on 2015-11-18
1087:
1083:
1077:
1062:on 2005-08-27
1061:
1057:
1051:
1044:
1040:
1037:
1032:
1025:
1024:0-582-44210-9
1021:
1017:
1011:
1003:
999:
994:
989:
985:
981:
977:
973:
969:
962:
958:
948:
947:Main Dolomite
945:
942:
939:
936:
933:
930:
927:
924:
921:
920:
914:
910:
908:
904:
899:
895:
891:
887:
883:
878:
875:
873:
868:
866:
862:
858:
854:
851:
847:
843:
839:
835:
831:
827:
823:
820:
816:
812:
808:
798:
796:
792:
788:
783:
781:
777:
773:
769:
765:
761:
757:
751:
749:
745:
741:
738:), but other
737:
733:
729:
725:
721:
717:
713:
709:
705:
695:
693:
689:
684:
668:
664:
660:
656:
652:
648:
644:
640:
636:
632:
630:
626:
622:
617:
607:
605:
601:
600:Tyrolean Alps
597:
594:
590:
586:
585:Carl Linnaeus
582:
579:As stated by
574:
570:
566:
562:
553:
551:
547:
544:
528:
525:
521:
518:
512:
452:
445:
441:
440:thin sections
437:
433:
430:Dolomite and
428:
420:
416:
412:
408:
402:
398:
394:
390:
387:
383:
381:
377:
374:= 0.179–0.181
373:
370:
368:
367:Birefringence
364:
357:
349:
346:
344:
340:
336:
332:
328:
326:
322:
318:
316:
312:
308:
306:
302:
298:
293:
289:
285:
283:
279:
275:
273:
269:
265:
263:
259:
255:
253:
249:
245:
243:
242:Crystal habit
239:
235:
231:
226:
222:
218:
214:= 4.8012(1),
213:
210:
208:
204:
198:
195:
193:
189:
181:
172:
170:
169:Crystal class
166:
163:
160:
158:
154:
150:
148:
144:
140:
138:
134:
123:
117:
113:
110:
107:
103:
98:
94:
88:
83:
78:
69:
59:
53:
51:
46:
41:
37:
32:
31:
19:
2311:
2111:
1991:Chalcopyrite
1793:ore deposits
1789:Ore minerals
1743:
1739:
1733:
1714:
1695:
1670:
1666:
1660:
1609:
1605:
1595:
1562:
1558:
1548:
1515:
1511:
1501:
1493:
1477:
1432:
1428:
1418:
1385:
1381:
1375:
1342:
1338:
1328:
1277:
1273:
1263:
1230:
1226:
1191:
1176:
1171:
1162:
1153:
1143:
1134:
1110:
1103:
1090:. Retrieved
1086:the original
1076:
1064:. Retrieved
1060:the original
1050:
1031:
1015:
1010:
975:
971:
961:
911:
890:gasification
879:
876:
872:horticulture
869:
832:deposits of
804:
784:
752:
735:
728:Persian Gulf
701:
685:
633:
613:
578:
522:composed of
450:
449:
406:
371:
355:
347:
337:Uniaxial (−)
220:
216:
211:
196:
63:
47:
45:lead section
2075:Pentlandite
2051:Molybdenite
1818:Cassiterite
1280:(1): 1876.
1233:: 558–582.
1163:geology.com
903:cosmic rays
865:float glass
834:base metals
756:geochemical
651:kutnohorite
631:is common.
543:sedimentary
192:Space group
2334:Categories
2219:Wolframite
2195:Sperrylite
2104:Carbonates
2087:Sphalerite
2056:molybdenum
2003:Chalcocite
1906:Pyrolusite
1746:: 137–142.
1082:"Dolomite"
1056:"Dolomite"
954:References
772:diagenesis
649:-dominant
641:-dominant
610:Properties
589:naturalist
529:, ideally
436:microscope
418:References
380:Solubility
292:Mohs scale
276:Conchoidal
180:H–M symbol
137:IMA symbol
2380:Evaporite
2207:Scheelite
2188:beryllium
2176:aluminium
2136:Malachite
2129:magnesium
2124:Magnesite
2117:magnesium
2027:Cobaltite
1967:Argentite
1955:Acanthite
1930:Uraninite
1918:Tantalite
1911:manganese
1894:Magnetite
1858:Columbite
1652:146426700
1644:0091-7613
1587:234012426
1579:1365-3091
1540:0012-8252
1367:0012-8252
1302:2045-2322
1255:0012-8252
1197:Sinkholes
1002:235729616
929:Evaporite
853:limestone
822:reservoir
819:petroleum
815:magnesium
795:Dalmatian
718:coast of
704:anaerobic
698:Formation
647:manganese
593:geologist
569:Dolomites
565:Cristallo
517:anhydrous
397:fluoresce
329:2.84–2.86
207:Unit cell
66:July 2023
50:summarize
18:Dolomitic
2224:tungsten
2212:tungsten
2200:platinum
2112:Dolomite
2015:Cinnabar
1947:Sulfides
1923:tantalum
1887:titanium
1882:Ilmenite
1870:Hematite
1851:tantalum
1835:chromium
1830:Chromite
1722:Archived
1703:Archived
1486:Archived
1469:23964124
1320:32024862
1200:Archived
1126:Archived
1092:12 March
1066:12 March
1039:Archived
1036:Dolomite
917:See also
909:levels.
882:catalyst
861:smelting
859:for the
848:. Where
836:such as
688:aquifers
645:and the
643:ankerite
515:) is an
451:Dolomite
295:hardness
282:Tenacity
272:Fracture
262:Cleavage
252:Twinning
162:Trigonal
105:Category
80:Dolomite
2291:Uranium
2171:Bauxite
2020:mercury
1979:Bornite
1935:uranium
1863:niobium
1847:niobium
1675:Bibcode
1614:Bibcode
1606:Geology
1520:Bibcode
1460:3767548
1437:Bibcode
1410:4371495
1390:Bibcode
1347:Bibcode
1311:7002378
1282:Bibcode
1235:Bibcode
980:Bibcode
894:biomass
888:in the
850:calcite
768:Neogene
726:in the
724:sabkhas
712:lagoons
710:saline
667:huntite
625:calcite
567:in the
556:History
531:CaMg(CO
524:calcium
432:calcite
361:= 1.500
299:3.5–4.0
286:Brittle
151:5.AB.10
124:CaMg(CO
116:Formula
100:General
2164:barium
2159:Baryte
2141:copper
2080:nickel
2063:Pyrite
2039:Galena
2032:cobalt
2008:copper
1996:copper
1984:copper
1972:silver
1960:silver
1842:Coltan
1810:Oxides
1650:
1642:
1585:
1577:
1538:
1467:
1457:
1408:
1382:Nature
1365:
1318:
1308:
1300:
1253:
1183:
1118:
1022:
1000:
846:copper
844:, and
828:(MVT)
734:(e.g.
720:Brazil
663:cobalt
661:, and
627:does.
438:, but
315:Streak
305:Luster
2183:Beryl
2152:Other
1648:S2CID
1583:S2CID
1406:S2CID
998:S2CID
793:of a
692:karst
674:Ca(CO
319:White
233:Color
2092:zinc
2068:iron
2044:lead
1899:iron
1875:iron
1849:and
1801:Ores
1640:ISSN
1575:ISSN
1536:ISSN
1465:PMID
1363:ISSN
1316:PMID
1298:ISSN
1251:ISSN
1181:ISBN
1116:ISBN
1094:2024
1068:2024
1020:ISBN
857:flux
842:zinc
838:lead
801:Uses
659:zinc
655:Lead
639:iron
591:and
395:May
93:talc
1823:tin
1683:doi
1630:hdl
1622:doi
1567:doi
1528:doi
1455:PMC
1445:doi
1433:110
1398:doi
1386:337
1355:doi
1306:PMC
1290:doi
1243:doi
1231:171
988:doi
892:of
886:tar
870:In
830:ore
623:as
386:HCl
182:: (
141:Dol
2336::
1744:22
1742:.
1681:.
1671:44
1669:.
1646:.
1638:.
1628:.
1620:.
1610:47
1608:.
1604:.
1581:.
1573:.
1563:68
1561:.
1557:.
1534:.
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1516:52
1514:.
1510:.
1492:,
1463:.
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1443:.
1431:.
1427:.
1404:.
1396:.
1384:.
1361:.
1353:.
1343:27
1341:.
1337:.
1314:.
1304:.
1296:.
1288:.
1278:10
1276:.
1272:.
1249:.
1241:.
1229:.
1225:.
1211:^
1161:.
1124:.
996:.
986:.
976:85
974:.
970:.
867:.
840:,
782:.
683:.
670:Mg
657:,
602:.
511:-/
499:oʊ
484:aɪ
410:sp
403:.
177:)
2226:)
2222:(
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2210:(
2202:)
2198:(
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2174:(
2166:)
2162:(
2143:)
2139:(
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2127:(
2119:)
2115:(
2094:)
2090:(
2082:)
2078:(
2070:)
2066:(
2058:)
2054:(
2046:)
2042:(
2034:)
2030:(
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2018:(
2010:)
2006:(
1998:)
1994:(
1986:)
1982:(
1974:)
1970:(
1962:)
1958:(
1937:)
1933:(
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1921:(
1913:)
1909:(
1901:)
1897:(
1889:)
1885:(
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1873:(
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1861:(
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1845:(
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1821:(
1781:e
1774:t
1767:v
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1632::
1624::
1616::
1589:.
1569::
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1530::
1522::
1471:.
1447::
1439::
1412:.
1400::
1392::
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1357::
1349::
1322:.
1292::
1284::
1257:.
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1237::
1165:.
1096:.
1070:.
1026:.
1004:.
990::
982::
680:4
678:)
676:3
672:3
539:.
537:2
535:)
533:3
508:ə
505:l
502:.
496:d
493:ˈ
490:,
487:t
481:m
478:ˌ
475:ə
472:.
469:l
466:ɒ
463:d
460:ˈ
457:/
453:(
407:K
372:δ
359:ε
356:n
351:ω
348:n
221:Z
217:c
212:a
200:3
197:R
186:)
184:3
175:3
130:2
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20:)
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