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Heavy mineral sands ore deposits

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Anecdotal reports of certain beach placers forming in modern times suggest that the greatest enrichment tended to occur in storm events energetic enough to remove most of the beach's sediment load—a process favoring the lighter minerals. The resultant 'clinker' sands left behind were mined during low
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rising from the ocean, may also cause a beach system to become stranded above the high-water mark and lock in the heavy mineral sands. Similarly, a beach system that is drowned by the subsidence of a coastline may be preserved, often for millions of years, until it either is covered by sedimentation
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The grade of a typical heavy mineral sand ore deposit is usually low. Within the 21st century, the lowest cut-off grades of heavy minerals, as a total heavy mineral (THM) concentrate from the bulk sand, in most ore deposits of this type is around 1% heavy minerals, although several are higher grade.
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Generally, as zircon is the most valuable component and a critical ore component, high-zircon sands are the most valuable. Thereafter, rutile, leucoxene and then ilmenite in terms of value given to the ore. As a generality, typically the valuable components of the THM concentrate rarely exceed 30%.
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The Tormin mine, on the Western Cape of South Africa's coastline, provides a unique ocean beach feature, which exposes the resource to wave and tidal conditions that result in a natural jigging effect. Large proportions of the quartz and light heavies waste material are removed by the ocean tidal
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The accumulation of a heavy mineral deposit requires a source of sediment containing heavy minerals onto a beach system in a volume which exceeds the rate of removal from the trap site. For this reason not all beaches which are supplied by sands containing heavy minerals will form economic
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operations that have gained public attention and galvanised environmental activism responses to mining proposals include the Tuart-Ludlow mineral sands mine, Western Australia, and the culmination of conservationist efforts to preserve
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The heavy minerals within the source sediments attain an economic concentration by accumulation within low-energy environments in streams and most usually on beaches. In beach placer deposits the lowest energy zone on the beach is the
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Being ancient stranded dune systems, the tonnage of most deposits is in excess of several tens of millions of tonnes to several hundred million tonnes. For example; the medium-sized Coburn mineral sands deposit,
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The size and position of a heavy mineral deposit is a function of the wave energy reaching the beach, the mean grainsize of the beach sediments, and the current height of the ocean.
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that feed the placer deposits are rich trap sites where the winnowing action of the waves is most efficient, because heavy minerals too heavy to be moved will deposit at an
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systems often are exploited for heavy mineral sands because they are from the ocean and because they are often remnants of previous
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and isolating stretches of coastline. The beaches are so isolated that they are sometimes processed in their entirety, down to the
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grains they accompany. It is for this reason that beach placer deposits are often referred to as "strand-line deposits".
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The source rocks which provide the heavy mineral sands determine the composition of the economic minerals. The source of
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The mining of beach sands and of fossilized beach placers is often controversial because the operation requires the
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tide following major storm events, suggesting that most beach placer deposits are formed during such cycles.
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of the mineral grains. It is equally likely that some concentrations of heavy minerals (aside from the usual
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Similar mineral sand mining operations were carried out for 35 years in and adjacent to National Parks at
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concentrations of the minerals. This factor can be qualitatively or quantitatively measured through the
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Slimes, typically minerals as above and heavy clay minerals, too fine to be economically extracted.
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of large areas. Often this land is in ecologically sensitive surroundings and contains fragile
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action, resulting in run of mine (ROM) grades as high as 86% heavy mineral concentrate (HMC).
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deposits is carried out in such an environmentally responsible manner, although some
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is host to economic diamantiferous beach sands, which are exploited by building
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Specific trap sites for heavy mineral sand placer deposits are in beaches on the
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The mining process is ideally modelled on the extraction operations underway in
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side of headlands, where low-energy zones trap sediments carried along by the
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Of this total heavy mineral concentrate (THM), the components are typically
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Examples of environmentally sensitive and politically sensitive mineral
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The source of heavy mineral sands is in a hardrock source within the
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Geelwal Karoo mineral sand deposit, on the west coast of
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into the ocean, where the sediments are caught up in
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Garnet is also sourced commonly from 732: 730: 632:mines do practice dune rehabilitation 108: 70:, and occasionally precious metals or 7: 847:adding citations to reliable sources 117:according to U.S. Geological Survey 1726:Volcanogenic massive sulfide (VMS) 858:"Heavy mineral sands ore deposits" 14: 617:operations, due to the advent of 16:Ore deposits of rare earth metals 1743: 1171: 823: 619:electrostatic mineral separation 303:, generally of 10% to 60% of THM 1706:Magmatic nickel-copper-iron-PGE 1696:Kambalda-type komatiitic nickel 834:needs additional citations for 624:In practice, not all mining of 1716:Sedimentary exhalative (SedEx) 667:in coastal Western Australia. 598:built up on poor sandy soils. 105:Grade and tonnage distribution 1: 1691:Iron oxide copper gold (IOCG) 676:Stradbroke Island, Queensland 635:. The mining of the coast of 113:in thousands of tons for 2006 111:Estimated ilmenite production 672:Hawks Nest, New South Wales 534:activity, which results in 1801: 1681:Carbonate-hosted lead-zinc 771:. May 2003. Archived from 58:, the industrial minerals 1739: 1167: 539:or rises from the ocean. 712:"U.S. Geological Survey" 1221:, mineral mixtures and 742:Mineral Commodities Ltd 514:intraglacial highstands 315:, from 1% to 10% of THM 309:, from 5% to 25% of THM 85:formed most usually in 586:Environmental concerns 528: 484: 374: 97:placers) exist within 28: 1731:Orogenic gold deposit 1676:Banded iron formation 522: 479: 372: 22: 843:improve this article 1750:Minerals portal 1686:Heavy mineral sands 1178:Minerals portal 626:sub-Saharan African 121: 56:rare-earth elements 32:Heavy mineral sands 674:, and continue on 529: 485: 375: 109: 29: 1775:Titanium minerals 1757: 1756: 1664: 1663: 1185: 1184: 1148:carbonate mineral 1085:Silicate minerals 1079: 1078: 952:Titanium minerals 919: 918: 911: 893: 554:developed at the 453:metamorphic rocks 442:metamorphic rocks 355:Western Australia 284: 283: 118: 1792: 1770:Economic geology 1748: 1747: 1746: 1701:Lateritic nickel 1657: 1645: 1633: 1621: 1609: 1597: 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717: 714: 710: 709: 705: 701: 684: 588: 568: 548:longshore drift 474: 461: 432:rocks, such as 391:longshore drift 367: 269:Other countries 114: 112: 107: 83:placer deposits 34:are a class of 17: 12: 11: 5: 1798: 1796: 1788: 1787: 1782: 1777: 1772: 1762: 1761: 1755: 1754: 1740: 1737: 1736: 1734: 1733: 1728: 1723: 1718: 1713: 1708: 1703: 1698: 1693: 1688: 1683: 1678: 1672: 1670: 1666: 1665: 1662: 1661: 1659: 1658: 1646: 1634: 1622: 1610: 1598: 1585: 1583: 1579: 1578: 1576: 1575: 1563: 1551: 1538: 1536: 1530: 1529: 1527: 1526: 1514: 1502: 1490: 1478: 1466: 1454: 1442: 1430: 1418: 1406: 1394: 1381: 1379: 1373: 1372: 1370: 1369: 1357: 1345: 1333: 1321: 1309: 1297: 1285: 1269: 1257: 1244: 1242: 1233: 1227: 1226: 1217: 1215: 1214: 1207: 1200: 1192: 1183: 1182: 1168: 1165: 1164: 1162: 1161: 1158:borate mineral 1151: 1140: 1138: 1134: 1133: 1131: 1130: 1125: 1120: 1118:Nenadkevichite 1115: 1110: 1105: 1100: 1095: 1089: 1087: 1081: 1080: 1077: 1076: 1074: 1073: 1068: 1063: 1058: 1053: 1048: 1043: 1038: 1033: 1028: 1026:Freudenbergite 1023: 1018: 1013: 1008: 1006:Aeschynite-(Y) 1002: 1000: 996: 995: 993: 992: 987: 982: 977: 971: 969: 962: 960:Oxide minerals 956: 955: 950: 948: 947: 940: 933: 925: 917: 916: 831: 829: 822: 816: 815: 789: 753: 726: 702: 700: 697: 696: 695: 690: 683: 680: 587: 584: 567: 564: 473: 470: 460: 457: 387:littoral drift 366: 363: 346: 345: 342: 316: 310: 304: 298: 282: 281: 278: 274: 273: 270: 266: 265: 260: 254: 253: 248: 242: 241: 236: 230: 229: 226: 220: 219: 216: 210: 209: 206: 200: 199: 196: 190: 189: 186: 180: 179: 176: 170: 169: 166: 160: 159: 156: 150: 149: 146: 140: 139: 136: 130: 129: 126: 106: 103: 77:Heavy mineral 15: 13: 10: 9: 6: 4: 3: 2: 1797: 1786: 1783: 1781: 1778: 1776: 1773: 1771: 1768: 1767: 1765: 1752: 1751: 1738: 1732: 1729: 1727: 1724: 1722: 1719: 1717: 1714: 1712: 1709: 1707: 1704: 1702: 1699: 1697: 1694: 1692: 1689: 1687: 1684: 1682: 1679: 1677: 1674: 1673: 1671: 1669:Deposit types 1667: 1655: 1650: 1647: 1643: 1638: 1635: 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Retrieved 804:. 7 Aug 2004 801: 792: 780:. Retrieved 773:the original 768: 756: 745:. Retrieved 741: 718:. Retrieved 706: 669: 649: 623: 613:rather than 600: 592:strip mining 589: 569: 541: 530: 525:South Africa 505: 501: 498: 486: 483:concentrates 462: 412:, sometimes 399: 376: 359: 351: 347: 321:, typically 289: 285: 262: 250: 238: 144:South Africa 119: 110: 76: 31: 30: 1505:Pentlandite 1481:Molybdenite 1248:Cassiterite 1108:Lorenzenite 1098:Grossmanite 1093:Aenigmatite 1066:Zirconolite 1061:Zimbabweite 1031:Haggertyite 1011:Armalcolite 688:Ore genesis 652:sand mining 621:processes. 607:groundwater 446:amphibolite 420:is usually 416:, and some 277:Total world 128:Production 1764:Categories 1649:Wolframite 1625:Sperrylite 1534:Carbonates 1517:Sphalerite 1486:molybdenum 1433:Chalcocite 1336:Pyrolusite 1154:Warwickite 1103:Keilhauite 1051:Perovskite 1046:Latrappite 1041:Keilhauite 985:Geikielite 869:newspapers 747:2016-08-08 738:"Projects" 720:2006-03-07 699:References 693:Black sand 611:dry mining 596:ecosystems 536:coastlines 507:Fossilised 490:swash zone 481:Black sand 444:, such as 434:kimberlite 426:ultramafic 246:Madagascar 234:Mozambique 99:streambeds 1637:Scheelite 1618:beryllium 1606:aluminium 1566:Malachite 1559:magnesium 1554:Magnesite 1547:magnesium 1457:Cobaltite 1397:Argentite 1385:Acanthite 1360:Uraninite 1348:Tantalite 1341:manganese 1324:Magnetite 1288:Columbite 1144:Sabinaite 1071:Zirkelite 1056:Polycrase 603:Australia 576:sea walls 552:sand bars 466:ZTR index 459:Transport 379:erosional 327:magnetite 313:Leucoxene 134:Australia 72:gemstones 40:zirconium 27:, India). 1654:tungsten 1642:tungsten 1630:platinum 1542:Dolomite 1445:Cinnabar 1377:Sulfides 1353:tantalum 1317:titanium 1312:Ilmenite 1300:Hematite 1281:tantalum 1265:chromium 1260:Chromite 1123:Titanite 1113:Melanite 1036:Ilmenite 1021:Euxenite 1016:Betafite 980:Brookite 682:See also 615:dredging 550:. Also, 532:Tectonic 418:ilmenite 414:tungsten 406:monazite 395:detritus 383:sediment 335:chromite 301:Ilmenite 125:Country 64:sapphire 52:tungsten 44:titanium 1721:Uranium 1601:Bauxite 1450:mercury 1409:Bornite 1365:uranium 1293:niobium 1277:niobium 975:Anatase 883:scholar 645:Ecuador 580:bedrock 572:Namibia 560:isthmus 544:leeward 449:schists 422:granite 365:Sources 339:kyanite 258:Senegal 224:Vietnam 194:Ukraine 60:diamond 48:thorium 25:Chennai 1594:barium 1589:Baryte 1571:copper 1510:nickel 1493:Pyrite 1469:Galena 1462:cobalt 1438:copper 1426:copper 1414:copper 1402:silver 1390:silver 1272:Coltan 1240:Oxides 990:Rutile 968:Simple 885:  878:  871:  864:  856:  808:15 May 782:15 May 769:epa.wa 494:quartz 438:basalt 410:rutile 402:zircon 331:garnet 323:quartz 319:Gangue 307:Rutile 295:Zircon 280:4,800 214:Brazil 174:Norway 154:Canada 138:1,140 68:garnet 1613:Beryl 1582:Other 1137:Other 999:Mixed 890:JSTOR 876:books 776:(PDF) 765:(PDF) 715:(PDF) 641:Chile 430:mafic 263:(150) 251:(700) 239:(750) 204:India 164:China 87:beach 79:sands 1785:Sand 1522:zinc 1498:iron 1474:lead 1329:iron 1305:iron 1279:and 1231:Ores 862:news 810:2016 784:2016 659:and 643:and 510:dune 472:Trap 428:and 337:and 272:120 228:100 218:130 208:200 198:220 188:300 178:380 168:400 158:809 148:952 95:gold 81:are 1253:tin 845:by 802:abc 436:or 389:or 36:ore 1766:: 800:. 767:. 740:. 729:^ 678:. 516:. 468:. 455:. 408:, 404:, 333:, 329:, 325:, 74:. 66:, 62:, 54:, 50:, 46:, 42:, 1656:) 1652:( 1644:) 1640:( 1632:) 1628:( 1620:) 1616:( 1608:) 1604:( 1596:) 1592:( 1573:) 1569:( 1561:) 1557:( 1549:) 1545:( 1524:) 1520:( 1512:) 1508:( 1500:) 1496:( 1488:) 1484:( 1476:) 1472:( 1464:) 1460:( 1452:) 1448:( 1440:) 1436:( 1428:) 1424:( 1416:) 1412:( 1404:) 1400:( 1392:) 1388:( 1367:) 1363:( 1355:) 1351:( 1343:) 1339:( 1331:) 1327:( 1319:) 1315:( 1307:) 1303:( 1295:) 1291:( 1283:) 1275:( 1267:) 1263:( 1255:) 1251:( 1211:e 1204:t 1197:v 1160:) 1156:( 1150:) 1146:( 944:e 937:t 930:v 912:) 906:( 901:) 897:( 887:· 880:· 873:· 866:· 839:. 812:. 786:. 750:. 723:. 527:.

Index


Chennai
ore
zirconium
titanium
thorium
tungsten
rare-earth elements
diamond
sapphire
garnet
gemstones
sands
placer deposits
beach
specific gravity
gold
streambeds
Australia
South Africa
Canada
China
Norway
United States
Ukraine
India
Brazil
Vietnam
Mozambique
Madagascar

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