Knowledge (XXG)

Geology of Niger

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288:, with estimated reserves of 200,000 tons. Low global demand for uranium has driven down production for more than 30 years since 1986. There may be other reserves at Imouraren, Afasto Ouest, Abkorum-Azelik, Afasto Est, Tassa N'Taghalgue and Teguida N'Tessoun, with uranium concentrations ranging between 0.22 and 0.45 percent. Molybdenum is often produced as a byproduct of uranium mining. Niger also has vein-type copper deposits, with 185:
ring complexes with significant variety in structure and rock type formed in the Air Massif. In fact, the Air Massif has the largest ring-dike in the world, with a diameter of 65 kilometers. Geologists subdivide the different ring complexes into three different types. The Taghouaji-type has plutonic
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in the Abuzegueur overthurst, in the Air region also show potential for platinum mineralization and may also have chromite, nickel and cobalt. The Fantio deposit in the Liptako area has heavily weathered ultra-mafic rocks, with 0.8 percent nickel, totaling up to as much as 200,000 tons. Makalondi,
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and small amounts of petroleum. The Liptako area in the northeast is the terminus of the West African gold belt, which extends from the Atlantic in Ghana. It hosts gold in the Birimian greenstones of Tera-Gasso and Gorouel belts. The gold belt actually extends further east, past the Niger River,
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Mined uranium is Niger's biggest export, but mining remains a relatively small part of GDP. The country also has gold and coal and deposits of tin and phosphate were mined in the past. Uranium is extracted from two concessions at Arlit and Akouta, more than 200 kilometers northwest of
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Relatively low-grade coal formed in a small basin at Anou-Araren, with estimated reserves of 10 megatons. Because of its poor quality, it is mainly used to provide electricity for uranium mines. The Iullemeden Basin contains
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rocks, with the oldest rocks near the edge of the basin. After the 50 percent of basement rocks that are metamorphic, the rest of the rocks in the Air Massif Renatt type and Dabaga type granite, which formed during the
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Iron is common in Niger, in rocks from the Precambrian through the Cenozoic, although the Cenozoic rocks of the Termit-Agadem and Ader-Doutchi regions have the highest iron concentrations, at up to 55 percent.
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but is largely concealed by younger sediments and sedimentary rocks. Gold mineralization also occurs in shear-related quartz veins. Some gold has been freed from sulfides in these veins by
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alkaline rocks and may have peralluminous granites while the Goudai-type is mainly acid volcanic rocks. The Ofoud-type is the most varied, encompassing gabbros, granites and anorthosite.
321:. Silver mineralization occurs where greenstones and granite intrusions meet, in the same quartz veins that host gold and sulfides. The silver is typically mineralized within 134:. More than half of the basement rock in the massif is metamorphic, including the Edoukel mesozonal micaschist, Azanguerene gneiss, Tafourfouzete letpynite and possible 845: 615: 178:
formed ring complexes, that now comprise 30 different massifs in the Niger-Nigerian Younger Granite Province. The oldest, Cambrian massifs formed in the north.
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Favreau; et al. (2009). "Estimating specific yield and transmissivity with magnetic resonance sounding in an unconfined sandstone aquifer (Niger)".
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comprises very ancient igneous and metamorphic crystalline basement rocks in the west, more than 2.2 billion years old formed in the late
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hosted, granite and sedimentary deposits of tin were mined commercially from 1984 until 1991 in the Air Massif. Today, only small scale
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sediments. The Tidekelt region has up to 25 million tons of salt brines, with a yield of 70 percent sodium chloride.
197:. Sedimentary rocks from the Paleozoic, thicken toward the mountains and to the south. East of Tamesna, Cambrian and 530: 111:
gneiss which are younger. These rocks formed after a granite-gneiss complex in the area, but before the mudstones,
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between these deposits and glacial sediments, associated with the widespread glaciation and global cooling of the
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of the Amarasinde and Bellekoire beds. These Upper Birimian Supergroup rocks are intruded by younger granites.
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associated with molybdenum, lithium and silver—or zinc and lead in the Proche-Tenere District. Native copper,
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The Iullemeden Basin at Tamesna began to form in the Paleozoic. The center of the basin was uplifted by the
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There are some indications of platinum in the Makalondi District, south of Liptako, associated with
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sedimentary rocks are up to 500 meters thick and include conglomerates and sandstones. There is an
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weathering including uranium, molybdenum, iron, coal, silver, nickel, cobalt and other resources.
52:, along with numerous ring complexes, as the region experienced events such as glaciation and the 897: 888: 810: 780: 765: 750: 740: 730: 695: 690: 640: 585: 560: 489: 354: 92: 820: 815: 755: 710: 670: 565: 546: 190: 795: 700: 685: 665: 655: 630: 570: 481: 402: 252: 194: 263:, before drying out and shifting from marine sediment deposition to continental sediments. 805: 715: 605: 79:
rocks common in much of West Africa. The pre-Birimian crystalline basement rocks include
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topped off the Iulllemeden Basin with marine sedimentary rocks, often on top of
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terrestrial sedimentary rocks. The region remained flooded well into the
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also in Liptako, hosts chromium concentrations of 5.1 to 17.4 percent.
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weathering due to heavy rainfall in the last 2.5 million years of the
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is overlain by shales and limestones, which contain coral and
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Continental Terminal is an unconfined sandstone aquifer.
209:. In ascending order, glacial deposits are overlain by 107:, meta-andesite, meta-arkose, micaceous quartzites and 72:
and northern Ghana predate the 2.2 billion year old
859: 834: 553: 68:The oldest rocks in Niger, along the border with 271:Hydrogeology in Niger is poorly researched. The 162:mountain building event 600 million years ago. 142:Neoproterozoic (1 billion-539 million years ago) 341:. One hundred thirty five kilometers south of 64:Stratigraphy, Tectonics & Geologic History 531: 304:are found in sediments in the Agadez region. 8: 239:Mesozoic-Cenozoic (251-66 million years ago) 153:along the border with Burkina Faso contains 174:as multi-cellular life became commonplace, 538: 524: 516: 506: 451: 436: 414: 227:A coal bearing layer, likely tied to a 95:. The Liptako region, in the west has 166:Paleozoic (539-251 million years ago) 7: 207:Ordovician-Silurian extinction event 130:The Air Massif began to form in the 14: 345:, is the Tapoa phosphate deposit 846:Sahrawi Arab Democratic Republic 616:Democratic Republic of the Congo 243:A marine transgression in the 1: 138:of the Aouzeueur formation. 961: 424:Geological Atlas of Africa 220:sandstones and shales and 486:10.1007/s10040-009-0447-x 422:SchlĂĽter, Thomas (2008). 353:sedimentary rocks of the 91:grade in the sequence of 601:Central African Republic 426:. Springer. p. 190. 279:Natural resource geology 761:SĂŁo TomĂ© and PrĂ­ncipe 621:Republic of the Congo 44:began to form in the 466:Hydrogeology Journal 229:marine transgression 224:deltaic sandstones. 176:anorogenic magmatism 836:States with limited 509:, pp. 192–193. 478:2009HydJ...17.1805B 222:Early Carboniferous 160:Pan-African orogeny 54:Pan-African orogeny 547:Geology of Africa 247:, during the late 93:metamorphic facies 932: 931: 863:other territories 636:Equatorial Guinea 259:, throughout the 191:Hercynian orogeny 87:metamorphosed to 952: 945:Geology of Niger 924: 923:(United Kingdom) 919:Tristan da Cunha 915:Ascension Island 907: 894: 885: 861:Dependencies and 554:Sovereign states 540: 533: 526: 517: 510: 504: 498: 497: 472:(7): 1805–1815. 461: 455: 449: 440: 434: 428: 427: 419: 403:artisanal mining 253:Early Cretaceous 195:Hoggar Mountains 42:Iullemeden Basin 18:geology of Niger 960: 959: 955: 954: 953: 951: 950: 949: 935: 934: 933: 928: 927: 922: 905: 892: 883: 864: 862: 855: 839: 837: 830: 549: 544: 514: 513: 505: 501: 463: 462: 458: 450: 443: 435: 431: 421: 420: 416: 411: 386:chloritoschists 281: 269: 241: 181:Throughout the 168: 144: 66: 12: 11: 5: 958: 956: 948: 947: 937: 936: 930: 929: 926: 925: 908: 895: 886: 872:Canary Islands 868: 867: 865: 860: 857: 856: 854: 853: 848: 842: 840: 835: 832: 831: 829: 828: 823: 818: 813: 808: 803: 798: 793: 788: 783: 778: 773: 768: 763: 758: 753: 748: 743: 738: 733: 728: 723: 718: 713: 708: 703: 698: 693: 688: 683: 678: 673: 668: 663: 658: 653: 648: 643: 638: 633: 628: 623: 618: 613: 608: 603: 598: 593: 588: 583: 578: 573: 568: 563: 557: 555: 551: 550: 545: 543: 542: 535: 528: 520: 512: 511: 499: 456: 454:, p. 192. 441: 439:, p. 190. 429: 413: 412: 410: 407: 347:Neoproterozoic 280: 277: 268: 265: 240: 237: 211:Early Silurian 167: 164: 155:Neoproterozoic 143: 140: 65: 62: 46:Neoproterozoic 13: 10: 9: 6: 4: 3: 2: 957: 946: 943: 942: 940: 920: 916: 912: 909: 903: 899: 896: 890: 887: 881: 877: 873: 870: 869: 866: 858: 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266: 264: 262: 258: 254: 250: 246: 238: 236: 234: 230: 225: 223: 219: 215: 212: 208: 204: 200: 196: 192: 187: 184: 179: 177: 173: 165: 163: 161: 156: 152: 149: 141: 139: 137: 133: 128: 126: 122: 118: 114: 110: 106: 102: 98: 94: 90: 86: 82: 78: 75: 71: 63: 61: 59: 55: 51: 47: 43: 39: 35: 31: 27: 23: 19: 911:Saint Helena 882:   786:South Africa 776:Sierra Leone 745: 581:Burkina Faso 502: 469: 465: 459: 432: 423: 417: 395: 371: 331:arsenopyrite 327:chalcopyrite 306: 294:chalcopyrite 282: 270: 267:Hydrogeology 242: 226: 203:unconformity 193:to form the 188: 180: 169: 145: 129: 121:conglomerate 70:Burkina Faso 67: 28:eons of the 17: 15: 838:recognition 791:South Sudan 681:Ivory Coast 405:continues. 382:anorthosite 355:Volta Group 298:chrysocolla 170:During the 148:Volta Basin 132:Precambrian 97:amphibolite 89:amphibolite 74:Proterozoic 34:Volta Basin 30:Precambrian 26:Proterozoic 893:(Portugal) 851:Somaliland 771:Seychelles 736:Mozambique 721:Mauritania 706:Madagascar 661:The Gambia 596:Cape Verde 409:References 390:Ophiolites 376:lenses in 323:sphalerite 319:Quaternary 245:Cenomanian 214:graptolite 199:Ordovician 38:Air Massif 726:Mauritius 494:129592122 399:Pegmatite 363:Paleocene 339:covellite 290:malachite 261:Paleocene 235:fossils. 183:Paleozoic 136:ophiolite 125:greywacke 117:quartzite 85:migmatite 50:Paleozoic 939:Category 917: / 913: / 906:(France) 900: / 878: / 874: / 826:Zimbabwe 801:Tanzania 651:Ethiopia 646:Eswatini 626:Djibouti 591:Cameroon 576:Botswana 374:chromite 351:Cambrian 315:laterite 257:Cenozoic 249:Mesozoic 233:conodont 218:Devonian 216:shales, 172:Cambrian 151:syncline 101:chlorite 77:Birimian 58:laterite 40:and the 902:RĂ©union 898:Mayotte 889:Madeira 884:(Spain) 880:Melilla 811:Tunisia 781:Somalia 766:Senegal 751:Nigeria 741:Namibia 731:Morocco 696:Liberia 691:Lesotho 641:Eritrea 611:Comoros 586:Burundi 561:Algeria 474:Bibcode 378:gabbros 359:apatite 310:lignite 302:cuprite 22:Archean 921:  904:  891:  821:Zambia 816:Uganda 756:Rwanda 711:Malawi 671:Guinea 566:Angola 492:  367:Eocene 343:Niamey 335:pyrite 286:Agadez 273:Eocene 109:garnet 105:schist 81:gneiss 32:. The 876:Ceuta 796:Sudan 746:Niger 701:Libya 686:Kenya 666:Ghana 656:Gabon 631:Egypt 571:Benin 490:S2CID 806:Togo 716:Mali 606:Chad 384:and 365:and 349:and 300:and 292:and 146:The 123:and 113:tuff 83:and 48:and 24:and 16:The 482:doi 361:in 337:or 941:: 488:. 480:. 470:17 468:. 444:^ 388:. 380:, 333:, 329:, 325:, 119:, 115:, 99:, 36:, 539:e 532:t 525:v 496:. 484:: 476:: 103:-

Index

Archean
Proterozoic
Precambrian
Volta Basin
Air Massif
Iullemeden Basin
Neoproterozoic
Paleozoic
Pan-African orogeny
laterite
Burkina Faso
Proterozoic
Birimian
gneiss
migmatite
amphibolite
metamorphic facies
amphibolite
chlorite
schist
garnet
tuff
quartzite
conglomerate
greywacke
Precambrian
ophiolite
Volta Basin
syncline
Neoproterozoic

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