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Uranium Resources of Africa
Identified Resources
2014 Red Book
J.R. Blaise Johannesburg November 2014
Identified Resources
Johannesburg November 2014
Resource terminology
Resource estimates are divided into separate categories
reflecting different levels of confidence in the quantities reported.
Reasonably Assured Resources (RAR)
Inferred resources (IR)
Prognosticated resources (PR)
Speculative resources (SR)
The resources are further separated into categories
based on the cost of production.
<USD 40 / kgU
<USD 80 / kgU
<USD 130 / kgU
<USD 260 / kgU
Identified Resources
Johannesburg November 2014
Resource terminology
Uranium resources are broadly classified as either conventional
or unconventional.
Conventional resources are those that have an established
history of production where uranium is a primary product, co-
product or an important by-product (e.g. from the mining of
copper and gold).
Very low-grade resources or those from which uranium is only
recoverable as a minor by-product are considered unconventional
resources.
Identified Resources
Johannesburg November 2014
Resource terminology
Reasonably assured resources (RAR) refers to uranium that
occurs in known mineral deposits of delineated size, grade and
configuration such that the quantities which could be recovered
within the given production cost ranges with currently proven
mining and processing technology, can be specified.
Estimates of tonnage and grade are based on specific sample
data and measurements of the deposits and on knowledge of
deposit characteristics.
Reasonably assured resources have a high assurance of
existence.
RAR are expressed in terms of quantities of uranium recoverable
from mineable ore.
Identified Resources
Johannesburg November 2014
Resource terminology Inferred resources (IR) refers to uranium that is inferred to occur
based on direct geological evidence, in extensions of well-explored
deposits, or in deposits in which geological continuity has been
established but where specific data, including measurements of the
deposits, and knowledge of the deposit’s characteristics, are
considered to be inadequate to classify the resource as RAR.
Estimates of tonnage, grade and cost of further delineation and
recovery are based on such sampling as is available and on
knowledge of the deposit characteristics as determined in the best
known parts of the deposit or in similar deposits.
Less reliance can be placed on the estimates in this category than on
those for RAR.
IR are expressed in terms of quantities of uranium recoverable from
mineable ore.
Identified Resources
Johannesburg November 2014
Resource terminology
Approximate correlation of terms used in major
resources classification systems
Identified Resources
Johannesburg November 2014
Uranium 2014
RAR (tU)
<USD40/kgU <USD80/kgU
<USD130/kgU
<USD260/kgU
World Africa
507 400
0
1 211 600
166 100
3 698 900
865 100
4 587 200
1 001 300
Africa/World (%)
0 13.7 23.4 21.8
RAR are reported by 14 African countries: Algeria, Botswana,
Central African Rep., Dem. Rep. of Congo, Gabon, Malawi, Mali,
Namibia, Niger, Somalia, South Africa, Tanzania, Zambia,
Zimbabwe.
Identified Resources
Johannesburg November 2014
Uranium 2014
RAR (tU)
Distribution of reasonably assured resources (RAR) among
countries with a significant share of resources
Identified Resources
Johannesburg November 2014
Uranium 2014
RAR (tU)
Distribution of resources by production method
Production method <USD 40/kgU <USD 80/kgU <USD 130/kgU <USD 260/kgU
Open-pit mining - 53 171 646 597 698 190
Underground mining - - 35 690 35 690
In situ leaching acid - - - -
In situ leaching alkaline - - - -
Co-product/by-product - 113 024 169 536 228 253
Unspecified - - 13 332 39 232
Total - 166 195 865 155 1 001 365
Identified Resources
Johannesburg November 2014
Uranium 2014
RAR (tU)
Distribution of resources by processing method
Processing method <USD 40/kgU <USD 80/kgU <USD 130/kgU <USD 260/kgU
Conventional from OP - 48 419 383 890 406 484
Conventional from UG - 113 024 205 226 261 738
In situ leaching acid - - - -
In situ leaching alkaline - - - -
In-place leaching* - - - -
Heap leaching** from OP - 4 752 262 707 291 706
Heap leaching** from UG - - - -
Unspecified - - 13 332 41 437
Total - 166 195 865 155 1 001 365
Identified Resources
Johannesburg November 2014
Uranium 2014
RAR (tU)
Distribution of resources by processing method
Deposit type <USD 40/kgU <USD 80/kgU <USD 130/kgU <USD 260/kgU
Proterozoic unconformity - - - 1 500
Sandstone - 53 171 407 963 410 975
Polymetallic iron-oxide breccia complex - - - -
Paleo-quartz-pebble conglomerate(a) - 113 034 169 536 226 048
Granite-related - - - 19 400
Metamorphite - - - -
Intrusive - - 196 979 217 740
Volcanic-related - - - -
Metasomatite - - 7 179 7 179
Surficial deposits - - 51 498 81 523
Carbonate - - - -
Collapse breccia pipe - - - -
Phosphate - - 32 000 32 000
Lignite - coal - - - -
Black shale - - - -
Unspecifed - - - 5 000
Total - 166 205 865 155 1 001 365
Identified Resources
Johannesburg November 2014
Uranium 2014
IR (tU)
<USD40/kgU <USD80/kgU
<USD130/kgU
<USD260/kgU
World Africa
175 500
0
745 100
78 400
2 204 000
472 500
3 048 000
562 800
Africa/World (%)
0 10.5 21.4 18.5
IR are reported by 13 African countries: Botswana, Chad, Dem. Rep. of
Congo, Egypt, Gabon, Malawi, Mali, Namibia, Niger, Somalia, South
Africa, Tanzania, Zambia.
Identified Resources
Johannesburg November 2014
Uranium 2014
IR (tU)
Distribution of Inferred resources (IR) among countries with a
significant share of resources
Identified Resources
Johannesburg November 2014
Uranium 2014
IR (tU)
Production method <USD 40/kgU <USD 80/kgU <USD 130/kgU <USD 260/kgU
Open-pit mining 0 9 082 297 028 327 059
Underground mining 0 0 66 529 84 277
In situ leaching acid 0 0 581 581
In situ leaching alkaline 0 0 0 0
Co-product/by-product 0 69 286 103 929 139 097
Unspecified 0 0 4 526 11 818
Total 0 78 368 472 593 562 832
Distribution of resources by production method
Identified Resources
Johannesburg November 2014
Uranium 2014
IR (tU)
Distribution of resources by processing method
Processing method <USD 40/kgU <USD 80/kgU <USD 130/kgU <USD 260/kgU
Conventional from OP - 9 082 222 646 252 589
Conventional from UG - 73 036 177 958 228 549
In situ leaching acid - - 581 581
In situ leaching alkaline - - - -
In-place leaching* - - - -
Heap leaching** from OP - - 74 382 74 382
Heap leaching** from UG - - - -
Unspecified - - 4 526 14 231
Total - 82 118 480 093 570 332
Identified Resources
Johannesburg November 2014
Uranium 2014
IR (tU)
Distribution of resources by geological type
Deposit type <USD 40/kgU <USD 80/kgU <USD 130/kgU <USD 260/kgU
Proterozoic unconformity - - - -
Sandstone - 9 082 177 307 183 735
Polymetallic iron-oxide breccia complex - - - -
Paleo-quartz-pebble conglomerate - 69 286 103 929 138 572
Granite-related - - - 5 492
Metamorphite - - - -
Intrusive - - 97 944 117 547
Volcanic-related - - - -
Metasomatite - - 2 529 2 529
Surficial deposits - - 43 040 48 565
Carbonate - - - -
Collapse breccia pipe - - - -
Phosphate - - - -
Lignite coal - - 47 844 63 792
Black shale - - - -
Unspecified - - - 2 600
Total - 78 368 472 593 562 832
Identified Resources
Johannesburg November 2014
Uranium 2014
Identified Resources (RAR + IR)
<USD40/kgU <USD80/kgU
<USD130/kgU
<USD260/kgU
World Africa
682 900
0
1 956 700
244 500
5 902 900
1 337 600
7 635 200
1 564 100
Africa/World (%)
0 12.5 22.7 20.5
Identified Resources are reported by 16 African countries
Identified Resources
Johannesburg November 2014
Uranium 2014 Identified Resources (RAR + IR)
Global distribution of identified resources (<USD 130/kgU)
Identified Resources
Johannesburg November 2014
Uranium 2014
Additional identified resources
The Secretariat identified additional identified resources since some
countries do not include resource determinations by junior exploration
companies in national totals until additional information is provided to the
pertinent agencies or until a mining licence application is filed, and others
do not always have sufficient human resources to provide detailed
information and evaluation as requested in the questionnaire.
The following table is a Secretariat estimate based on technical reports of
resources that have been classified either as Joint Ore Reserves
Committee (JORC), NI 43-101 or South African Mineral Resource
Committee (SAMREC) compliant.
Identified Resources
Johannesburg November 2014
Uranium 2014
Additional identified resources
Country Deposit/Project Resources (RAR+IR)
Cameroon Kitongo Lolodorf
11 100 1 000
Egypt Gabal Gutter Abu Zenina
2 000 100
Guinea Firawa 7 500
Mauritania Bin En Nar A 238 Reguibat
800 9 000
19 300
Total Africa 50 800
Total World 119 100
Identified Resources
Johannesburg November 2014
Algeria
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
0 0
0 0
19 500 0
Total 0 0 0 19 500
Reasonably assured resources in Algeria are associated to two
geological categories: upper Proterozoic vein deposits in the western
Hoggar and a deposit linked to the Pre-Cambrian basement and its
Palaeozoic sedimentary unconformity in the central Hoggar.
The first category includes vein deposits linked to the faults crossing
the pan-African batholith in the Timgaouine region, represented by the
Timgaouine, Abankor and Tinef deposits of the south-west Ahaggar.
Identified Resources
Johannesburg November 2014
Botswana
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
0 0
12 800 56 000
12 800 56 000
Total 0 0 68 800 68 800
Identified resources are associated to the Letlhakane deposit.
The uranium mineralisation, hosted predominately in carbonaceous
mudstones and siltstones, occurs in relatively thin (0.5-5 m), laterally
extensive lenses with lower-grade material separating higher-grade ore
horizons.
The nature of the ore combined with shallow, flat-lying and soft strata
lends itself well to open-pit extraction methods.
The current resource estimate (in place) is 118 615 tU at 0.018% U.
Identified Resources
Johannesburg November 2014
Cameroon
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR Ad Resources
NA
NA
NA
12 100
Total NA NA NA 12 100 Identified resources are associated to the Kitongo and Lolodorf
deposits.
The Kitongo deposit was explored from 1971–1981, and drilled from
surface and from two adits. Only a fraction of the potential area was
explored. Trenching and drilling revealed uranium mineralization in a
shear zone cutting what was later identified as an albititized and
desilicified granite (episyenite) and Paleozoic andesites.
The uranium anomalies of the Lolodorf syenite were first discovered in
1979. The syenite occurs in a narrow band along the northwestern
edge of the Archean Ntera Complex. It is 2–5 km wide and about 60 km
long. Grades of up to 0.1% U have been reported.
Identified Resources
Johannesburg November 2014
Central African Republic
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
0 0
32 000 32 000
32 000 32 000
Total 0 0 32 000 32 000
The Bakouma Basin uranium is associated with phosphate lenses
interstratified with the silts and the siliceous horizons of the M'Patou
formation (Eocene period). These lenses constitute the uranium ore
and are grouped in several small deposits: Patricia, Patou, Pama,
Palmyre, Pamela and Pâquerette.
Together they represent the Bakouma uranium deposit which contains
about 32 000 tU in ore with an average grade of 0.26% U at an
average depth of 35–40 m.
Identified Resources
Johannesburg November 2014
Chad
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
0 0
0 0
0 2 400
Total 0 0 0 2 40
The Lere deposit has uranium hosted near vertical shear zones and
secondary foliation in albitised and silicified granite in a mixed terrain
of Precambrian units.
Resources compliant with the South African code for the reporting of
exploration results, mineral resources and minerals reserves
[SAMREC] Code have been evaluated to amount to 3 190 tU (in
place), at an average grade of 200 ppm U.
Identified Resources
Johannesburg November 2014
Dem. Rep. of Congo
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
0 0
0 0
1 400 1 300
Total 0 0 0 2 700
Identified resources are associated to the Swambo, Shinkolobwe and Kasompi
deposits, in the “Copper–Cobalt belt” in the Shaba province.
These deposits are similar, except in size, to the Shinkolobwe deposit (23 000–
28 000 tU have been produced at the Shinkolobwe mine from ore ranging in
grade from 0.38–1.0% U.
Vein deposits in Precambrian metamorphic dolomites, shales, and
quartzites associated with cobalt, nickel and copper.
Identified Resources
Johannesburg November 2014
Egypt
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR Ad. Resources
0 0
0 0
0 0
0 0
2 100
Total 0 0 0 2 100
Uranium resources are associated to the In Gabal Gattar prospect
located in the N part of the Sinaï Desert (Shear zones cutting
Precambrian granites) and to the Abu Zenina prospect located in the
SW part of the Sinaï Peninsula.
Identified Resources
Johannesburg November 2014
Gabon
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
0 0
4 800 0
4 800 1 000
Total 0 0 4 800 4 800
After the closure of mine operations in 1999, remaining
resources are associated to the Bagombe and
Mikouloungou deposits (Sandstone type deposits).
Identified Resources
Johannesburg November 2014
Guinea
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR Ad Resources
NA
NA
NA
7 500
Total NA NA NA 7 500
Uranium resources are associated to the Firawa deposit (uranium
occurrences identified in large fractures and adjacent mylonites related
to Archean and Proterozoic metamorphic complexes).
Identified Resources
Johannesburg November 2014
Malawi
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
0 0
8 200 2 300
10 400 4 600
Total 0 0 10 500 15 000
Malawi’s total in situ identified resource is 19 910 tU. This is based on
resources at three locations:
-Paladin’s Kayelekera mine (13 090 tU), in sandstone
-Resource Star’s Livingstonia deposit (2 270 tU @ 0.0229% U), in
sandstone,
-Globe Metal’s Kanyika niobium deposit (4 550 tU) where uranium will
be produced as a by-product (0.28% Nb2O5, 0.0135% Ta2O5 and
0.0666% U).
Pegmatite quartz vein, hosted in Proterozoic felsic schists
Identified Resources
Johannesburg November 2014
Mali
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
0 0
8 500 4 500
8 500 4 500
Total 0 0 13 000 13 000
The mineralisation at the Falea Project occurs within the Neoproterozic
to Carboniferous sedimentary sequence of the Taoudeni Basin. The
uranium mineralisation is believed to be a sandstone-type – roll-front –
deposit.
Total identified resources amount to 17 412 tU which includes 11 377
tU RAR and 6 035 tU inferred (NI 43-101compliant resource estimate).
Identified Resources
Johannesburg November 2014
Mauritania
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR Ad Resources
NA
NA
NA
29 100
Total NA NA NA 29 100
At Reguibat calcrete type uranium occurrences have been identified
related to Precambrian complexes.
A 238 and Bin En Nar deposits are related to shear zones in the
Reguibat shield.
Identified Resources
Johannesburg November 2014
Namibia
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
0 0
248 200 134 600
296 500 159 100
Total 0 0 382 800 455 600
Identified recoverable conventional resources in Namibia amounted to
455 591 tU in 2013. Deposits in Namibia are typically large and low
grade. In 2013, about 84% of the recoverable identified uranium
resources are classified in the <USD 130/kgU(USD 50/lb U3O8) cost
category with no resources reported in the <USD 80kg/U category.
Intrusive type deposits: Rössing, Husab, Valencia, Namibplaass,
Etango
Calcrete type deposits: Langer Heinrich, Trekkopje, Omahola.
Surficial type deposits: Marenica, Tubas.
Identified Resources
Johannesburg November 2014
Niger
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
14 800 600
325 000 79 900
325 000 79 900
Total 0 15 400 404 900 404 900
The total recoverable identified conventional resources for Niger, as of
the end of 2013, amount to 404 914 tU, a decline of 40 585 tU
compared to estimates in 2011, owing to the change in processing
method and recoveries for the Imouraren deposit.
Imouraren was originally planned (2011) to be mined by open-pit by
conventional processes with a 95% recovery, but in 2013 the plan was
updated – mining will be open-pit with heap leaching process and
recoveries of approximately 75%. Resources: 279 085 tU @ 0.07 %U
All uranium deposits in Niger are sandstone-hosted, with average
grades of 0.07 to 0.40% U.
Identified Resources
Johannesburg November 2014
Somalia
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
0 0
0 0
7 600 2 600
Total 0 0 0 10 200
At Alio Ghelle, the mineralization is related to an albititic process
coming from sodium-metasomatism of fractured zones of the
basement.
The proved reserves of Alio Ghelle ore bodies amount to 1 950 tU
with an average content of 0.076% U and the semi-proved
reserves to 3 400 tU.
In the Mudug Province, the mineralization is found in friable rocks,
mainly in clays and fluvial sandstone of a Miocene suite overlain
by a massive gypsum crust.
The ore amount to 5 500 tU at an average grade of 0.068% U.
Identified Resources
Johannesburg November 2014
South Africa
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
113 000 69 300
175 300 162 800
233 700 217 100
Total 0 182 300 338 100 450 800
The majority of past and present production was as a by-product of gold,
or to a minor extent, copper (Palabora). Only two primary uranium
producers have existed in South Africa (the Beisa mine in the Free State
and the Dominion Reefs Uranium Mine near Klerksdorp).
The Witwatersrand Basin contains about 81% of total identified uranium
resources in South Africa, in both the underground, hosted by quartz-
pebble conglomerates, and their resulting tailings storage facilities.
Approximately 49% of the total identified resources are in the
Witwatersrand underground operations, 32% in their associated
tailings facilities, 14% in the Springbok Flats Basin where uranium is
hosted by both coal and shale and about 5% in the sandstone-hosted
deposits of the Karoo Basin.
Identified Resources
Johannesburg November 2014
Tanzania
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
38 300 8 500
40 400 17 700
40 400 17 700
Total 0 46 800 58 100 58 100
Total identified in situ uranium resources from four areas in Tanzania
amount to 72 738 tU.
Over 80% of the total relates to the Nyota sandstone deposit at Mkuju
River. It contains 47 927 tU of measured and indicated and 10 578 tU
of inferred resources all in the <USD 80/kgU cost category.
The Manyoni playa lake calcrete deposits make up 11 146 tU of
identified resources of which 9 477 tU is inferred.
The remaining resources include two sandstone-type deposits:
the Likuju North of 2 312 tU and the Mtonya deposit which comprises
775 tU and is potentially in situ recovery amenable.
Identified Resources
Johannesburg November 2014
Zambia
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
0 0
9 900 14 700
9 900 14 700
Total 0 0 25 600 25 600
Only three properties in Zambia have reached the stage of development
where NI 43-101 or JORC compliant resources have been published.
The Mutanga Project (sandstone type deposit) has a total of 75.4 Mt of
measured, indicated and inferred ore at a grade of 0.025% U containing
18 923 tU including inferred resources at Dibwe East.
The Chirundu Project, adjacent to Mutanga, has total measured,
indicated and inferred resources of 18.7 Mt at a grade of 0.023%
containing 4 270 tU.
The third is the Lumwana copper mine, where resources are hosted by
mica-quartz-kyanite schists of the Katangan Supergroup. Measured,
indicated and inferred resources of 7 492 tU are contained within 11.2
Mt of ore.
Identified Resources
Johannesburg November 2014
Zimbabwe
<USD40/kgU
<USD80/kgU <USD130/kgU <USD260/kgU
RAR IR
0 0
0 0
0 0
1 400 0
Total 0 0 0 1 400
The resources are associated with the Kanyemba deposit located in
the northern part of the country, near the boundary with
Mozambique.
The deposit consists of several lens shaped bodies, 0.20–3 m thick,
20–100 m wide and up to 600 m long. It is a tabular deposit
occurring in sandstones of the Upper Pebbly Arkose Formation,
Upper Triassic, of the Upper Karoo System.
6 750 t V2O5