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Introduction
 Yukon(The great River) Territory is one of the three smallest
territories in Canada, Locates in north west of Canada , and it’s
Capital city is White Horse .
 Boarders :
• East :Northwest Territories
• West :Alaska
• North: Arctic ocean
• South : British Columbia
 The industry is mining and account’s for 30% of the economy
 The Yukon contains many undeveloped mines of zinc , lead , silver,
copper and iron.
 Sedimentary rocks are the main type of the Yukon territory
Territory map of Yukon
Source : http://geology.com/canada/yukon-territory.shtml
 Over the last 190 million years , the area was affected by
folding , faulting , metamorphism and uplifting which ended
by stratigraphy of sedimentary units above a stable geological
basement.
 The Yukon is classified into five mineral areas :
• Peel (river) class 1 notification area
• Ross river class1 notification area (105O03)
• South western Yukon class 1 notification area
• Watson lake class1 notification area
• Southern Yukon class 1 notification
area(http://mapservices.gov.yk.ca/Mining/WebMap.aspx)
 (Class 1 means class 1 exploration program)
In this presentation , I will present different maps layers of map
sheet 105O03 which show the deposits in the area, the geological
events ,rock units and also a brief sample analysing for
Ag(Silver), Pb (Lead) and Zn(Zinc) elements to prove the presence
of SEDEX (Sedimentary Exhalative Deposits) .
Yukon Classified Mineral Area
Source : http://mapservices.gov.yk.ca/Mining/WebMap.aspx
The Google Erath map shows the young belt of Cordillera province
which formed billion years ago .Map sheet 105O03 location is :
Lat.: 63.1347 Long.: -131.2661 (Earth Google)
Basin : Selwyn Basin : undeveloped districts and contains massive sulphides
The mountain belt series is divided into five belts :
• Insular belt : Volcanic and sedimentary rock type
(C . Hart)
• Intermontane belt : Sedimentary rock type.
(C.Hart)
• Omineca belt : Metamorphosed sedimentary rock
and granite. ( C. Hart)
• Foreland belt :Entirely sedimentary. (C. Hart)
• Coast belt : Granitic rock type. (C. Hart)
The area of Map sheet 105O03 is : 689,319,057 m²
Source :Yukon Energy ,Mines and Resources Land viewer.
 Town Map : The closest town to the map sheet 105O03 is Faro
Town .The Faro town has the largest lead and zinc mine in the
world and producer of silver . It’s area is 203’000 squared
meter.
Source:http://mapservices.gov.yk.ca/YGS/WebMap.aspx
 Access : The nearest road to the area is Canol Road .Macmillan
Pass airport is too close to the area from the east and Dall
Mountain from the north west.
Source : Earth Google
Regional Geology
Source:http//mapservices.gov.yk.ca/YGS/WebMap.aspx
Undefined
The area has two types of Faults :
1) Normal/ reverse faults in the lower part.
2) Thrust/ upright faults in the upper part.
Tectonic activity result in faults is very
important for SEDEX deposits formation.
Rock Units :
Source: http://mapservices.gov.yk.ca/
History of Existing Claims : Undeveloped area
Source: http://mapservices.gov.yk.ca/
Mineral Occurrence :
Au :no hand sample
Barite ,Zn ,Ni ,Pb ,Mo , Cu
Barite , Cd, Ag ,Ni , Cu
Source: http://mapservices.gov.yk.ca/
Sample locations Map
Source: http://mapservices.gov.yk.ca/
 The drainage pattern in the area is dendritic (common
in river ,streams and lakes)Majority of the samples were
collected from the river and the distributary.
 In the area , there are deposits of Silver ,Lead and Zinc .
 The Selwyn basin main types of deposits are is the
SEDEX deposits.
 The tonnage of deposits in Selwyn basin over 9’283’700
tones are as follows:
• Ag 69.4 g/t
• Pb 7.5%
• Zn 6.2%
• Cu 1.81% over 8’510’000 tones
(http://www.geology.gov.yk.ca/pdf/SelwynBasin.pdf)
Elements Tonnage
 By analyzing the data for the concentrations of
metals in map sheet 105O03 ,Silver , Lead ,Zinc
and Copper, have the highest concentration
and no concentration for Gold was detected .
 The deposit type could be VMS or SEDEX.
The tonnage value of Sliver is 69.4 g/t which is
higher than in case if the sediment is VMS
( max 30g/t).
 Also for Lead , the tonnage is 7.5% which higher than
the tonnage in VMS deposits which maximum 2 %.
 The Zinc tonnage is 6.2% which is close to the
maximum values in both VMS and SEDEX.
 The absence of the Gold concentration , can lead to a
result of type of deposit which is SEDEX.
Pathfinder Indicator :
• The area is rich with Shale and Barite and
sedimentary rocks .
• Zn-Pb are shale hosted in an area with faults .
• The Paleozoic deep water environment contains
SEDEX deposits.(Chverier and Turner,2013-2014)
• The SEDEX formation model is Vent distal
• The fluid move along permeable sedimentary rock or
along the fault .
Anomalous Values :
Values that occurred above 20th and 90th percentile
Highest Pb concentration 65 p.p.m. at elevation 1360m
Highest Zn concentration 6050p.p.m.at 1160m
Highest Ag concentration 3.8 p.p.m.1240
Ag Sample locations
Source: http://mapservices.gov.yk.ca/
Ag Concentration
0 0.5 1 1.5 2 2.5 3 3.5 4
1
(B.G 0.20) 0.6 p .p . m
(B.G 0.90 )2 p .p . m
Anomaly 3.8
Ag Concentrations
Pb Sample locations
Source: http://mapservices.gov.yk.ca/
Pb Concentrations
0 10 20 30 40 50 60 70
1
2
3
B.G (0.20)12 p . p.m.
(B.G 0.90)24.4 p. p. m.
Max 65
Pb Concentrations
Zn Samples location
Source: http://mapservices.gov.yk.ca/
Zn Concentrations
0 1000 2000 3000 4000 5000 6000 7000
1
2
3
(B.G 0.90) 207.2p. p. m .
(B.G 0.20)3432 p. p. m .
Max
6050
Zn Concentrations
Geochemistry Map
Source: http://mapservices.gov.yk.ca/
Samples with Highest Concentrations Locations
Source: http://mapservices.gov.yk.ca/
References
http://miningyukon.ca/miningandexplorationopportunities/min
eralexploration/geologicalframework/leadzinc/selwynbasin/
http://geoscan.nrcan.gc.ca/starweb/geoscan/servlet.starweb?p
ath=geoscan/downloade.web&search1=R=291878
http://mapservices.gov.yk.ca/Mining/WebMap.aspx
http://www.geogratis.gc.ca/geogratis/search?lang=en
http://www.aitc.sk.ca/saskschools/canada/facts/yt.html
http://emrlibrary.gov.yk.ca/gsc/open_files/7144/of_7144.pdf
Thank you
Questions ?

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Nts map105 o03 yukon copy

  • 1. <iframe src="//www.slideshare.net/slideshow/embed_code/45735748" width="476" height="400" frameborder="0" marginwidth="0" marginheight="0" scrolling="no"></iframe>
  • 2. Introduction  Yukon(The great River) Territory is one of the three smallest territories in Canada, Locates in north west of Canada , and it’s Capital city is White Horse .  Boarders : • East :Northwest Territories • West :Alaska • North: Arctic ocean • South : British Columbia  The industry is mining and account’s for 30% of the economy  The Yukon contains many undeveloped mines of zinc , lead , silver, copper and iron.  Sedimentary rocks are the main type of the Yukon territory
  • 3. Territory map of Yukon Source : http://geology.com/canada/yukon-territory.shtml
  • 4.  Over the last 190 million years , the area was affected by folding , faulting , metamorphism and uplifting which ended by stratigraphy of sedimentary units above a stable geological basement.  The Yukon is classified into five mineral areas : • Peel (river) class 1 notification area • Ross river class1 notification area (105O03) • South western Yukon class 1 notification area • Watson lake class1 notification area • Southern Yukon class 1 notification area(http://mapservices.gov.yk.ca/Mining/WebMap.aspx)  (Class 1 means class 1 exploration program) In this presentation , I will present different maps layers of map sheet 105O03 which show the deposits in the area, the geological events ,rock units and also a brief sample analysing for Ag(Silver), Pb (Lead) and Zn(Zinc) elements to prove the presence of SEDEX (Sedimentary Exhalative Deposits) .
  • 5. Yukon Classified Mineral Area Source : http://mapservices.gov.yk.ca/Mining/WebMap.aspx
  • 6. The Google Erath map shows the young belt of Cordillera province which formed billion years ago .Map sheet 105O03 location is : Lat.: 63.1347 Long.: -131.2661 (Earth Google) Basin : Selwyn Basin : undeveloped districts and contains massive sulphides
  • 7. The mountain belt series is divided into five belts : • Insular belt : Volcanic and sedimentary rock type (C . Hart) • Intermontane belt : Sedimentary rock type. (C.Hart) • Omineca belt : Metamorphosed sedimentary rock and granite. ( C. Hart) • Foreland belt :Entirely sedimentary. (C. Hart) • Coast belt : Granitic rock type. (C. Hart)
  • 8. The area of Map sheet 105O03 is : 689,319,057 m² Source :Yukon Energy ,Mines and Resources Land viewer.
  • 9.  Town Map : The closest town to the map sheet 105O03 is Faro Town .The Faro town has the largest lead and zinc mine in the world and producer of silver . It’s area is 203’000 squared meter. Source:http://mapservices.gov.yk.ca/YGS/WebMap.aspx
  • 10.  Access : The nearest road to the area is Canol Road .Macmillan Pass airport is too close to the area from the east and Dall Mountain from the north west. Source : Earth Google
  • 12. The area has two types of Faults : 1) Normal/ reverse faults in the lower part. 2) Thrust/ upright faults in the upper part. Tectonic activity result in faults is very important for SEDEX deposits formation.
  • 13. Rock Units : Source: http://mapservices.gov.yk.ca/
  • 14. History of Existing Claims : Undeveloped area Source: http://mapservices.gov.yk.ca/
  • 15. Mineral Occurrence : Au :no hand sample Barite ,Zn ,Ni ,Pb ,Mo , Cu Barite , Cd, Ag ,Ni , Cu Source: http://mapservices.gov.yk.ca/
  • 16. Sample locations Map Source: http://mapservices.gov.yk.ca/
  • 17.  The drainage pattern in the area is dendritic (common in river ,streams and lakes)Majority of the samples were collected from the river and the distributary.  In the area , there are deposits of Silver ,Lead and Zinc .  The Selwyn basin main types of deposits are is the SEDEX deposits.  The tonnage of deposits in Selwyn basin over 9’283’700 tones are as follows: • Ag 69.4 g/t • Pb 7.5% • Zn 6.2% • Cu 1.81% over 8’510’000 tones (http://www.geology.gov.yk.ca/pdf/SelwynBasin.pdf)
  • 18. Elements Tonnage  By analyzing the data for the concentrations of metals in map sheet 105O03 ,Silver , Lead ,Zinc and Copper, have the highest concentration and no concentration for Gold was detected .  The deposit type could be VMS or SEDEX. The tonnage value of Sliver is 69.4 g/t which is higher than in case if the sediment is VMS ( max 30g/t).
  • 19.  Also for Lead , the tonnage is 7.5% which higher than the tonnage in VMS deposits which maximum 2 %.  The Zinc tonnage is 6.2% which is close to the maximum values in both VMS and SEDEX.  The absence of the Gold concentration , can lead to a result of type of deposit which is SEDEX.
  • 20. Pathfinder Indicator : • The area is rich with Shale and Barite and sedimentary rocks . • Zn-Pb are shale hosted in an area with faults . • The Paleozoic deep water environment contains SEDEX deposits.(Chverier and Turner,2013-2014) • The SEDEX formation model is Vent distal • The fluid move along permeable sedimentary rock or along the fault .
  • 21. Anomalous Values : Values that occurred above 20th and 90th percentile Highest Pb concentration 65 p.p.m. at elevation 1360m Highest Zn concentration 6050p.p.m.at 1160m Highest Ag concentration 3.8 p.p.m.1240
  • 22. Ag Sample locations Source: http://mapservices.gov.yk.ca/
  • 23. Ag Concentration 0 0.5 1 1.5 2 2.5 3 3.5 4 1 (B.G 0.20) 0.6 p .p . m (B.G 0.90 )2 p .p . m Anomaly 3.8 Ag Concentrations
  • 24. Pb Sample locations Source: http://mapservices.gov.yk.ca/
  • 25. Pb Concentrations 0 10 20 30 40 50 60 70 1 2 3 B.G (0.20)12 p . p.m. (B.G 0.90)24.4 p. p. m. Max 65 Pb Concentrations
  • 26. Zn Samples location Source: http://mapservices.gov.yk.ca/
  • 27. Zn Concentrations 0 1000 2000 3000 4000 5000 6000 7000 1 2 3 (B.G 0.90) 207.2p. p. m . (B.G 0.20)3432 p. p. m . Max 6050 Zn Concentrations
  • 29. Samples with Highest Concentrations Locations Source: http://mapservices.gov.yk.ca/