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Ancient Northwest

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Xenoliths/Magma (Carrying pieces of basement to the surface) Drill Cores Samples ... Mantle Xenolith. A-4. Young. Basement. Old. Basement ... – PowerPoint PPT presentation

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Title: Ancient Northwest


1
Ancient Northwest
Logan Pass, Glacier National Park
  • The Foundation of a Continent
  • and the Belt Supergroup

2
Exposed Rocks of the Precambrian
3
A-3
Location in Lecture Handouts
Cordillera
4
Cordillera
Part of the North American Mobile Belt
Mobile Belt
Compared to Craton
5
Anatomy of a Continent
Craton
Continental Shelf
Mobile Belt
Basement Rock
Exposed ancient basement rock
Sedimentary rock covering basement rock
6
How do we study basement rock?
  • Windows(Basement exposed at the surface)
  • Xenoliths/Magma(Carrying pieces of basement to
    the surface)
  • Drill Cores Samples(Drilling to the basement)
  • Geophysics(Imaging the basement)

7
Basement Rock Windows in NA
A-1
Note Not many in the west
8
How do we study basement rock?
  • Windows(Basement exposed at the surface)
  • Xenoliths/Magma(Carrying pieces of basement to
    the surface)
  • Drill Cores Samples(Drilling to the basement)
  • Geophysics(Imaging the basement)

Mantle Xenolith
9
A-4
Old Basement
Young Basement
10
How can we use magma chemistry to tell old/young
basement rocks?
  • Rubidium-87 (Rb-87) is radioactive and decays to
    form Strontium-87 (Sr-87)
  • Rb-87 is common in felsic rocks (continental
    crust)
  • Young crust - most Rb had not decayed(not much
    Sr-87)
  • Old crust - lots of Rb has decayed into Sr-87
  • When crust melts - these chemicals end up in
    magma and magma carries chemical signal to the
    surface
  • High Sr-87 old basement belowLow Sr-87 young
    basement below

11
The Edge of the Old Basement
A-4
706 Line
gt 0.706 (Old Basement Rock)
lt 0.704 (Young Basement Rock)
Measure Sr-87 relative to Sr-86
Sr87/Sr86 in Plutons
gt 0.706 (high)
lt 0.704 (low)
12
How do we study basement rock?
  • Windows(Basement exposed at the surface)
  • Xenoliths/Magma(Carrying pieces of basement to
    the surface)
  • Drill Cores Samples(Drilling to the basement)
  • Geophysics(Imaging the basement)

13
How do we study basement rock?
  • Windows(Basement exposed at the surface)
  • Xenoliths/Magma(Carrying pieces of basement to
    the surface)
  • Drill Cores Samples(Drilling to the basement)
  • Geophysics(Imaging the basement)

14
Seismic Profile
15
BasementProvinces of North America
A-2
A.K.A. The United Plates of America
GF
Archean Basement (gt2.5 billion years)
Proterozoic Basement (2.5-0.5 billion years)
Mobile Belts
16
Northwest Basement
A-2
Wyoming Provenance 2.8-3.5 Gyrs old Includes
rocks found in Beartooth Mtns and Grand Teton
National Park
GF
Hearne Provenance 2.8-3.5 Gyrs old
Collision Zone Great Falls Tectonic Zone
(GF) 2.8 Gyrs ago
17
Northwest Basement
A-2
Collision Zone Trans-Hudson Belt 1.9-1.8 Gyrs
ago Wyoming/Hearne collide with Superior
Provenance
GF
By 1.8 Gyrs the basement rock of NA was in place
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