+ All Categories
Home > Documents > Short Course: U-Pb Geochronology and Hf Isotope Geochemistry Applied to Detrital Minerals

Short Course: U-Pb Geochronology and Hf Isotope Geochemistry Applied to Detrital Minerals

Date post: 11-Feb-2016
Category:
Upload: ofira
View: 44 times
Download: 1 times
Share this document with a friend
Description:
Short Course: U-Pb Geochronology and Hf Isotope Geochemistry Applied to Detrital Minerals. George Gehrels Department of Geosciences University of Arizona Tucson, AZ 85721. Jeff Vervoort School of Earth & Environmental Sciences Washington State University Pullman, WA 99164. - PowerPoint PPT Presentation
Popular Tags:
18
Short Course: U-Pb Geochronology and Hf Isotope Geochemistry Applied to Detrital Minerals Funding from NSF (Instrumentation & Facilities) Help from Thermo Instruments, GV Instruments, Nu Plasma Instruments, New Wave Research & Photon Machines George Gehrels Department of Geosciences University of Arizona Tucson, AZ 85721 Jeff Vervoort School of Earth & Environmental Sciences Washington State University Pullman, WA 99164
Transcript
Page 1: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Short Course: U-Pb Geochronology

and Hf Isotope Geochemistry Applied to Detrital Minerals

Funding from NSF (Instrumentation & Facilities)

Help from Thermo Instruments, GV Instruments, Nu Plasma Instruments, New Wave Research & Photon Machines

George GehrelsDepartment of Geosciences

University of ArizonaTucson, AZ 85721

Jeff VervoortSchool of Earth & Environmental Sciences

Washington State UniversityPullman, WA 99164

Page 2: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Outline 1. Basics of U-Th-Pb decay system2. Measurement methods3. Mineral systems & applications4. Complexities for zircon5. Detrital geochronology (plots & analyses) 6. Future opportunities7. Basics of Lu-Hf decay system8. Measurement challenges9. Application to detrital minerals

Page 3: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

U-Th-Pb chronometers:

0.0

0.2

0.4

0.6

0.8

1.0

1.2

0 1 2 3 4Age (Ga)

206*

/238

0

10

20

30

40

50

60

70

80

90

0 1 2 3 4Age (Ga)

207*

/235

0.0

0.1

0.1

0.2

0.2

0.3

0.3

0 1 2 3 4Age (Ga)

208*

/232

0.0

5.0

10.0

15.0

20.0

25.0

0 1 2 3 4Age (Ga)

206*

/207

*

Any mineral with U and/or Th is a potential chronometer!

Best if little Pb included during crystallization

Need to know conditions of retention of Pb to understand age

206Pb/238U 207Pb/235U 206Pb/207Pb 208Pb/232Th

Page 4: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Geochronometers &Thermochronometers

Geochronometer:Mineral grows below blocking temp Age records crystallization

Thermochronometer:Mineral grows above blocking temp Age records cooling

Page 5: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Common: Less common:Garnet MonaziteRutile MagnetiteTourmaline IlmeniteZircon Chromite

OlivineDiamond

Heavy minerals in sand:

Page 6: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Why zircon is king….

ZrSiO4

High U concentration (100-1000 ppm) Moderate Th concentration (10-100 ppm) Zr, U, Th tightly held [similar in size (0.8-1.0 Å)

and charge (+4)] Low common Pb during crystallization (ppt) Grows @ 600-1100 ºC, retains Pb to >800°C Common in felsic & intermediate igneous rocks Chemically and mechanically resistant.

Page 7: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Zircon (ZrSiO4)• Birthstone for December• Protects travelers from harm• Increases one's appetite• Induces deep sleep (no nightmares)• Helps one be at peace• Loss of luster warns of danger• Provides wisdom, honor, and riches• Heals mental disturbances• Feeding the zircon gorilla = team building activity!

Brown: heals headachesColorless: clears the auraYellow: attracts loveRed: heals injuries, soothes painsGreen: draws wealthLight blue: stabilizes mind & emotionsPink: assists in astral travel at nightViolet: money magnet

Zircon should be placed in dry sea salt once a month for discharge and recharge…

Page 8: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Zircon: Provenance of modern sediment

Page 9: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Zircon: Provenance of ancient sediment…

Page 10: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Zircon: Provenance of artifacts…

Mano Temper sands

Page 11: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Zircon: Age of Sediment Accumulation

Detrital grains =

Maximum depositional age

Dating volcanic layers

Page 12: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Zircon: Growth history & Thermal history

“Multi-Dating”

Page 13: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Rutile (TiO2)... Low-mod U content (~10-100 ppm) Moderate common Pb (<10% of total Pb),

206/204 < 1,000 Blocking temp = ~380–450 °C Resists mechanical and chemical weathering

Strength with love

Ease transitions Calm, reason,

order Stabilizes

relationships Off-planet

connector

Page 14: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Low-mod U content (~10-100 ppm) Moderate common Pb (<10% of total Pb) Blocking temp = 400-500 °C Multi-dating

Apatite Ca5(PO4)3

Appetite suppression

Discern truth within

Enhances creativity

Unconditional acceptance

Vibrates to the number 9

Page 15: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Very high Th content (1000-10,000 ppm) Moderate U content (100-1000 ppm) Very low common Pb (ppt) Blocking temperature = ~680–750 °C Can tie age to metamorphic reactions mod- to high-grade metamorphism Multi-dating?

Monazite CeLaThPO4

??

Page 16: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Monazite CeLaThPO4

From: Hietpas et al. (2010)

zircon

monazite

Page 17: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Occurs as inclusions in other minerals (e.g., garnet) many potential applications!

Monazite CeLaThPO4

From: http://webhost.bridgew.edu/mkrol/Research-2.html

Page 18: Short Course: U-Pb Geochronology  and Hf Isotope Geochemistry  Applied to Detrital Minerals

Xenotime YPO4

From: McNaughton et al. (1999)

Moderate U & Th contents (~100 ppm) Moderate to low common Pb (ppt) Blocking temperature = 600-700 °C (?) Peraluminous igneous rocks Diagenetic overgrowths on zircon

depositional ages??


Recommended