Short Course: U-Pb Geochronology and Hf Isotope Geochemistry

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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 Funding from NSF (Instrumentation & Facilities) Help from Thermo Instruments, GV Instruments, Nu Plasma Instruments, New Wave Research & Photon Machines

Outline Basics of U-Th-Pb decay system Measurement methods Mineral systems & applications Complexities for zircon Detrital geochronology (plots & analyses) Future opportunities Basics of Lu-Hf decay system Measurement challenges Application to detrital minerals

U-Th-Pb chronometers: 206Pb/238U 207Pb/235U 206Pb/207Pb 208Pb/232Th 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

Geochronometers & Thermochronometers Mineral grows above blocking temp  Age records cooling Geochronometer: Mineral grows below blocking temp  Age records crystallization

Heavy minerals in sand: Common: Less common: Garnet Monazite Rutile Magnetite Tourmaline Ilmenite Zircon Chromite Olivine Diamond

Why zircon is king…. 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. Remember the leads (204Pb-208Pb) are not going to fractionate from one another in nature very easily. ZrSiO4

Zircon (ZrSiO4) Brown: heals headaches Colorless: clears the aura Yellow: attracts love Red: heals injuries, soothes pains Green: draws wealth Light blue: stabilizes mind & emotions Pink: assists in astral travel at night Violet: money magnet 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! Zircon should be placed in dry sea salt once a month for discharge and recharge…

Zircon: Provenance of modern sediment

Zircon: Provenance of ancient sediment…

Zircon: Provenance of artifacts… Temper sands Mano

Zircon: Age of Sediment Accumulation Detrital grains = Maximum depositional age Dating volcanic layers

Zircon: Growth history & Thermal history “Multi-Dating”

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

Apatite Ca5(PO4)3 Low-mod U content (~10-100 ppm) Moderate common Pb (<10% of total Pb) Blocking temp = 400-500 °C Multi-dating Appetite suppression Discern truth within Enhances creativity Unconditional acceptance Vibrates to the number 9

Monazite CeLaThPO4 ? ? 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 zircon monazite From: Hietpas et al. (2010)

Monazite CeLaThPO4 Occurs as inclusions in other minerals (e.g., garnet)  many potential applications! From: http://webhost.bridgew.edu/mkrol/Research-2.html

Xenotime YPO4 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?? From: McNaughton et al. (1999)