Assessing
Zircon Fission Track Analysis as a paleotemperature tool for sedimentary
basins
Paul F. Green1, Ian R. Duddy1,
Kerry A. Hegarty1, Sara S. Foland2
and Valery Gorbachev3
1 Geotrack International Pty Ltd, Melbourne,
Australia
2 Amoco Corporation, Denver, Co
3 Nedra Enterprise, Jaroslavl, Russia
Why study fission track
annealing kinetics in zircon?
AFTA® provides paleotemperatures and timing information
up to ~130ºC (depending on Cl content)
Because of the greater stability of fission tracks in zircon,
ZFTA can, in principle, provide similar information at higer temperatures
if the annealing kinetics are understood
Laboratory studies of fission track annealing kinetics in zircon
are difficult because of radiation damage in natural zircons
Natural studies are also difficult because of the rarity of geological
situations where present temperatures are high enough to produce observable
effects
Geological Studies
Zircon fission track ages in slowly cooled rocks from
the European Alps suggest a "closure temperature" for
fission track retention in zircon of 240±50ºC by comparison with
other radiometric dating techniques. Other opinions have favoured
a value around 175ºC. |
|
Laboratory Studies
Recent laboratory studies involving measurement of
confined track lengths have given better definition of annealing
kinetics
Extrapolating the results to geological timescales (~106 Ma)
indicates that the zircon "Partial Annealing Zone" spans
the temperature range 170 to 390ºC (±50ºC) |
|
Our Approach
- Investigate geologiacl conditions where present-day temperatures
exceed 200ºC
Kola Peninsula Ultra Deep
Drillhole
- Investigate correlation between zircon fission track age reduction
and other paleo-thermal indicators in rocks which have reached temperatures
in excess of 200ºC
South wales coalfield (UK)
Cleveland Basin (UK)
Arkoma Basin (USA)
Southern Alps (NZ)
Kola Peninsula Ultra
Deep Drillhole
Zircon fission track age pattern shows a decrease
with depth, reflecting a Paleozoic cooling episode (ca. 250 to 300
Ma), also shown by sphene and apatite ages
Correlation of zircon fission track age in the deepest sample
with the timing of this episode as revealed by sphene and apatite
data suggests that this sample, from a present-day temperature
of ~212ºC, has undergone little or no significant age reduction
since cooling to that temperature |
|
Zircon track length data show very little decrease
with depth, suggesting that cooling to a temperature of ~212ºC,
the deepest sample has undergone very little annealing
Combined with the fission track age data, the Kola data suggest
that temperatures well above 212ºC are required to produce significant
annealing effects in zircon |
|
South Wales Coalfield
and Devon
Cloughton-1, Cleveland
Basin (UK)
Devils Backbone Unit
No.1, Arkoma Basin
Southern Alps, New
Zealand
The Southern Alps of
New Zealands South Island provide an excellent example of
an "exhumed Zircon Partial Annealing Zone". Torlesse Metasediments
and their equivalents the Alpine Schists, have been exposed as a
result of uplift and erosion causedby Late Tertiary compression
across the modern Plate Boundary represented by the Alpine Fault.
Comparison of ZFTA data with conventional paleotemperature indicators
such as Vitrinite Reflectance data, provides an insight into the
conditions required to reset zircon fission track ages |
|
Southern Alps (NZ):
Arthurs Pass Transect
Southern Alps (NZ):
Lewis Pass Transect
Conclusions
The results of this study suggest a broad correlation between
fission track annealing in zircon and equivalent VR levels:
No detectable annealing <4% Romax
Some age reduction ~6% Romax
Total annealing ~8% Romax
VR kinetics developed by Burnham and Sweeny (1989) suggest that
a VR of 4% corresponds to a maximum paleotemperature around 260ºC (for
a heating rate of 1C/Ma)
Total annealing in samples from the Southern Alps of New Zealand
correlates with the onset of chlorite-grade greenschist metamorphism,
for which temperatures of around 300ºC or above have been suggested.
Further work is in progress to compare zircon data with other
paleotemperature indicators to refine the details of fission track annealing
kinetics in zircon.
All present indications are that zircon will only prove useful
in regions that have been subjected to greenschist metamorphism.