1 / 51

Application of the fission track method in Geology

Part - II. Application of the fission track method in Geology. 3 key questions. What geologic questions can be answered? What sampling strategy is required? How can we interpret our fission track data?. Part 2 - The application.

trevor
Télécharger la présentation

Application of the fission track method in Geology

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Part - II Application of the fission track method in Geology

  2. 3 key questions What geologic questions can be answered? What sampling strategy is required? How can we interpret our fission track data? Part 2 - The application

  3. What are the processes that we can "date" with fission track data? Very fast processes with rock cooling:volcanic eruptions, intrusions with fast cooling, hydrothermal event, shear heating along fault plane Fast processes with rock cooling:fast exhumation or erosion in an active orogen, fast movements along faults (e.g. tectonic unroofing) Moderately fast processes with rock cooling:moderate exhumation or erosion, moderately cooling in and around intrusive body, Slow processes with rock cooling:slow erosion or exhumation in a decaying orogen Part 2 - The application

  4. Real "dating" with the FT method Only with fast to very fast cooling, the fission track method is able to "date an event" Potential events: • volcanic eruption • fast cooling intrusion • impact event • hydrothermal event • shear heating along thrust plane Part 2 - The application

  5. Process rate estimation with the FT method With moderate and slow cooling, the fission track method only estimates cooling rates. It does NOT necessarily mean an "event". Possible processes: • erosive denudation • tectonic denudation • topography formation • thermal relaxation Part 2 - The application

  6. Fission track dating of a single event - I Australian tektite Glass drops ejected from German impact crater Part 2 - The application

  7. Fission track dating of a single event - II Bohemian Glass from 1849 with 1% of U can be dated with FT  check of the fission decay constant Part 2 - The application

  8. Comparison between dating methods - I Example from German volcano (Kraml et al., in prep.): apatite FT data Part 2 - The application

  9. Comparison between dating methods - II Example from German volcano (Kraml et al., in prep.): Part 2 - The application

  10. Comparison between dating methods - II Part 2 - The application

  11. FT dating and anthropology Titanite 0.306 ± 0.056 Ma Thermoluminescence 0.292 ± 0.026 Ma 0.312 ± 0.028 Ma U-series dating 0.300 ± 0.040 Ma Titanite 0.462 ± 0.045 Ma (Guo et al. 1991) Part 2 - The application

  12. How do we know that the FT age represents a single event ? Track length distribution:All tracks are long (mean length > 14.5 mm) and the track length distribution is very narrow. Radial plot:All single grain ages plot in a narrow cluster (except for very young ages or grains with low U content). Statistical tests:The calculated central age passes Poissonian c2 tests. Isochrons:The FT age is in agreement with ages from other dating techniques (e.g. U/Pb, Ar/Ar, (U-Th)/He). Absence of regional variation:The FT age is identical within the same material, also if sampled at other localities. Part 2 - The application

  13. Nanga Parbat - I 100 km Part 2 - The application

  14. Fast exhumation processes: example Nanga Parbat - II 25 km Part 2 - The application

  15. Fast exhumation processes: example Nanga Parbat - III Part 2 - The application

  16. Fast exhumation processes: example Nanga Parbat - IV Part 2 - The application

  17. Fast exhumation processes: example Nanga Parbat - V From: Brozovic et al. (1997) apatite FT ages: A: 0-1 Ma B: 1-6 Ma C: 6-15 Ma Part 2 - The application

  18. Fast exhumation processes: example Taiwan - I from Dadson et al. (2003):Exhumation rates (mm yr-1) based on apatite FT ages:red: reset FT ageorange: partially resetblue: not reset Part 2 - The application

  19. Fast exhumation processes: example Taiwan - II from Dadson et al. (2003):Bedrock incision rates (mm yr-1) as derived from age dating of fluvial terraces much larger than exhumation rates ! Part 2 - The application

  20. Chicken or egg? The main question in research today: Who was first, erosion or tectonics ? How can we know ? • regional plate tectonic context • very fast cooling points to tectonics • climatic evidence • accompagnying processes • topography analysis Part 2 - The application

  21. Uplift - Exhumation - Denudation (England & Molnar 1990) Part 2 - The application

  22. The effect of topography Part 2 - The application

  23. Convex and concave T-t paths Assumption: topography evolves in a vertical direction only, no lateral valley shift Part 2 - The application

  24. The effect of fluid flow (from Kohl & Rybach, www.gtr. geophys.ethz.ch/ neatpiora.html) Part 2 - The application

  25. Fault planes and ages Part 2 - The application

  26. Fault movements in the Central Alps Part 2 - The application

  27. Exhumation in a cratonic continent - I (Gleadow et al. 2002) Part 2 - The application

  28. Exhumation in a cratonic continent - II (Gleadow et al. 2002)  2750 apatite FT ages Part 2 - The application

  29. Exhumation in a cratonic continent - III (Gleadow et al. 2002) Part 2 - The application

  30. Exhumation in a cratonic continent - IV (Gleadow et al. 2002) Part 2 - The application

  31. The principles of fission track data modelling Part 2 - The application

  32. The modelling of FT data: age and track length Part 2 - The application

  33. Genetic algorithm and shrinking of T-t-boxes Part 2 - The application

  34. Why are detrital zircons better than apatites? Part 2 - The application

  35. The lag time concept Part 2 - The application

  36. orogenic cycle Part 2 - The application

  37. Uplift - erosion - topography Davis (1899): uplift is short-term process Penck (1953): uplift is „waxing-waning“ Hack (1975): uplift and topography form steady-state Part 2 - The application

  38. Detrital age spectra: static and younging age components steady age component younging age component Part 2 - The application

  39. raw data with error envelope Probability density plots of FT ages statistical fit to density plot fitted age populations (from Garver et al. 1999) Part 2 - The application

  40. Decrease and increase of lag time (from Bernet et al. 2001) Part 2 - The application

  41. Example: European Alps pro-wedge retro-wedge Part 2 - The application

  42. Example for a decrease of lag time (from Bernet et al. 2004) Part 2 - The application

  43. Example for a steady lag time (from Bernet et al. 2004) Part 2 - The application

  44. FT ages along vertical bore hole Part 2 - The application

  45. FT age evolution along vertical bore hole Part 2 - The application

  46. FT age evolution along vertical bore hole Part 2 - The application

  47. FT age evolution along vertical bore hole Part 2 - The application

  48. example I: bore hole @ Hünenberg (from Cederbom et al., in press) Part 2 - The application

  49. example II: Rigi Mountain and bore hole @ Weggis (from Cederbom et al., in press) Part 2 - The application

  50. Exhumed PAZ at Denali, Alaska (Fitzgerald et al. 1995) Part 2 - The application

More Related