دورية أكاديمية

Single-shot laser ablation split stream (SS-LASS) petrochronology deciphers multiple, short-duration metamorphic events.

التفاصيل البيبلوغرافية
العنوان: Single-shot laser ablation split stream (SS-LASS) petrochronology deciphers multiple, short-duration metamorphic events.
المؤلفون: Viete, Daniel R.1,2 daniel.viete@gmail.com, Kylander-Clark, Andrew R.C.2, Hacker, Bradley R.2
المصدر: Chemical Geology. Nov2015, Vol. 415, p70-86. 17p.
مصطلحات موضوعية: *METAMORPHISM (Geology), *LASER ablation, *GEOLOGICAL time scales, *URANIUM-lead dating, *ZIRCON
مستخلص: Single-shot laser ablation split stream (SS-LASS) petrochronology offers spatial resolution of < 1 μm per (surface) analysis. This enables the technique to interrogate metamorphic zircon overgrowths that are very thin, or that preserve a composite age structure. To demonstrate the advantages of SS-LASS, the technique was applied to metamorphic zircon overgrowths in five rocks from the Cordillera de la Costa, Venezuela. In these rocks, SS-LASS was able to decipher discrete, short-duration (< 10 6 yr) zircon growth events at c. 33.0, c. 28.3, c. 23.0 and c. 18.2 Ma. Comparison with existing geo-/thermochronology suggests that the SS-LASS dates represent (hydro)thermal events that mark distinct episodes of tectonism affecting the northern margin of South America. With an external error of 5% incorporated into isotope ratios (as required to achieve satisfactory analytical precision), SS-LASS dates for reference materials were accurate to within 1.5% of published values. The SS-LASS technique is thus, in favorable cases, capable of providing < 10 6 yr resolution for Cenozoic rocks. Methods in ‘geospeedometry’—which employ forward models to reproduce observed diffusion length scales—have obtained anomalously short time scales of 10 4 –10 6 yr for metamorphism. The high spatial and temporal resolution of SS-LASS offers tremendous promise for investigating the veracity of these claims. [ABSTRACT FROM AUTHOR]
قاعدة البيانات: Academic Search Index
الوصف
تدمد:00092541
DOI:10.1016/j.chemgeo.2015.09.013