کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
6429567 1634766 2014 7 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Experimental evidence regarding the pressure dependence of fission track annealing in apatite
ترجمه فارسی عنوان
شواهد تجربی درباره وابستگی فشار انحلال مسیر شکافت در آپاتیت
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات علوم زمین و سیاره ای (عمومی)
چکیده انگلیسی


- We submitted samples to various pressures, temperatures and time lengths.
- Fission tracks annealing is more effective when combined with pressure.
- When extrapolated to pressures of ⩽150 MPa this dependence becomes negligible.
- Consequently there is no need to worry about current annealing models.

The main purposes of fission track thermochronology are unravelling the thermal histories of sedimentary basins, determining uplift and denudation rates, identifying the structural evolution of orogenic belts, determining sedimentary provenance, and dating volcanic rocks. The effect of temperature on fission tracks is well known and is used to determine the thermal history; however, the effect of pressure on the stability of tracks is still under debate. The present work aims to understand the role of pressure on the annealing kinetics of apatite fission tracks. The samples of Durango apatite used in our experiments were chosen for their international recognition as a calibration standard for geological dating. Neutron irradiation of the samples, after total annealing of their spontaneous tracks, produced induced tracks with homogeneous densities and lengths. The effect of pressure associated with temperature on fission track annealing was verified by experimental procedures using a hydraulic press of 1000 t with a toroidal chamber profile. The experiments consisted of a combination of applying 2 and 4 GPa with 20,150,190,235, and 290°C for 1 and 10 h. The annealing rate was analysed by measuring the lengths of the fission tracks after each experiment using optical microscopy. The results demonstrate that the annealing of apatite fission tracks has a pressure dependence for samples subjected to 2 and 4 GPa. However, when extrapolated to pressures of ⩽150 MPa, compatible with the normal geological context in which apatite fission track methodology is broadly used, this dependence becomes insignificant compared to the temperature effect.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Earth and Planetary Science Letters - Volume 390, 15 March 2014, Pages 1-7
نویسندگان
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