کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
10119962 | 1637918 | 2018 | 59 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
The isotope effect for Mg-Fe interdiffusion in olivine and its dependence on crystal orientation, composition and temperature
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
ژئوشیمی و پترولوژی
پیش نمایش صفحه اول مقاله
![عکس صفحه اول مقاله: The isotope effect for Mg-Fe interdiffusion in olivine and its dependence on crystal orientation, composition and temperature The isotope effect for Mg-Fe interdiffusion in olivine and its dependence on crystal orientation, composition and temperature](/preview/png/10119962.png)
چکیده انگلیسی
Isotopic fractionation associated with diffusion in crystals is the most reliable means of understanding the origin of mineral zoning in igneous and metamorphic rocks. We have experimentally determined the relative diffusivities of iron isotopes in olivine as a function of crystallographic orientation, composition, and temperature. For two isotopes i and j of an element, the isotope effect for diffusion is parameterized as Di/Djâ¯=â¯(mj/mi)β, where β is a dimensionless parameter, and D and m stand for diffusivity and mass, respectively. A series of single crystal diffusion couple experiments were conducted at an oxygen fugacity of QFM - 1.5 at temperatures of 1200, 1300, and 1400â¯Â°C. For the Fo83.4-Fo88.8 composition pair, βFe is isotropic and a value of 0.16â¯Â±â¯0.09 can be used to describe diffusion along all major crystallographic axes in olivine. Based on our experiments and previously reported coupled Mg-Fe isotopic data, we also estimate βMgâ¯=â¯0.09â¯Â±â¯0.05 for this range of olivine composition. For the Fo88.8-Fo100 composition pair, βFe becomes anisotropic with βFe [100] = 0.11â¯Â±â¯0.03, βFe [010] = 0.14â¯Â±â¯0.03 (both within error of the value measured for the Fo83.4-Fo88.8 pair), and βFe [001] = 0.03â¯Â±â¯0.03. For Fo# between 83.4 and 100, βFe [100] and βFe [010] are thus independent of composition. The reason why βFe [001] transitions from â¼0.16 to â¼0.03 close to the Mg-endmember is unclear. Over the temperature range studied, a dependence of βFe on temperature was not resolved. General analytical expressions are introduced to calculate isotopic fractionation as a function of distance, time, β, and the concentration contrast between the diffusing media for spherical, cylindrical, and planar geometries.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Geochimica et Cosmochimica Acta - Volume 239, 15 October 2018, Pages 463-480
Journal: Geochimica et Cosmochimica Acta - Volume 239, 15 October 2018, Pages 463-480
نویسندگان
Corliss K. Sio, Mathieu Roskosz, Nicolas Dauphas, Neil R. Bennett, Timothy Mock, Anat Shahar,