کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
9528387 | 1636671 | 2018 | 63 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
40Ar/39Ar muscovite dating of thrust activity: a case study from the Axial Zone of the Pyrenees
دانلود مقاله + سفارش ترجمه
دانلود مقاله ISI انگلیسی
رایگان برای ایرانیان
کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
فرآیندهای سطح زمین
پیش نمایش صفحه اول مقاله
چکیده انگلیسی
Petrographic observations confirm that pressure solution and recrystallization/dissolution processes in presence of fluids are the main mechanisms that controlled the chemical/textural changes in the fault core zone. Three groups of muscovite are identified in the fault zone i.e. detrital, diagenetic and newly-formed muscovites. The detrital and diagenetic muscovites are mainly present in the damage zone, while the newly-formed muscovite is abundant in the core zone and is synkinematic to the fault activity. The fractions 50-16â¯Î¼m, 16-2â¯Î¼m, 2-0.5â¯Î¼m, <0.5â¯Î¼m and the bulk of two samples from the core and damage zones were encapsulated and dated using the 40Ar/39Ar technique. All size-fractions of the core zone sample have younger ages compared to ones from the damage zone and the ages decrease with grain-size reduction. This indicates the strong effect of deformation in the core zone that enhanced the recrystallization of younger muscovite. The finest fraction (<0.5â¯Î¼m) of the core zone sample has a plateau-like spectrum with a total gas age of 36.9â¯Â±â¯0.2â¯Ma. This age is interpreted as the oldest age possible for the activity of the PPVT during the late Eocene (Priabonian) that coincides with the activity of the GT.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Tectonophysics - Volume 745, 16 October 2018, Pages 412-429
Journal: Tectonophysics - Volume 745, 16 October 2018, Pages 412-429
نویسندگان
Ahmed Abd Elmola, Martine Buatier, Patrick Monié, Pierre Labaume, Pierre Trap, Delphine Charpentier,