کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4694311 1636895 2009 5 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Comments on “Kinematic variations across Eastern Cordillera at 24°S (Central Andes): Tectonic and magmatic implications” by Acocella, et al. [Tectonophysics 434 (2007) 81-92]
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
پیش نمایش صفحه اول مقاله
Comments on “Kinematic variations across Eastern Cordillera at 24°S (Central Andes): Tectonic and magmatic implications” by Acocella, et al. [Tectonophysics 434 (2007) 81-92]
چکیده انگلیسی
The interpretation of Acocella et al. about (i) westward increase of strike-slip motion, (ii) strain partitioning, (iii) symmetry of the Central Andes, as well as (iv) the interpreted cause for the occurrence of magmatic centres behind the arc, from the Late Miocene onward, is largely speculative and contains major flaws. We demonstrate all above, that successive phases of deformation from Middle Eocene to Quaternary in the edge of the Puna-Eastern Cordillera, as well as the occurrence of arc/intraplate signatures in the magmatic centres of the Eastern Cordillera, result in complex geological framework which requires more detailed and intensive work in order to achieve sustainable interpretations.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Tectonophysics - Volume 469, Issues 1–4, 20 April 2009, Pages 150-154
نویسندگان
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