کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
4690016 | 1636114 | 2011 | 18 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
The Latemar: A Middle Triassic polygonal fault-block platform controlled by synsedimentary tectonics
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
فرآیندهای سطح زمین
پیش نمایش صفحه اول مقاله
چکیده انگلیسی
The horse-shoe shape of the platform and its margins, rectilinear for long tracts, are explained by the existence of a network of extensional faults, whose activity lasted for part of the growth of the platform. The Latemar is thus a polygonal, fault-block platform controlled by synsedimentary tectonics. The resulting sedimentary architecture is that of a growth wedge, deposited probably on the uplifted side of a submerged half graben. Continuous reactivation of faults at platform margins locally determined anomalous facies transitions, with well layered platform interior directly in contact with the clinostratified slopes.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Sedimentary Geology - Volume 234, Issues 1â4, 1 March 2011, Pages 1-18
Journal: Sedimentary Geology - Volume 234, Issues 1â4, 1 March 2011, Pages 1-18
نویسندگان
Nereo Preto, Marco Franceschi, Giovanni Gattolin, Matteo Massironi, Alberto Riva, Pierparide Gramigna, Luca Bertoldi, Sergio Nardon,