کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
9527003 | 1636968 | 2005 | 29 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Alpine polyphase tectono-metamorphic evolution of the South Carpathians: A new overview
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
فرآیندهای سطح زمین
پیش نمایش صفحه اول مقاله
![عکس صفحه اول مقاله: Alpine polyphase tectono-metamorphic evolution of the South Carpathians: A new overview Alpine polyphase tectono-metamorphic evolution of the South Carpathians: A new overview](/preview/png/9527003.png)
چکیده انگلیسی
Early Cretaceous thick-skinned tectonics was replaced by thin-skinned tectonics in Late Cretaceous. Thus, the former Middle Cretaceous “Austrian” nappe stack and its Albian-Lower Senonian cover got incorporated in the intra-Senonian “Laramide/Getic” stacking of the Getic-Supragetic/Severin/Arjana nappes onto the Danubian nappe duplex. The two contraction events are separated by an extensional tectonic phase in the upper plate recorded by the intrusion of the “Banatitic” magmas (84-73 Ma). The overthrusting of the entire South Carpathian Cretaceous nappe stack onto the fold/thrust foredeep units and to the Moesian Platform took place in the Late Miocene (intra-Sarmatian) times and was followed by extensional events and sedimentary basin formation.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Tectonophysics - Volume 410, Issues 1â4, 9 December 2005, Pages 337-365
Journal: Tectonophysics - Volume 410, Issues 1â4, 9 December 2005, Pages 337-365
نویسندگان
Viorica Iancu, Tudor Berza, Antoneta Seghedi, Ion Gheuca, Horst-Peter Hann,