کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
---|---|---|---|---|
4734191 | 1357077 | 2006 | 11 صفحه PDF | دانلود رایگان |
عنوان انگلیسی مقاله ISI
Influence of deflection on a fold-to-fault progression: field evidence from near Marietta, South Carolina
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کلمات کلیدی
موضوعات مرتبط
مهندسی و علوم پایه
علوم زمین و سیارات
زمین شناسی
پیش نمایش صفحه اول مقاله
![عکس صفحه اول مقاله: Influence of deflection on a fold-to-fault progression: field evidence from near Marietta, South Carolina Influence of deflection on a fold-to-fault progression: field evidence from near Marietta, South Carolina](/preview/png/4734191.png)
چکیده انگلیسی
The early stages of D3b were formed by deflection of northwest-directed, layer-parallel shortening and active, down-section propagation of folds and thrusts. Following connection with a splay of basal detachment, later D3b stages resulted from up-section movement that produced kink folding and a throughgoing thrust. This up-section movement deformed and modified the geometries of older, down-section structures. Detailed mesoscopic field observations, integrated with a combination of current thrust fault models, are used to interpret the D3b fold-to-fault progression.
ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Structural Geology - Volume 28, Issue 7, July 2006, Pages 1316-1326
Journal: Journal of Structural Geology - Volume 28, Issue 7, July 2006, Pages 1316-1326
نویسندگان
C.W. Clendenin, J.M. Garihan,