نمایش منو
صفحه اصلی
جستجوی پیشرفته
فهرست کتابخانه ها
انتخاب زبان
فارسی
English
العربی
عنوان
Active flexural-slip faulting:
پدید آورنده
Li, T; Chen, J; Thompson, JA; Burbank, DW; Yang, X
موضوع
رده
کتابخانه
مرکز و کتابخانه مطالعات اسلامی به زبانهای اروپایی
محل استقرار
استان:
قم
ـ شهر:
قم
تماس با کتابخانه :
32910706
-
025
شماره کتابشناسی ملی
شماره
LA4f1893qp
عنوان و نام پديدآور
عنوان اصلي
Active flexural-slip faulting:
نام عام مواد
[Article]
نام نخستين پديدآور
Li, T; Chen, J; Thompson, JA; Burbank, DW; Yang, X
عنوان اصلي به قلم نويسنده ديگر
A study from the pamir-tian shan convergent zone, NW China
یادداشتهای مربوط به خلاصه یا چکیده
متن يادداشت
© 2015. American Geophysical Union. All Rights Reserved. The flexural-slip fault (FSF), a type of secondary fault generated by bed-parallel slip, occurs commonly and plays an important role in accommodating fold growth. Although the kinematics and mechanics of FSFs are well studied, relatively few field observations or geometric models explore its geomorphic expression. In the Pamir-Tian Shan convergent zone, NW China, suites of well-preserved FSF scarps displace fluvial terraces in the Mingyaole and Wulagen folds. Integrating interpretations of Google Earth images, detailed geologic and geomorphic mapping, and differential GPS measurements of terrace surfaces, we summarize geomorphic features that typify these faults and create kinematic models of active flexural-slip faulting. Our study indicates the following: (i) FSF scarps commonly occur near synclinal hinges, irrespective of whether (a) the dip direction of beds on either side of the hinge is unidirectional or in opposite directions, (b) the hinge is migrating or fixed, or (c) the hinge shape is narrow and angular or wide and curved. (ii) Active FSFs are likely to produce higher scarps on steeper beds, whereas lower or no topographic scarps typify gentler beds. (iii) Tilt angles of the terrace surface displaced above FSFs progressively decrease farther away from the hinge, with abrupt changes in slope coinciding with FSF scarps; the changes in tilt angle and scarp height have a predictable geometric relationship. (iv) Active FSFs can accommodate a significant fraction of total slip and play a significant role in folding deformation. (v) Active FSFs may be used to assess seismic hazards associated with active folds and associated blind thrusts.
مجموعه
تاريخ نشر
2015
عنوان
UC Santa Barbara
دسترسی و محل الکترونیکی
نام الکترونيکي
مطالعه متن کتاب
اطلاعات رکورد کتابشناسی
نوع ماده
[Article]
کد کاربرگه
275578
اطلاعات دسترسی رکورد
سطح دسترسي
a
تكميل شده
Y
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