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Donald G. York Pushpa Khare Daniel Vanden Berk Varsha P. Kulkarni Arlin P. S. Crotts James T. Lauroesch Gordon T. Richards Donald P. Schneider Daniel E. Welty Yusra Alsayyad Abhishek Kumar Britt Lundgren Natela Shanidze Tristan Smith Johnny Vanlandingham Britt Baugher Patrick B. Hall Edward B. Jenkins Brice Menard Sandhya Rao Jason Tumlinson David Turnshek Ching-Wa Yip Jon Brinkmann 《Monthly notices of the Royal Astronomical Society》2006,367(3):945-978
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Wilfried Bauer Ivan Callegari Naila Al Balushi Ghaliya Al Busaidi Maryam Al Barumi Yusra Al Shoukri 《Arabian Journal of Geosciences》2018,11(5):94
The Saih Hatat region, in northeastern Oman, is characterized by a large tectonic window, tectonically overlain during the upper Cretaceous by nappes composed of sedimentary rocks from the Mesozoic Hawasina ocean and the Samail ophiolite. In this window, the autochthonous sedimentary cover of the eastern Arabian Platform from the Late Neoproterozoic to the Cenomanian is well exposed. The oldest of these strata, the Hatat schists, were deformed into a NE-facing fold nappe during the upper Cretaceous. Within the overturned and thrusted lower limb of that fold nappe, we identified three small windows exposing stratigraphically younger Hiyam carbonates and Ordovician sandstone. The structural inventory of the windows and the surrounding area indicates three major tectonic phases. The first deformation led to NNE-SSW trending fold structures which probably formed simultaneously with the major fold nappe of the Hatat schists, followed by the extreme attenuation and thrusting of the lower limb of the fold nappe. The second phase was a gentle folding of the thrust with N-S oriented fold axes and third deformation phase that formed WNW-ESE oriented open folds. The windows are situated in the intersection of anticline axes of these two superposed fold generations and represent a mini basin-and-dome structure with an extension of just 1 km?×?1 km. 相似文献
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