《Table 2 Mammal localities compiled from literature(see Fig.3 for stratigraphic location within the

《Table 2 Mammal localities compiled from literature(see Fig.3 for stratigraphic location within the   提示：宽带有限、当前游客访问压缩模式
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《"Alluvial sedimentation and tectonostratigraphic evolution in a narrow extensional zigzag basin margin (northern Teruel Basin, Spain)"》


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The overall structure of the Neogene units is a strongly asymmetric syncline.Its western limb represents the gentle rollover monocline asociated to the El Pobo Fault Zone，dipping eastward usually in the range of 2–3°（locally up to 12°）.The eastern，shorter limb represents the accommodation bend at the active margin，with usual dips of about 20°W.Stronger deformation is usually recognized in the lower beds cropping out near the active margin，in the form of either pure brittle offset or drag folds（see below）.Deformation usually attenuates upward，indicating that extensional tectonics was coeval with deposition of Pliocene beds.

图表编号XD002006700    严禁用于非法目的
绘制时间2019.10.01
作者Lope Ezquerro、Aránzazu Luzón、José L.Simón、Carlos L.Liesa
绘制单位Departamento de Ciencias de la Tierra, Facultad de Ciencias, Geotransfer Research Group and Instituto de Investigación en Ciencias Ambientales (IUCA), Universidad de Zaragoza、Departamento de Ciencias de la Tierra, Facultad de Ciencias, Geotransfer Researc
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