Fig. 5From: Paleosols in an outcrop of red beds from the Upper Cretaceous Yaojia Formation, southern Songliao Basin, Jilin Province, NE ChinaPhotographs showing field characteristics of the soil structures in paleosols of the Yaojia Formation. a Pseudo-anticlinal structures in the vertic horizon (Bw) (marked with white rectangles), and prismatic soil structure (marked with a yellow rectangle) in the paleosols; b Gently sloping synclines in pseudo-anticlinal structures in the vertic horizon (Bw); c Small pseudo-anticlines in the vertic horizon (Bw); d Close-up of the small pseudo-anticlines (Fig. 5c) in the vertic horizon (Bw) of the paleosols with angular blocky structure; the fracture surfaces are infilled by calciteBack to article page