Fig. 8From: Thickening-upward cycles in deep-marine and deep-lacustrine turbidite lobes: examples from the Clare Basin and the Ordos Basina Examples of deep-lacustrine turbidite channel-fill deposits of the Yanchang Formation in Yangmahe area, Ordos Basin; b–c Close-up views of turbidite channels, generally irregular, with sharp bed bases and abundant erosional surfaces. Rip-up clasts develop in thick sandstones, and no thickening-upward cycle occurs within turbidite channel-fill depositsBack to article page