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Since the Mesozoic, the North China Craton has been located at a triangular junction surrounded by subduction or collision zones. This craton thus marks the frontier of a super‐convergent regime. Within the super‐convergence tectonic domains, however, distinct extensional regimes operated in the Meso‐Cenozoic Bohai Bay Basin located at the eastern part of the North China Craton. In this synthesis,...
Investigations on turbidite sandstones are mostly confined to marine deep‐water systems with only limited information available on those developed in lacustrine environments. In this paper, we document the characteristics and distribution of a previously unrecognized sequence of lacustrine turbidite sandstones from the Dongying Sag in the Bohai Bay Basin, North China Craton. The Eocene Shahejie Formation...
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