Corrigendum to: Architecture of lacustrine deposits in response to early Carboniferous rifting and Gondwanan glaciation, Nova Scotia, south-east Canada

Abstract

Tang, W., Pe Piper, G., Piper, D.J.W., Chen, A., Hou, M., Guo, Z. and Zhang, Y. (2024) Architecture of lacustrine deposits in response to early Carboniferous rifting and Gondwanan glaciation, Nova Scotia, south-east Canada. Sedimentology, 71, 457–485.

The published version of Fig. 5 is incorrect. The correct version, with its caption, is provided below.

Fig. 5

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Soft-sediment deformation structures in sandstones and siltstones. (A) Brittle thrust fold (a) and bedding-parallel shear plane (b) in deformed siltstone bed. (B) Brittle boudinage of otherwise undeformed sandstone bed. (C) Detail of sandstone dyke in Fig. 4D; (a) shale parting in dyke; (b) bedding-parallel injection of sand from dyke. (D) Detail of boudins in (B) showing abrupt and undeformed lateral terminations of sandstone bed; (a) load structure at base of bed. (E; right) Detail of ‘breccia’ in Fig. 4D showing loading relationship of sandstone to envelopingblack shale; (left) complex dyke, (a) bedding parallel sandstone; (b) upward injected dyke; (c) downward injecteddyke. The locations of the photographs are shown in Fig. 2.