The Mesoproterozoic ‘seismite’ at Laiyuan (Hebei Province, E China) re-interpreted

Journal Title: Geologos - Year 2014, Vol 20, Issue 2

Abstract

A 1-million m3 breccia near Laiyuan (Hebei Province, E China) occurs as a block-like lithological unit between dolostones of the 1.55–1.45 Ga (Early Mesoproterozoic) Wumishan Formation. It has previously been interpreted as a seismite, but it appears not to fulfil any of the commonly accepted criteria that jointly are considered diagnostic for seismites. Its presence in a graben-like structure with almost vertical bounding fault planes rather indicates an origin as a (submarine) valley fill. As the valley originated by tectonic activity in the form of faulting, the breccia can be considered as a secondary effect of seismic activity, but it does not represent a seismite.

Authors and Affiliations

A. J. Loon

Keywords

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  • EP ID EP165176
  • DOI 10.2478/logos-2014-0012
  • Views 169
  • Downloads 0

How To Cite

A. J. Loon (2014). The Mesoproterozoic ‘seismite’ at Laiyuan (Hebei Province, E China) re-interpreted. Geologos, 20(2), 139-146. https://europub.co.uk/articles/-A-165176