Typical earthquake-induced soft-sediment deformation structures in the Mesoproterozoic Wumishan Formation, Yongding River Valley, Beijing, China and interpreted earthquake frequency
The Mesoproterozoic Wumishan Formation, composed of dolomite is a widely distributed stratigraphic unit in the Beijing area. It was formed over a long period of time in the Yan-Liao aulacogen, a stable peritidal environment that was ideal for recording earthquakes in the form of soft-sediment deform...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
SpringerOpen
2012-07-01
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Series: | Journal of Palaeogeography |
Subjects: | |
Online Access: | http://www.sciencedirect.com/science/article/pii/S2095383615301140 |