1556年陕西华县大地震的地面破裂
GROUND RUPTURES DURING THE LARGE EARTHQUAKE OF 1556, HUAXIAN COUNTY, SHANXI
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摘要: 本文着重研究了近代工程施工中发现的大量震害遗迹, 诸如断层、裂缝、喷水冒砂现象, 诱发滑坡和坠入地震断裂带中的木炭与文物.又经考古研究和 C14鉴定属明代之物, 证实这条在极震区延伸大于70公里的破裂带就是这次大地震极震区地面破裂带.Abstract: In the present paper, a large number of vestiges of earthquake damage, discovered in engineering works: in recent times, such as faults, fissures, phenomena of water and sand eruption, induced eboulements, charcoal and cultural relics fallen in earthquake fault zones, are studied. By means of archaeological study and verification of C14, it is proved that those mentioned above might originate in the Ming Dynasty and that the rupture zone extended for more than 70 kilometres in the meizoseismal area is the very ground rupture zone of the meizoseismal area of this large earthquake.
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[1] 郭增建, 1556年1月23日关中大地震, 地球物理学报, 6, 1, 1957.
[2] 蒋溥、高维安, 强震地面破坏效应及其形成的地质条件, 地质科学, 1, 1976.
[3] 时振樑、环文林、姚国干、谢原定, 1932年昌马地震破裂带及其形成原因的初步探讨, 地球物理学报, 17, 4, 1974. -
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