1) The Taoshang fault
桃山断裂
2) The Tongshan fracture
铜山断裂
3) the Tangshan faulted zone
唐山断裂
1.
This active fault is the stretch of the east branch fault(F5) of the Tangshan faulted zone which was triggered tectonics of the Tangshan earthquake in 1976.
得出地表地裂缝生成的主要原因是其地下深处可能存在隐伏活动断裂的活动(蠕动),该活动断裂为1976年唐山大地震发震构造—唐山断裂带东支唐山矿F5断层之延伸,而小煤矿采空塌陷加剧了地裂缝的发展,是诱因。
4) Mishan fault
米山断裂
1.
Mishan fault is considered as a multi period deformed fault with ductile deformation in early period and brittle deformation in later period.
米山断裂是一多期变形的断裂。
2.
Main alteration is intense silicification Therefore, formation and devolopment of Mishan fault is important to petrogenesis and metallo-genesis in east Jiaodong.
米山断裂是─多期变形断裂，早期以韧性变形为主，后期以脆性变形为主，断裂变形具有准对称性，西盘变形强度大于东盘。
5) Shanxi downfaulted zone
山西断裂
1.
Study on the relation of crustal deformation with seismic activity in Shanxi downfaulted zone;
山西断裂带的地震活动与形变资料分析研究
补充资料：猕猴桃(Actinidia chinensis)，猕猴桃科
李泽贤摄
[图]
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条