1) Yinwashan Fault
阴洼山断裂
1.
The Yinwashan Fault situates in the western part of Hexi Corridor at the northern side of the Yinwashan Mountains, about 18km to the west of Jiayuguan city.
阴洼山断裂属于河西走廊内的断裂带,位于嘉峪关以西28km的阴洼山北侧及附近,呈NW向延伸,长25km,自NW向SE具有活动时代逐渐变新的特点。
2) western Yinwashan fault
阴洼山西缘断裂
3) The Tongshan fracture
铜山断裂
4) 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。
5) 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。
6) The Taoshang fault
桃山断裂
补充资料：阴那山
阴那山位于梅县雁南镇，距梅城46公里。这里的山呈东北西南走向，绵延300余里。风景区范围6.6平方公里。山顶五峰并列，海拔均超千米，故有"白云深处望三州(梅州、潮州、汀州)之说。阴那山突起于梅江平原之上，山势雄奇，峰峦叠翠，冬季山顶有积雪。具有"神山、群峰、奇石、翠瀑、浮云"的特色。
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