张节理是由于张应力超过岩石的抗性强度而在岩体中产生的张破裂面。
... gash jointn.张节理,逐渐尖灭的张裂隙 gash joint张节理;逐渐尖灭的张裂隙 gash breccian.崩塌角砾岩,裂隙角砾岩 ...
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晚期无金石英脉受控于南北向张节理。
The late quartz vein of non-gold is controlled by the tension joint of SN.
在较高的法向应力下，含起伏角较高齿形节理面的非贯通节理岩体可能出现破坏模式II（先张拉后剪切破坏模式）。
However, at higher angle of tooth-shaped asperities and under higher normal stress, the failure model II is found, which is in first tension but final shear failure.
张振南，葛修润。地震载荷作用下的节理岩体破裂模型。岩石力学与工程学报，2005,24 (10)：1645 ~ 1648。
Zhang Zhennan, Ge Xiurun. Fracture model of jointed rock mass subjected to seismic loading. Chinese Journal of rock Mechanic and Engineering, 2005, 24 (10) : 1645 ~ 1648.
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