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在室内航片解释的基础上,依据野外现场实测资料,应用地质地貌学方法,对走滑断裂上由蠕滑作用形成的弧形,“正”、“逆”牵引变形山脊及断错变形冲沟的4种地貌形态进行了讨论,并根据这些蠕滑标志,测量了昌马断裂带中、东段的蠕滑量。给出了粘滑与蠕滑量的比值及蠕滑量占总走滑量的比例在断裂带上的分布情况。
On the basis of interpretation of indoor aerial photos, according to the field observation data and geomorphology method, the arc, “positive” and “inverse” traction deformation ridge on the strike slip fracture and fault deformation According to these creep signs, the creep slip in the middle and east Changma fault zone was measured. The ratio of stick-slip to creep slip and the distribution of creep slip in the fault zone are given.