并依据电性资料划分了构造单元，探讨了各单元的构造接触关系。
Moreover, tectonic units are divided and the tectonic contact relations of each unit are approached according to electrical data.
由于受后期构造叠加改造的影响，现今二者呈断层或隐蔽不整合接触关系。
Owing to the influence of tectonic superimposition and reworking at the late stage, both show fault or hidden unconformable contact relationships at present.
伊犁盆地新构造运动在地貌、断裂活动和地层接触关系等方面表现十分明显。
Neotectonic activity of Yili basin shows apparent evidences on land form, fault activities and stratigraphic contact.
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