构造岩的研究已取得很大进展。
Some developments have taken place in the study of tectonites.
糜棱岩是断层泥破碎带常见的构造岩类。
该方法不仅能提供盆地基底构造形态，而且能提供基底岩性信息。
Therefore, the method can supply not only basement structure but also basement lithological information.
利用这些测量特性可以得到岩性、沉积构造特征和裂缝等信息。
Information of lithology, sediment structure and crack are gotten from imaging log measure information.
完整岩体压剪破裂失稳是构造地震的另一种可能孕震机制。
The fracturing of initial rock mass is another mechanism of tectonic earthquake.
研究了岩体的构造层次与其力学行为之间的关系。
The relationship between the structure hierarchy of rock masses and their mechanical behavior is studied.
圈闭类型主要发育构造-岩性复合型隐蔽圈闭。
The main trap is subtle composite trap of structure and lithology.
构造、构造—岩性复合是主要的油气藏类型；
The structure trap and structure-lithologic trap are main types of the oil and gas accumulation.
岩浆岩的侵入明显受断裂构造控制。
Magmatic intrusion obviously is controlled by faulted structure.
构造地层学方法是变质岩，尤其是前寒武纪变质岩地区地层研究的有效方法。
Structure-stratigraphic method is an effective method for stratigraphic study in Precambrian metamorphic rock area.
因此，该岩带出露区的大地构造位置应归属华北板块。
Therefore, the intrusions are located in the North China plate tectonically.
因此，该岩带出露区的大地构造位置应归属华北板块。
Therefore, the intrusions are located in the North China plate tectonically.
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