The Regional Tectonic Characteristic and Their Evolution of Metamorphic Rock Formation Kekesha Area in Dulan County, Qinghai
青海都兰县可可沙地区变质岩层构造变形特征及其构造演化
separation fracture
分离剥裂；张裂隙；岩层或岩体构造分离破裂
some thin beds of layered sandstone and dark grey siltstone show slump structures.
一些薄层砂岩和暗灰色粉砂岩显示出滑动构造。
Bedding is the most important structural feature of sedimentary rock.
层理是沉积岩最主要的构造特征。
Tectonic-sequence-based Lithofacies and Paleogeography of Permian in South of China
中国南方二叠纪构造—层序岩相古地理
The layer order of ore-hosted strata is normal by structural feature.
根据小构造标志，判定含矿岩系地层为正常层序。
Results It shows that lithology of turbidite is similar with that of wallrocks. Blocky bedding,parallel bedding, cross-bedding and convolute structure are better developed in this area.
结果 该套浊积岩岩性同围岩类似,块状层理、平行层理、交错层理和包卷构造较发育;
The Evolution of Tectonic Sequence-based Lithofacies-paleogeography and Its Significance of Accumulation of Superimposed Basins;
叠合盆地构造—层序岩相古地理演化及成藏效应
The Seismic Prospecting Technology for Deep Clastic Non-Structural Trap in Tahe Oilfield
塔河油田深层碎屑岩非构造圈闭地震勘探技术
Layered intrusions are characterized by a typical layering structure and rhythmic texture.
层状岩体的典型特征是其具有层状构造和韵律结构。
Forecasting Method of Tectoclase in the Igneous Reservoirs Using a Curvature of the Microtectonics
火成岩油气储层中构造裂缝的微构造曲率预测法
Structure of Metamorphic Rock and Deformation ?
变质岩构造及变形构造
Folds are undulations or waves in the rocks of the earth. They are best displayed by layered rocks, such as sedimentary and volcanic rocks.
褶皱构造就是地球中岩石的波状起伏。它们在沉积岩和火山岩这些层状岩石中发育最好，
Stratigraphic System and Framework of Non-Smith Strata in Mianxian-Lueyang Tectonic Melange Belt, South Qinling Mountains
南秦岭勉略构造混杂岩带非史密斯地层系统和地层格架
Without internal structure or layers and homogeneous in composition. Used of a rock.
块状的无内部结构或层理的或构造相同的，用于指岩石
Foliated fault rocks are characterized by well-developed foliation which is resulted from the preferred orientation of mineral grains in the rock.
片理化断层岩石具有发育良好的面理构造，这些面理是岩石中矿物颗粒优选定向而造成的。
These reservoirs may develop as a result of either structural or stratigraphic causes.
由于构造或地层方面的原因，这些储集岩可以进一步发育。
In order to map the structure of the upper surface of such a sandstone body, abundant well control is required.
要编出这种砂岩体的上层面构造图，需要有大量的钻井资料。