构造断阶带的不同类型控制了不同的沉积样式。
Different types of fault terraces control different sedimentary types.
东濮凹陷胡-庆断阶带为三个斜列展布的台阶式结构。
Hu - Qing fault step zone in Dongpu Depression has an echelon three - step structure.
根据构造演化剖面的分析结果，确定了高邮凹陷南部断阶带。
The south terrace in Gaoyou sag is presented, according to the analysis of the structural evolution section.
高邮凹陷南部断阶带构造破碎、藏条件复杂，导致勘探效益低。
The exploration in south fault-terrace belts of Gaoyou Depression is of low benefit owing to its fractured structure and complex oil-forming condition.
从结构上可以将陡坡带分成同向断阶带、反向断阶带和单斜型断超带三种原型。
Structurally, they were classified into three types, synthetic fault bench, antithetic fault bench and monocline overlap fault belt.
稠油主要分布在断阶带上盘，正常油和轻质油分布在断阶带的下盘及断阶带之间。
The heavy oil is distributed at the handing wall, light oil and gas reservoir at the footwall.
北部为受生长断层控制的陡坡断阶带，以典型的水下扇、浊积扇和扇三角洲近端前缘沉积为主。
But in the north part of the sub-sag, controlled by the syn-sedimentary fault, steep fault-step was developed with mainly deposition of sub-aqueous fan, turbidity fan, and front of fan-delta.
东部为单斜、顺向断阶带构造背景控制下的多期次的扇三角洲沉积体系，部分地方发育冲积扇体系。
The eastern part is multi-stages fan delta deposit system witch is controlled by the monocline and step-fault zone and another parts in the area grow alluvial fan system.
准噶尔盆地西北缘红车断阶带油气分布复杂，油气藏类型多，有稠油、正常油和轻质油，还有干气藏。
The oil and gas reservoir types are very various in Hongthe faults of northwestern part of Zhungaer basin, including heavy oil, light oil and dry gas.
歧南断阶带的成岩-孔隙演化模式表明，研究区内特定的成岩-孔隙演化史有利于深层沙河街组二段砂岩孔隙的保存。
The diagenesis-porosity evolution history is beneficial to porosity preservation of Shahejie Formation at great depths in the vicinity of Qi'nan fault-step zone, Bohai Bay.
断阶型陡坡坡折带控制着扇三角洲或近岸水下扇及前方的湖底扇体系的形成和分布；
The faulted terrace type steep slope break belt controlled the development of the fan-deltas and sub-aqueous fan system.
断阶型缓坡坡折带控制着扇三角洲沉积体系的形成和分布；
The gentle slope type slope break belt controlled the development of the fan delta system.
裂陷期的同沉积断裂组成了多种复合的构造样式：西部斜坡带主要发育断阶、地堑和地垒构造；
Faults developed in synrift phases formed several structural styles: the fault terraces, grabens and horsts were generated in the western slope belt;
裂陷期的同沉积断裂组成了多种复合的构造样式：西部斜坡带主要发育断阶、地堑和地垒构造；
Faults developed in synrift phases formed several structural styles: the fault terraces, grabens and horsts were generated in the western slope belt;
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