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1)  fault steep slope belt
断裂陡坡带
1.
The article analyzed the sequence patterns and the characteristics of the first-member of Shahejie Formation in the area of the fault steep slope belt.
板桥凹陷为一单断式箕状断陷,在凹陷的西北侧断裂陡坡带发育,本文以该区断裂陡坡带沙河街组一段为研究对象,对其层序样式和沉积体系特征进行了深入研究。
2)  actic region of faulted lake basin
断陷湖盆陡坡带
3)  fault slope break
断裂坡折带
1.
The study reveals the fault slope break correlates intimately with the exploration of subtle oil and gas reservoir in fault basin.
从系统的角度出发,分析了渤南洼陷新生代断裂坡折带的构成、特征、演化及其沉积模式。
4)  fault slope-break zone
断裂坡折带
1.
The main syndepositional faults along the southeastern and northeastern margins of the ancient uplift formed obvious geo-morphologic abrupt zones or fault slope-break zones.
古隆起的东南和东北缘发育的主要同沉积断裂形成明显的古地貌突变带或断裂坡折带。
5)  steep slope
陡坡带
1.
Sedimentation feature and controlling factors of the deep glutenite fans in the northern steep slope.Dongying sag——taking Well Fengshen-1 area as an example;
东营凹陷北部陡坡带深层砂砾岩体沉积特征及控制因素——以丰深1地区为例
2.
Sedimentary characteristics of nearshore subaqueous fans in steep slope of Dongying depression;
东营凹陷北部陡坡带近岸水下扇沉积特征
3.
Classification and distribution of glutenite on the steep slope of faulted lake basin in Jiyang depression;
济阳坳陷断陷湖盆陡坡带砂砾岩体分类及展布
6)  steep slope belt
陡坡带
1.
Tectonic pattern and hydrocarbon reservoir formation in steep slope belt of Yangxin Subsag;
阳信洼陷陡坡带构造样式与油气成藏
2.
Fault structures of northern steep slope belts and their influences on sedimentation and reservoir formation in Chezhen Sag;
车镇凹陷北部陡坡带断裂结构及其对沉积和成藏的控制
补充资料:断裂带

亦称“断层带”。有主断层面及其两侧破碎岩块以及若干次级断层或破裂面组成的地带。在靠近主断层面附近发育有构造岩,以主断层面附近为轴线向两侧扩散,一般依次出现断层泥或糜棱岩、断层角砾岩、碎裂岩等,再向外即过渡为断层带以外的完整岩石。断层带的宽度以及带内岩石的破碎程度,决定于断层的规模、活动历史、活动方式和力学性质,从几米至几百米甚至上千米不等。一般压性活压扭性断层带比单纯剪切性质的断层带宽。在一些大型的断层带中,由于被后期不同方向的断层切错,和夹有一些未破碎的大型岩块,只是断层带的结构趋于复杂化,从而在近代的断层活动中容易形成运动的阻抗,是应力易于积累和发生地震的场所。

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