1) large fracture belt
大断裂带
1.
At the end of Tertiary, hydrocarbons migrated vertically upward from the upper mantle along large fracture belts and accumulated in the porous-fractured reservoirs in the basement and sedimentary cove.
已故的乌克兰科学院院士波尔菲利也夫提出了油气深部起源的理论,即石油的形成与上地幔的活动有关,于第三纪末由上地幔沿大断裂带进行垂直运移并在基底及沉积盖层的孔隙-裂隙岩石储集层中聚集而形成油气田。
2) deep fractured zone
深大断裂带
1.
This paper gives a brief introduction to the structural layer, tectonic unit and structural feature of the deep fractured zone in the North-east of Jiangxi.
简要介绍了赣东北深大断裂带构造层、构造单元和构造特征,探讨了赣东北深大断裂带演化史,阐述了对寻找中生代煤炭资源的现实意义。
3) Major deep fracture zones
深-大断裂带
4) Daliangshan fault zone
大凉山断裂带
1.
The results indicate that the seismicity of the Anninghe-Zemuhe fault zone has always been stronger than that of the Daliangshan fault zone in history, which is consistent with the results from the active fault and paleoearthquake studies.
通过对比分析,研究了大凉山断裂带和安宁河—则木河断裂带的地震活动性。
5) faulted fracture belt
断裂裂缝带
6) fault zone
断裂带
1.
Analysis of hydrocarbon migration through the fault based on the interior structure of fault zone;
断裂带内部结构与油气运移及封闭
2.
Physical simulation for oil percolation migration through fault zones and its research significance;
原油通过断裂带渗滤运移的物理模拟及其研究意义
3.
Analysis of hydrocarbon migration based on the interior structure of fault zone;
从断裂带内部结构剖析油气沿断层运移规律
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。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条