1) Kongxi fracture belt
孔西断裂带
1.
Control role of lateral oil migration along fault on Mesozoic reservoir-forming of Kongxi fracture belt;
侧接式运移对孔西断裂带中生界成藏的控制
2) Gangxi faulted zone
港西断裂带
1.
Based on analyses of Helium isotope and laser Raman spectroscopic component of Ordovician and Tertiary inclusion samples in Gangxi faulted zone of Huanghua depression, it is believed that the inclusions are commonly mantle-derived and are locally enriched.
对黄骅坳陷港西断裂带奥陶系和第三系包裹体样品的氦同位素分析以及对单个包裹体激光拉曼组分测试表明,包裹体普遍具有地幔成因,且局部十分富集,同时发现包裹体中的硫化氢含量较高,范围分布在5。
3) Wenxi fault zone
文西断裂带
1.
The relationship between structural characteristics and hydrocarbon migration in Wenxi fault zone;
文西断裂带构造特征与油气运聚关系
4) Shanxi rift zone
山西断裂带
1.
Analysis on horizontal deformation of Shanxi rift zone in recent years;
近几年山西断裂带水平形变的初步分析
5) Guxi fault zone
孤西断裂带
1.
The Guxi fault zone, controlled by the Guxi fracture in the north direction, has three reservoir types, including unconformity .
通过对孤西断裂带下古生界褶皱块断型潜山油藏的综合研究,总结出孤西潜山带经历印支期挤压逆冲、燕山期拉张负反转和喜马拉雅期拉张断裂改造3个构造演化阶段,形成了受北西向孤西断裂控制的内幕褶皱块断型潜山带,发育了不整合面风化壳型、潜山内幕孔洞型和构造裂缝型3种储集层类型,进一步厘定了高潜山和低潜山2大类5种潜山油气成藏模式,其中高潜山油气藏模式有风化壳型、反向断块内幕型和地层不整合型,低潜山油气藏模式有反向断块和顺向断块型2种,这对济阳坳陷潜山勘探及多样性潜山理论的完善具有重要意义,为实现成藏规律指导下的潜山勘探奠定了基础。
2.
Previous research has concluded that the natural gas is mainly composed of coal-bed gas in Guxi fault zone,one of the richest areas of deep natural gas in Jiyang depression.
针对以前的研究认为济阳拗陷孤西断裂带深层天然气主要发育煤成气,以烃源岩特征分析为基础,综合运用天然气组分、稳定碳同位素、稀有气体同位素、轻烃组成和伴生油生物标志物等多种指标,并结合成藏地质条件分析,系统剖析了孤西断裂带古生界天然气的成因和来源。
3.
The geological structure of Guxi fault zone is very complex and the velocity changes a lot at lateral direction.
孤西断裂带地质构造十分复杂,速度横向变化较大,该区已进行了三维连片处理,但潜山的构造背景及准确细致的构造形态仍不清楚,制约了对该区带的深入地质研究和评价。
6) west Lamulun fault zone
西拉木伦断裂带
1.
Typical migmatites within the northern Shuangjing micro-plate in west Lamulun fault zone of Inner-mongolia,were characterized by obvious alternated bands of mesosome-melanosome-leucosome.
西拉木伦断裂带双井微地块北部边缘出露有以条带状为主的混合岩,岩石中中色体-暗色体-浅色体明显分带,岩相学特征显示暗色体和浅色体经历了较高温的交代变质作用。
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