1) fault fluid pressure
断裂带流体压力
2) the vertical pressure of faulted zone
断裂带正压力
1.
Based on the analysis of the vertical sealing mechanism of fault and its influncing factors, this paper puts forward the conception of favounable depth forming the vertical sealing of fault, establishes the method determining upper and lower limit depth by the equalization of the vertical pressure of faulted zone to elastic limit and intensive limit of mudstone.
在深入分析断层垂向封闭机理及其影响因素的基础上 ,提出了断层垂向封闭形成有利深度的概念 ,并建立了利用作用于断裂带正压力与泥岩弹性极限和强度极限相等来确定形成断层垂向封闭上、下限深度的方法 。
3) high displacement pressure of fault zone
断裂带高排替压力
4) hydrofracturing
[,haidrəu'fræktʃəriŋ]
流体压裂
1.
Based on a systematic analysis of gas accumulation mechanism and its main constraints together with the background and origin of overpressure in Yinggehai basin, it can be shown that the abnormal pressure is the major driver of gas migration, and that the natural hydrofracturing has produced vertical paths for gas migration.
系统地分析了莺歌海盆地天然气成藏动力学机制及主控因素 ,阐释了盆地内异常超压的发育背景及成因 ,指出异常压力是天然气运移的主驱动力 ,而流体压裂则产生了天然气垂向运移输导网络。
2.
According to the main effect parameters of hydrofracturing,the episodic compaction stage includes hydraulic fracture and hyd.
流体压裂是在异常高流体压力体系的低渗泥岩中流体活动的主要输导通道。
5) Changliu-Xiangou fault zone
长流-仙沟断裂带
1.
The Holocene volcanic activity of the Leihuling Group are distributed mainly along the Changliu-Xiangou fault zone in the Shishan-Yongxing area Many large-scale faults are found in the base-surge deposits which are created by phreatomagmatic eruptions in Shishan area.
琼北地区的火山活动以裂隙喷溢为主,晚更新世道堂期的射气岩浆喷发形成了众多的低平火山口,全新世雷虎岭期火山口主要分布于石山、永兴一带,沿NW向长流-仙沟断裂带分布。
6) steep tropopause belt
对流层顶断裂带
1.
In the steep tropopause belt to the north of the jet,the CTF varies in a zonal wave-like pattern from TST(troposphere to stratosphere tr.
分析结果表明:(1)CTF分布呈现纬向型,在副热带西风急流北侧即对流层顶断裂带中存在东西向的TST(对流层向平流层输送)-STT(平流层向对流层输送)-TST的波列结构(水平输送项决定),而南侧分布决定于垂直输送项。
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