断裂带

密山&抚顺断裂带构造岩之显微构造特征

Microstructural Features of the Mishan & Fushun Fault Zone Tectonite

招平断裂带金矿勘查模型与成矿预测

Gold Exploration Model and Mineralization Predication in Zhao-Ping Fault Zone

两处地震没有关联性中国地震台网中心等部门的专家经过会商指出，两次地震地处我国不同断裂带，不做关联性分析。中国地震台网中心研究员孙士鋐表示，云南和青海地震没有关联。

There was no causal relationship between the Yunnan and Qinghai quakes , but they shared the same root cause , Sun Shihong , a researcher at the China Earthquake Networks Center , said .

铜山铜矿F1断裂带构造控矿特征分析

Ore-controlling character of f_1 fracture zone of Tongshan Copper Deposit

GPS测量所揭示的西秦岭北缘断裂带现今活动特征

Current Activity Characteristics of the Fault Zone Along the North Margin of West Qinling Mountain Revealed by GPS Measurements

长趋势GPS地壳形变图像反映了这条活动断裂带相对完整的左旋走滑活动。

The secular GPS crustal deformation image has reflected the relatively complete left lateral strike slip movement of this active fault zone .

秦岭地区城口&房县断裂带变形特征及ESR定年

Deformation Characteristics and the ESR Dating of Chengkou-Fangxian Fault Zone in the Qinling area

1067年和1574年地震可能都发生在NE向的滨海断裂带上。

Both the 1067 and the 1574 earthquakes were produced possibly along the NE-trending Off-shore Fault zone .

盆内深断裂带为CO2气藏供气或输气通道，深大断裂带控制了CO2气藏的空间分布，为主控因素。

The deep big faults provide CO2 with flowing paths , control the spatial distribution of the CO2 reservoirs . These faults are the most important controlling factor .

沂沭断裂带断层泥中K-Ar、FT和TL体系年代学含义的初步研究

GEOCHRONOLOGICAL implication of k-ar , ft and TL systems of fault gouge from Yi-Shu fault zone

利用山西断裂带布设的GPS监测网的6期复测资料（1996&2001），分析了山西断陷带的水平运动特征。

An Analysis of horizontal movement characteristics of Shanxi fault belt is made by using 6 retest data of 6 periods ( 1996-2001 ) of GPS monitoring network in Shanxi fault belt .

在印度板块向欧亚大陆俯冲碰撞过程中，产生一系列深大断裂带，形成大量CO2释放脱气点。

There are come into being a series of deep seated fault zone and a great deal CO2 degasification point through the collision between Indian and Asian plates .

相带C2沿着南部的盆地边缘断裂带分布，为冲积扇。

The C2 seismic facies area is scatted along the basin-bounding fault in the south depression and is interpreted as an alluvial fan .

湘东北普乐及横洞原生钴矿床均赋存于长平断裂带F2主干断裂下盘构造热液蚀变岩带中。

Original Co-deposits of Pule and Hengdong in northeast Hunan occurred in tectonic , hydrothermal , altered rock zone of the lower plate of main fracture belt F2 , Changping fracture zone .

震源投影图显示：震群集结于莲花山断裂带南沿的F1断层沿伸线两侧，说明F1断层是震群的发震断层；

Projections of sources have shown that swarm events were concentrated at both flanks of the extension of F2 fault which was located along the southern boundary of the Lianhuashan fault zone , suggesting that F1 fault was the seismogenic fault for the swarm .

本文较系统地阐述了利山金矿床的各项地质特征，并重点就控矿构造问题进行了总结讨论，认为NWW向断裂带严格控制了所有金矿体的产出。

This paper deals systematically with the various geological characteristics of the Lishan gold deposit , highlighting the ore controlling structures .

F1断裂带是区内铅锌矿床的主要控矿构造，V1主矿体沿断裂走向分布，各种构造变形现象较为丰富。

F1 fault is major controlling structures , and No. V1 ore body and some other ore bodies distributes along the fault strike , and which is rich in varieties of structural deformation phenomena .

该区断层产状沿走向变化频繁，在短短的20km范围内，出现了6个彼此倾向相反的断裂带。

In this area , fault occurrence changes frequently , so that in 20km extent there occur 6 fault zones whose dip directions are opposite each other .

新构造运动活跃，晚更新世以来的活动断裂带就有24条之多，断裂带展布的上风方向以NW及NWW向为主。

Neotectonic movement is active , since the epipleistocene active fault zone has had24 to be many , the predominant direction of fault zone by NW and NWW to primarily .

肥东韧性剪切带中糜棱岩、超糜棱岩测得的~（40）Ar/~（39）Ar全岩年龄分别为120.48Ma和118.75Ma，说明郯庐断裂带的大规模左行平移时代为早白垩世。

The mylonite and ultramylonite in the ductile shear zones yield whole-rock 40Ar / 39Ar ages of 120 . 48 Ma and 118 . 75 Ma respectively , which suggest that large-scale sinistral displacement in the Tan-Lu fault zone took place in the Early Cretaceous .

通过3个不同层次的遥感工作（1：10万TM卫片解译；1：3.5万航片判释；1：1万航测成图），在沂沭活动断裂带区成功进行铁路选线。

A location of railway route has been successfully made through three different levels of remote sensing work : TM satellite image interpretation ( scale 1 : 100000 ) , aerial photo interpretation ( scale 1 : 35000 ) and aerial surveying alignment ( scale 1:10000 ) .

变形构造研究显示阿尔金断裂带东段可划分成具有近水平拉伸线理的韧性左行走滑变形域（SS）和具有陡角度倾伏拉伸线理的收缩变形域（PS）。

Studies of deformation structure in the eastern segment of the Altun fault zone indicate that it can be divided into the ductile sinistral strike-slip domain with subhorizontal stretching lineations ( SS domain ) and the contractional deformation domain with steeply plunging stretching lineations ( PS ) .

银山背斜断裂带及次级构造，为导矿、容矿创造了有利空间，是控岩、控矿的主要因素，近EW向断裂控制了矿区各矿化带的矿体。

Yinshan upfolds the fault zone and the secondary construction create a favorable space for leading ore. It is the the main factor of rock control and ore control . Near EW , the fault zone controls the ore of every mineralized zone . 3 .

秦岭北缘洛南&栾川断裂带是华北板块南缘与秦岭造山带汇聚-拼合带，具有SW→NE向俯冲兼左旋走滑的性质，并构成叠瓦状构造和双重构造的组合样式。

The Luonan-Luanchuan fault zone on the northern margin of the Qinling Mountains is a convergence belt between the North China plate and Qinling orogenic belt with the natures of SW-NE-directed subduction and sinistral strike-slip motion . It shows an association style of imbricate structure and duplex structure .

地形变和地磁异常也观测到了.分析发现：前兆不是沿断裂带分布，而主要是位于近震中（≤50km）的破裂面法线方向；

It is found that the precursors had not distributed a-long rupture zones , but mainly in the normal direction of fracture plane near the epicenter (≥ 50 km ), the focus is not on early fracture .

在500MPa的压力范围内测定了红河断裂带断层泥的密度、纵波速度和横波速度随压力的变化。

The Change of density , compressive and shear wave velocity of gouge of the Red River fault zone followed pressure was measured up to 500 MPa .

额尔齐斯活动断裂带由5条活动断裂构成，自东向西撒开，延伸约650km，具右旋走滑逆冲性质。

Ertix active fault zone , consisting of five active faults with an extension of about 650 km from east to west , owns characteristics of right-handed strike-slip thrusting .

区域资料显示，沿阿尔金主断裂带旁侧普遍存在8Ma±的磷灰石裂变径迹年龄。

Regional data also show that 8 Ma obtained by fission track dating of apatite is widely spread along the fault , suggesting a period of rapid strike slip of the fault during this time .

在275口探井中，有31口探井探明了10个中型整装油气田，全部聚集在断阶、断裂带上继承性的坳边隆（Kz、Mz）的圈闭内；

275 prospecting wells were drilled here , and 10 medium-sized complete oil-gas fields have been found by 31 wells of them , all of which are concentrated in traps of successive depression-side uplifts ( Kz , Mz ) on the fault terrace and fracture belt ;

锡矿带受莲花山断裂带的次一级断裂制约，矿床、矿体主要产于NE-NEE向层间滑动断裂及其派生裂隙中，锡矿具有构造定位的特征。

The tin ore zone is restricted by the second-order fractures of the Lianhuashan fault belt , and the ore deposits and orebodies mainly occur along the NE-NEE interlayer-gliding fractures and their derivative fissures , showing structural positioning features .