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the ductile shear
    AN ANALYSIS ON THE ORE-CONTROLLED CHARACTERISTICS OF THE DUCTILE SHEAR STRUCTURE IN HUANGSHAN GOLD-ORE BELT, ZHEJIANG PROVINCE
    璜山金矿带韧性剪切构造控矿特征分析
    THE RELATIONSHIPS BETWEEN THE DUCTILE SHEAR BELT AND GOLD DEPOSIT
    韧性剪切带与金矿的关系
    Tectonic Characteristics of the Ductile Shear Zone on the North Margin of Qaidam Basin, Qinghai Province
    柴达木北缘大型韧性剪切带构造特征
    A STUDY OF INCLUSIONS FROM THE DUCTILE SHEAR BELT TYPE GOLD DEPOSITS IN HUANGTULING,HENAN
    河南鲁山黄土岭韧性剪切带型金矿床包裹体研究
    TECTONO GEOCHEMICAL CHARACTERISTICS OF THE DUCTILE SHEAR ZONE TYPE GOLD DEPOSIT IN KANGGUL,XINJIANG
    康古尔韧性剪切带型金矿构造地球化学特征
    TECTONIC CHARACTERISTICS OF THE DUCTILE SHEAR ZONE IN MAOPAI GOLD DEPOSIT AREA, JIANGXI PROVINCE, CHINA
    江西茅排金矿床含金韧性剪切带构造特征
    The tectonites in this zone include tectonic gneiss and mylonite. The biotite from the granitic mylonite gives a 40Ar/39Ar age of 105.2±1.7 Ma,implying that the ductile shear zone may be traced back to the Early Cretaceous.
    带内所形成的构造岩主要为构造片麻岩和糜棱岩类,对花岗质糜棱岩中的黑云母进行40Ar/39Ar年龄测试,获得105.2±1.7Ma,认为该韧性剪切带形成于早白垩世。
    GEOLOGICAL CHARACTERISTICS AND GENESIS OF THE DUCTILE SHEAR ZONE TYPE GOLD DEPOSIT IN MATOUTAN EASTERN TIANSHAN
    东天山马头滩韧性剪切带型金矿地质特征及成因
    MINERALIZATION SIGNIFICANCE OF GEOCHEMICAL BARRIER ON THE DUCTILE SHEAR BELT IN THE TIANWAN GOLD DEPOSIT,SHIMIAN,SICHUAN PROVINCE
    四川石棉田湾金矿床韧性剪切构造带地球化学障的成矿意义
    A Study On Fluid Action in the Ductile Shear Zone: A Review
    韧性剪切带内流体作用的研究
    Characteristics of the ductile shear zone of the eastern margin in the east section of the Mid-Qilian massif,Gansu
    中祁连东段东缘韧性剪切带特征
    Discussion on the ductile shear belt and Au-mineralization with mechanism of metallogenic dynamics from Kuangoukou to Hongqigou in the north margin of Qaidam basin
    柴北缘宽沟口—红旗沟韧性剪切带及其金成矿动力机制探讨
    On strain characters of rocks and minerals within the ductile shear zone, it is calculated that the strain value is 1.24-2.32,the forming depth is 13-20km,the temperature is 450-650℃, the surrounding pressure is 325-550MPa, the biggest shear stress is 113-141MPa and the discrepant stress is 31-35MPa.
    据韧性剪切带中岩石矿物的应变特征,计算出该韧性剪切带剪应变值为1.24—2.32,形成深度为13—20km,温度为450—650℃,围压为325—550MPa,最大剪应力为σ=113—141MPa,差异应力为31—35MPa。
    The ductile shear zone was formed under a temperature of about 400℃, differential stress of about 30 MPa, and strain rate of1.9×10-13s-1.
    此韧性剪切带形成时的温度约400℃,差异应力约30MPa,应变速率约1.9×10-13s-1。
    Study of the geological and mineralization features of three main gold deposits in the gold belt shows that gold mineralization is different during evolution of the ductile shear zone.
    通过对戈枕金矿带三种主要金矿类型地质特征及其成矿特征的研究,指出在戈枕韧性剪切带演化的不同阶段,金矿化作用不相同。
    According to its fabric characteristics the ductile shear zone migrated from SW to NE with displacement of1.94 km.
    根据其组构特征分析 ,韧性剪切带的运动方向是由南西向北东方向运移 ,位移量为 1.94 km。
    It belongs to the ductile shear zone type of a gold deposit in the greenstone belt.
    矿床受元古界基性、酸性双峰式火山岩层位及韧性剪切带双重控制, 属绿岩带中的韧性剪切带型金矿床。
    The altered mylonite type gold deposit is a kind of gold deposits whose ore\|forming mechanism and ore\|controlling factors are closely related to the ductile shear zone and mylonite zones.
    蚀变糜棱岩型金矿是一种成矿机制与控矿因素都与韧性剪切带及其糜棱岩密切相关的金矿床类型。
    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.
    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 results of~(40)Ar/~(39)Ar age dating to the K-feldspar and biotite from mylonites, and the relationships among ductile shear zone, strata and intrusions indicate that the ductile shear zone formed between 440 and 380 Ma.
    糜棱岩中钾长石、黑云母单矿物40 Ar/ 3 9Ar同位素测年结果及与地层和岩浆活动的关系表明韧性剪切带形成于 4 4 0~ 380Ma。
 

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