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Assessment of gas tungsten arc welding thermal cycles on Inconel 718 alloy 被引量:8
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作者 M.HERNANDEZ R.R.AMBRIZ +3 位作者 R.CORTES C.M.GOMORA G.PLASCENCIA D.JARAMILLO 《Transactions of Nonferrous Metals Society of China》 SCIE EI CAS CSCD 2019年第3期579-587,共9页
Heat moving source models along with transient heat analysis by finite element method were used to determine weld thermal cycles and isothermal sections obtained from the application of a gas tungsten arc welding bead... Heat moving source models along with transient heat analysis by finite element method were used to determine weld thermal cycles and isothermal sections obtained from the application of a gas tungsten arc welding beads on Inconel 718 plates. Analytical (Rosenthal’s thick plate model) and finite element results show an acceptable approximation with the experimental weld thermal cycles. The isothermal sections determined by numerical simulation show a better approximation with the experimental welding profile for double-ellipse model heat distribution than Gauss model. To analyze the microstructural transformation produced by different cooling rates in the fusion and heat affected zones, Vickers microhardness measurements (profile and mapping representation) were conducted. A hardness decrement for the heat affected zone (~200 HV0.2) and fusion zone (~240 HV0.2) in comparison with base material (~350 HV0.2) was observed. This behavior has been attributed to the heterogeneous solubilization process of the γ″ phase (nickel matrix), which, according to the continuous-cooling-transformation curve, produced the Laves phase,δ and MC transition phases, generating a loss in hardness close to the fusion zone. 展开更多
关键词 Inconel 718 gas tungsten arc welding (GTAW) weld thermal cycle finite element method heat moving source
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海沟金矿床的成矿热动力源:来自伴生闪长玢岩的锆石CL图像和U-Pb测年证据 被引量:4
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作者 常艳 张勇 +3 位作者 孙景贵 柴鹏 李亮 杨帆 《矿物岩石》 CAS CSCD 北大核心 2013年第1期35-42,共8页
通过对海沟大型中低温热液脉型金矿床与成矿伴生的闪长玢岩(脉)单颗粒锆石CL图像分析和LA-ICP-MS U-Pb年龄测定,获得三组内部组构和年龄时段不同的锆石。其中:第Ⅰ组锆石发育内部成分环带的同时,具有强烈脆性破裂构造、并在其内部有新... 通过对海沟大型中低温热液脉型金矿床与成矿伴生的闪长玢岩(脉)单颗粒锆石CL图像分析和LA-ICP-MS U-Pb年龄测定,获得三组内部组构和年龄时段不同的锆石。其中:第Ⅰ组锆石发育内部成分环带的同时,具有强烈脆性破裂构造、并在其内部有新生锆石充填,其单点年龄为不谐和年龄,变化区间在2 292 Ma~1 262 Ma,计算得上交点为2 515Ma±34Ma、下交点为502Ma±110Ma(MSWD=0.59);第Ⅱ组以发育弱成分环带、自形—半自形晶为特征,单点谐和年龄为1 925 Ma~1 720 Ma(N=12,Mean=1 815Ma±130Ma,MSWD=0.069,MSWD=1.00);第Ⅲ组锆石则以发育清晰内部成分结构、自形为特征,单点谐和年龄为131 Ma~122 Ma(Mean=128 Ma±12 Ma,N=3,MSWD=3.2,MSWD=0.041)。从闪长玢岩岩浆作用与区域地壳演化角度分析,第Ⅰ组和第Ⅱ组锆石均为岩浆作用过程捕获的碎屑锆石,而第Ⅲ组锆石则是闪长玢岩岩浆上侵后结晶形成的锆石;依据三组锆石的内部构造特征,结合区域地质演化特征,我们认为强烈缩减的新太古代地壳区可能是海沟金矿床的伴生脉岩和含矿流体产生的热动源区,其动力学背景与中生代库拉板块向中国东部大陆俯冲引发的和龙地体向北侧兴蒙造山带的强烈挤压剪切作用相适应。 展开更多
关键词 锆石 U—Pb测年 闪长玢岩 海沟金矿床
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