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Limit of crustal drilling depth 被引量:4
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作者 Y.S.Zhao Z.J.Feng +3 位作者 b.p.xi D.Yang W.G.Liang Z.J.Wan 《Journal of Rock Mechanics and Geotechnical Engineering》 SCIE CSCD 2017年第5期989-992,共4页
Deep drilling is becoming the direct and the most efficient means in exploiting deep mineral resources,facilitating to understanding the earthquake mechanism and performing other scientific researches on the Earth’s ... Deep drilling is becoming the direct and the most efficient means in exploiting deep mineral resources,facilitating to understanding the earthquake mechanism and performing other scientific researches on the Earth’s crust.In order to understand the limit of drilling depth in the Earth’s crust,we first conducted tests on granite samples with respect to the borehole deformation and stability under high temperature and high pressure using the triaxial servo-controlled rock testing system.Then the critical temperaturepressure coupling conditions that result in borehole instability are derived.Finally,based on the testing results obtained and the requirements for the threshold values of borehole deformations during deep drilling,the limit of drilling depth in the Earth’s crust is formulated with ground temperature. 展开更多
关键词 Drilling well Limit of drilling depth High temperature High pressure Borehole instability
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稀有金属伟晶岩的地球化学和岩石成因:以刚果(金)Karagwe-Ankole成矿带Kivu地区Lemera锡矿床为例
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作者 Rub’son N’nahano-Ruhindwa HERITIER Moïse LUEMbA +3 位作者 李欢 Charles NZOLANG Donat KAMpATA Joseph NTIbAHANANA 《Transactions of Nonferrous Metals Society of China》 SCIE EI CAS CSCD 2023年第6期1873-1892,共20页
本文报道刚果(金)Karagwe-Ankole成矿带Kivu地区Lemera花岗伟晶岩型锡矿床的岩石成因和地球化学研究结果。从露头采集7个花岗岩伟晶岩样品,并采用ICP-MS和XRF光谱法对其进行全岩岩石地球化学分析。花岗伟晶岩具有较高的Al_(2)O_(3)、较... 本文报道刚果(金)Karagwe-Ankole成矿带Kivu地区Lemera花岗伟晶岩型锡矿床的岩石成因和地球化学研究结果。从露头采集7个花岗岩伟晶岩样品,并采用ICP-MS和XRF光谱法对其进行全岩岩石地球化学分析。花岗伟晶岩具有较高的Al_(2)O_(3)、较低的Fe_(2)O_(3)(T)和MgO含量(平均值分别为12.95%、0.96%和0.16%,质量分数),岩石铝饱和指数范围为1.33~2.05。一些重要稀有金属的丰度以及相关关键参数计算结果如下:Sn((1~138)×10^(-6))、Ta((0.20~0.60)×10^(-6))、Nb((1~8)×10^(-6))、Cs((1.20~3.20)×10^(-6))、Rb((3~223)×10^(-6))、Zr((7~201)×10^(-6));w(K)/w(Rb)(150~272);w(K)/w(Cs)(9.06~23.3),w(Nb)/w(Ta)(3.33~14)。结果表明,Lemera花岗伟晶岩形成于碰撞后期至后碰撞的构造环境中,由过铝质S型花岗岩岩浆结晶而成,岩浆经历了强烈的分离结晶作用。该岩体具有锡和锆的矿化。 展开更多
关键词 Kibaran成矿带 Lemera花岗伟晶岩 锡矿床 S型花岗岩 分离结晶
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