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This study was only focused on the No.Ⅰore body. Based on detailed logging and dating results, it is considered that mineralization of the Cu_Au porphyry occurred in Late Jurassic. The formation of the ore body is related to the Late Jurassic augen quartz phenocryst_bearing hornblende_quartz diorite porphyrite intrusion(J3δομ).
通过对雄村铜金矿床Ⅰ号矿体详细的地质编录和测年成果,发现雄村斑岩型铜矿床形成于晚侏罗世,矿体的形成与晚侏罗世侵位的、含眼球状石英斑晶的闪长玢岩(J3δομ)有关,成矿岩体呈不规则的岩枝状,全岩矿化,岩体中Au的平均品位大于1g/t,Cu含量大于0.7 %。
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The mantle shear zone formed at lithospheric extensional setting of Meso-Tethys and reworked by serpentinization, cataclasis, and compressional deformation including deformed lens such as ophiolite, gabbro, and chronite, thrust faults, and folds produced during closure of the Meso-Tethys.
在南北向挤压导致海盆消亡的早期阶段,处于深层侵位环境的地幔橄榄岩由于物性的不均一性,变形分解作用产生不同尺度的透镜网络,如蛇绿岩体、辉长岩脉、纯橄岩异离体、豆荚状铬铁矿体、眼球状橄榄石、辉石残斑晶等。
- 更多网络解释与眼球状体相关的网络解释 [注:此内容来源于网络,仅供参考]
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augen:眼球状体
schist 片岩 | augen 眼球状体 | paragneiss 副片麻岩