- 更多网络例句与球状闪长岩相关的网络例句 [注：此内容来源于网络，仅供参考]
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The mineralization and the alteration types are clearly distributed around the hornblende quartz diorite porphyry intrusion.
其矿化围绕含眼球状石英斑晶的角闪石石英闪长玢岩及其环带状蚀变带分布。
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According to logging results of 167 boreholes and chemical analyses of 24 369 samples as well as characteristics of element distribution at 4 000 m, 3 950 m and 3 900 m levels, the deposit is characterized by alteration, mineralization and element geochemistry of the porphyry. Alteration and mineralization are spatially and temporally related to the augen quartz phenocryst_bearing hornblendequartz diorite porphyrite (J3δομ).
根据167个勘探钻孔编录和化学分析（24369件化学分析样品）资料，以及对海拔4000 m、3950 m、3900 m水平面的Cu、Au、Ag、Mo、Mn、P b、Zn、W、K、Na、Ca、Rb元素分布规律的分析，显示矿体具有斑岩型矿床的蚀变、矿化以及元素地球化学特征，主要矿化和围岩蚀变在时间上和空间上均与含眼球状石英斑晶的角闪石英闪长玢岩（J3δομ）有关。
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According to logging results of 167 boreholes and chemical analyses of 24 369 samples as well as characteristics of element distribution at 4000 m, 3950 m and 3900 m levels, the deposit is characterized by alteration, mineralization and element geochemistry of the porphyry. Alteration and mineralization are spatially and temporally related to the augen quartz phenocryst-bearing hornblende-quartz diorite porphyrite (J3δομ).
根据167个勘探钻孔编录和化学分析（24369件化学分析样品）资料，以及对海拔4000m、3950m、3900m水平面的Cu、Au、Ag、Mo、Mn、Pb、Zn、W、K、Na、Ca、Rb元素分布规律的分析，显示矿体具有斑岩型矿床的蚀变、矿化以及元素地球化学特征，主要矿化和围岩蚀变在时间上和空间上均与含眼球状石英斑晶的角闪石英闪长玢岩(J3δομ)有关。
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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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Luanping orbicular dioritic pluton has special geochemical characteristics with unusual enrichment in Al 2 O 3 (21.58%～26.80%)and relative poorness of K 2 O(0.35%～1.87%).
滦平球状闪长岩体具有特殊的地球化学性质，其中最显著的岩石化学特征表现为高度富Al2O3(21.58%～26.80%)而相对贫K2O(0.35%～1.87%)。
- 更多网络解释与球状闪长岩相关的网络解释 [注：此内容来源于网络，仅供参考]
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ball diorite：球状闪长岩
ball clay 球土 | ball diorite 球状闪长岩 | ball granite 球状花岗岩
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Napierian logarithms：自然对数;讷氏对数
"naphtholithe","沥青页岩" | "Napierian logarithms","自然对数;讷氏对数" | "napoleonite; corsite","球状闪长岩"
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orbicular：球状(构造)
橙黄石 orangite | 球状(构造) orbicular | 球状闪长岩 orbicular diorite
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orbicular diorite：球状闪长岩
球状(构造) orbicular | 球状闪长岩 orbicular diorite | 球状辉长岩 orbicular gabbro
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ball pitchstone：球状松脂岩
球状闪长岩 orbicular diorite | 球状松脂岩 ball pitchstone | 球状体 spheroid
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corsite：球状闪长岩
corrugation structure 煤的揉皱构造 | corsite 球状闪长岩 | corundellite 珍珠云母
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napoleonite; corsite：球状闪长岩
"Napierian logarithms","自然对数;讷氏对数" | "napoleonite; corsite","球状闪长岩" | "nappe","推覆构造;岩盖;岩幂"
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napoleonite：球状闪长岩
球状闪长岩 ball diorite | 球状闪长岩 napoleonite | 球状闪长岩 orbicular diorite
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napoleonite：球状辉长岩 球状闪长岩
napkintissues 餐巾薄纸 | napoleonite 球状辉长岩 球状闪长岩 | nappattern 毛结花纹