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mineralization相关的网络例句

查询词典 mineralization

与 mineralization 相关的网络例句 [注:此内容来源于网络,仅供参考]

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。

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。

The feature of oxygen isotope for magnetite from Abagong iron deposit reflects that the water in the fluid of mineralization resides in the initial magma, implying the magma genesis of mineralization. The similaritary features of REE and trace elements for coexisting apatite with magnetite in the Abagong, the Kiruna type and the Ninwu porphyrite iron deposit show their common genesis, indicating that Abagong iron deposit resulted from the intrusion of late ore magma due to the magma differentiation. The characteristic of sulfur isotope composition implies that the Abagong iron deposit resides in basaltic magma from mantle resource.

阿巴宫铁矿磁铁矿氧同位素特征反映了成矿流体中水来源于原始岩浆水,暗示该铁矿的岩浆成因;与磁铁矿共生的磷灰石稀土和微量元素特征与Kiruna型铁矿以及宁芜玢岩铁矿中磷灰石特征非常相似,表明它们具有相同的成因机理,反映出阿巴宫铁矿为岩浆分异的晚期矿浆贯入式成因;其硫同位素特征表明成矿物质源自幔源的玄武质岩浆。

The mineralization temperature is in a range of 90℃~300℃, and the mineralization fluid is a combination of slightly acidic-slightly alkalic precipitations, seawater and magmatic water.

其成矿温度在90~300℃之间,成矿流体为低盐度的弱酸性-弱碱性大气降水、海水和岩浆水的混合溶液。

Researches to the gold-bearing quality of sedimentary and magmatic rocks show that most of these rocks have more gold content than the average of the upper crust. Further evidences are quoted to support the view that fluids exist in shallow crust have the ability resolve some gold. Moreover, in the convergent compression, deep melting of the lower lithosphere can bring some Au and mineralization materials and move up to upper crust. Regional faults, which formed in geosynclinal and diwa periods, controlled the partial distribution of intrusions and gold mineralization belts, i.e.

区域地层和岩浆岩的含金性表明,岩浆岩和大部分地层均具较高的金异常含量,而进一步的研究表明浅部地壳的流体对地层中的金具一定的溶解和搬运迁移能力;而在汇聚挤压构造体制下由深熔作用生成的岩浆可以从岩石圈深部携带部分金和其它成矿物质并迁移到地表浅部,地槽期和地洼期形成的区域断裂构造共同控制了中新世岩浆的侵入和金成矿带的分布。

Results There were more mineralization nodes to form in shorter time in the 1×105/ml cell density group compared with in the 2×105/ml cell density group, but in the 5×105/ml cell density group, there were not, and with the DMEM medium contained β-glycerophosphate sodium and ascorbic acid, mineralization nodes formed more early compared with the DMEM medium.

结果 在培养30天内,条件培养液或常规培养液培养的5×105个/ml组细胞无结节形成;而2×105个/ml组和1×105个/ml组都有钙化结节形成,而且有细胞越少形成结节越早,数量越的趋势;给予条件培养液又较常规培养液培养有结节形成早而多的趋势。

Results There were more mineralization nodes to form in shorter time in the 1×105/ml cell density group cnpared with in the 2×105/ml cell density group, but in the 5×105/ml cell density group, there were not, and with the DMEM medium contained β-glycerophosphate sodium and ascorbic acid, mineralization nodes formed more early cnpared with the DMEM medium.

结果 在培养30天内,条件培养液或常规培养液培养的5×105个/ml组细胞无结节形成;而2×105个/ml组和1×105个/ml组都有钙化结节形成,而且有细胞越少形成结节越早,数量越多的趋势;给予条件培养液又较常规培养液培养有结节形成早而多的趋势。

Cultured osteoblasts at suitable cell density can easily form mineralization nodes in vitro, and β-glycerophosphate sodium and ascorbic acid just promote formation of mineralization nodes.

体外培养成骨细胞钙化结节的形成须接种适宜的细胞数量,用条件培养液培养细胞能促进钙化结节形成。

Results There were more mineralization nodes to form in shorter time in the 1×105/ml cell density group compared with in the 2×105/ml cell density group, but in the 5×105/ml cell density group, there were not, and with the DMEM medium contained β-glycerophosphate sodium and ascorbic acid, mineralization nodes formed more early compared with the DMEM medium.

结果 在培养30天内,条件培养液或常规培养液培养的5×105个/ml组细胞无结节形成;而2×105个/ml组和1×105个/ml组都有钙化结节形成,而且有细胞越少形成结节越早,数量越多的趋势;给予条件培养液又较常规培养液培养有结节形成早而多的趋势。

Combined with the regional data the research indicates that (1) the Tianmenshan main body formed in the Middle Jurassic Epoch, whereas the minor body was the further differentiated and evolutive product of the main body;(2) in the Chongyi-Dayu-Shangyou ore concentrated area, the west of Gannan area, the diagenetic age and metallogenic age are basically concordant, and the mineralization concentrated during 150~155 Ma;(3) from the middle-plutonic granite intrusion to the hypabyssal granite-porphyry vein, the magmatic activities experienced only 1~5Ma, indicating there was the concentrated period of mineralization.

结合区域资料,研究表明:①天门山岩体的主体形成于中侏罗世,补体是主体进一步分异演化的产物;②在赣南西部的崇余犹矿集区内成岩与成矿的年龄基本上是协调一致的,成矿集中期为150~155 Ma;③岩浆活动由中深成相花岗岩侵入体演化到浅成相花岗斑岩脉仅相差1~5Ma,表明存在成矿集中期。

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