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1)  Xiangshan orefield
相山矿田
1.
Metallogenic physica-chemical conditions analysis of Julong′an uranium deoposit in Xiangshan Orefield;
相山矿田居隆庵铀矿床成矿物理化学条件分析
2)  Xiangshan ore field
相山矿田
1.
F2 in Quaternary led to the subsidence of the northwestern part relative to the southeastern part in the Xiangshan ore field, forming two special image areas, namely the southeastern image area a.
通过Landsat 7 ETM+多光谱数字图像融合,对相山矿田的地表岩性、地貌景观及线环影像进行分析,共解译出NE向、NNW向、NWW向、SN向和EW向5组线性构造,这些线性构造具有多期次活动的特点,其中NE向线性构造F2在第四纪的活动,使相山矿田北西部相对于南东部陷落,形成北西、南东两个各具特色的影像区,南东影像区剥蚀程度较大,北西影像区更适合找矿。
3)  Xiangshan uranium orefield
相山铀矿田
1.
Phases of metamorphism in the metamorphic base of Xiangshan uranium orefield;
相山铀矿田变质基底的变质作用期次
2.
Comparative analysis of geological information between the northwest part and southeast part in Xiangshan uranium orefield;
相山铀矿田西北部与东南部地学信息对比研究
3.
The Xiangshan uranium orefield in Jiangxi Province is the largest volcanogenic hydrothermal uranium orefield in China.
相山铀矿田广泛发育热液水云母化 ,且水云母以伊利石、蒙皂石混层矿物居多。
4)  Xiangshan uranium ore-field
相山铀矿田
1.
Studies of petrology and elemental geochemistry indicate that the Xiangshan uranium ore-field dacite porphyry belongs to intra-plate shoshonitic rock type and is a kind of shoshonitic dacite porphyry.
岩石学、元素地球化学研究表明,相山铀矿田的英安斑岩属于板内型钾玄质岩类,为钾玄质英安斑岩。
5)  Xiangshan uranium ore field
相山铀矿田
1.
The results indicate that there are two uranium mineralization phases in Xiangshan uranium ore field,The first phase of mineralization (uranium haematite) took place at 115±0 6 Ma associated with the volcanic collapse and the intrusion of subvolcanic magma.
本文重点研究了相山铀矿田的成矿时代及成矿环境 ,并剖析了典型矿床在垂向上物质成份的变化规律。
6)  Xiangshan Uranium ore fieled
铀矿田相山
补充资料:山相
1.见"山中宰相"。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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