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Calculated the lower limit of abnormal after the plane through the delineation of the contour map of the occurrence and analysis of abnormal findings were as follows: work area on the lithology in terms of more or less divided into two parts, East and West, the western area for the low-resistivity, lithology is metamorphic carbonaceous sandstone or slate, for the emperor in eastern areas, lithology for granite and granite porphyry, quartz vein occurrence in eastern and more, these quartz veins is into the eastern part of the resistivity of the form of alternating high and low.

计算了异常下限值后,通过圈定了平面等值线图上的矿点异常和其它分析得到结论如下:工区就岩性而言大致划分为东西两部分,西部为低阻区,岩性为变质砂岩或炭质板岩,东部为高祖区,岩性为花岗岩及花岗斑岩,东部多赋存石英脉,这些石英脉是的东部电阻率成高低交替的形式。

The Geza island arc zone is an important component part of the 3-river metallogenetic zone.

中甸格咱岛弧带是三江成矿带的重要组成部份,也是我国近年来寻找斑岩铜矿取得重大突破的矿集区之一。

Ice copper, blister copper; nickel-iron alloy; cobalt carbonate; crude lead, electrolytic lead; electrolytic copper,; high ice nickel; cobalt sulphate

德兴市科艺有色金属资源再生有限公司熔炼厂位于中国著名铜都——江西省德兴市,境内的德兴铜矿是亚洲最大的斑岩铜矿,金属矿藏铜、金、银等十分丰富,公司熔炼厂距铁路车站等运输车程均不足1小时,工厂比邻省道、国道、高速公路,交通非常便利。

And as they adopt the alternative of Porphyry, they conclude that the universals are nuda intellecta (that is, purely intellectual representations).

当他们通过替代的斑岩型,他们得出结论认为,共性是蘑intellecta。

The fine-grained crystalline base of porphyritic rock in which larger crystals are embedded.

基质斑岩中均匀的水晶质石基,其中嵌有大粒水晶

A conspicuous, usually large, crystal embedded in porphyritic igneous rock .

基质斑岩中均匀的水晶质石基,其中嵌有大粒水晶

The ore fluid has a temperature range of 150|300℃, probably derived from intermediate|acid albite porphyritic dikes, but not typically of magmatic hydrothermal origin. The ore fluid seems to be of multi|source.

成矿流体很可能来源于中酸性钠长斑岩脉,但又不是典型的岩浆热液,具有多成因性。

The calculation results are in accord with the distribution of the known deposits and show some new significant catchments.

经野外检查,发现普上和地苏嘎两处斑岩型铜矿的矿化新区。

The Zijinshan Copper Gold Deposit in Fujian Province is a high sulfur epithermal deposit discovered at first in China.

福建省上杭紫金山铜金矿床是我国大陆发现的首例高硫型浅成低温热液矿床,在矿床深部相继发现了斑岩型铜矿、中低温热液型铜矿和低硫浅成热液型银矿。

Through the ReOs dating of molybdenite from quartz porphyry, the isochron age of (222.5±3.2) Ma and the model age of (222.1±3.2) Ma~(224.6±3.4) Ma were obtained, which means molybdenite formed in late Triassic.

通过对含辉钼矿石英斑岩中采集的辉钼矿样品进行铼-锇同位素年龄测定,获得铼-锇等时线年龄为(222.5±3.2) Ma,模式年龄变化于(222.1±3.2) Ma~(224.6±3.4) Ma,表明辉钼矿形成时代为晚三叠世。

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In the negative and interrogative forms, of course, this is identical to the non-emphatic forms.

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