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isochron相关的网络例句

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与 isochron 相关的网络例句 [注:此内容来源于网络,仅供参考]

Whole-rock Rb-Sr isochron age of 114Ma in Yanbei granite porphyry and single grained zircon U-Pb age of 138Ma in Tashan granite porphyry indicate that these two tin-bearing porphyry both are the products of Late Yenshan magmatic activity.

岩背花岗斑岩的全岩 Rb-Sr 等时线年龄(114Ma)和塌山花岗斑岩颗粒锆岩 U-Pb 年龄(138Ma)表明,这两个含锡花岗斑岩都是燕山晚期岩浆活动的产物。

It yields an Rb-Sr isochron age of 174.4Ma Ma (2σ), which is in accordance with their host granodiorite dated as 173.3±2.9 Ma by single-grained zircon U-Pb method.

黄铁矿Rb-Sr等时线年龄与花岗闪长岩体的单颗粒锆石U-Pb年龄十分一致,表明矿床的形成与岩体有密切的联系,花岗闪长岩体提供了矿床形成所需要的能量和部分流体,而地层也提供了部分成矿物质。

It is held that this isochron age may represent the metallogenic age of the Hetai gold deposit.

认为这一年龄值可能代表了河台金矿床的成矿年龄。

Based on the Re-Os isochron method of molybdenites, this paper measured directly the ore-forming age from skarn ore in the Huangshaping deposit, and got a Re-Os age of (153.8±4.8)Ma, which is in accordance with the previous K-Ar age of 153~157 Ma obtained from phlogopite in the ore-bearing skarn of the deposit.

文章采用高精度的辉钼矿Re-Os等时线定年法,直接测得硅卡岩型矿体的矿化年龄为(153.8±4.8)Ma,与前人获得的含矿硅卡岩中金云母的K-Ar年龄(153~157Ma)一致。

The syenite body inside the Tarim basin was first found during the study of magmatism inside the basin, and the isochron age of39Ar-40Ar is 277.7±l.3Ma, being equivalent to the Permian.

在研究塔里木盆地内部岩浆作用的过程中首次发现盆地内部正长岩岩体,其39Ar-40Ar年龄为277.7±l.3Ma,属于早二叠世。

U-Pb isotopic system of uraninite gives a mineralization age of 407 Ma ±, this is similar to the whole-rock isochron age of Rb-Sr.

通过铀铅同位素体系研究发现,矿化年龄在407Ma左右,与Rb-Sr全岩等时线年龄接近。

Both the lumpy albitite and the brecciated albitite have the same Rb-Sr isochron age of 364.9±10.9 Ma, indicating that the activity of the alkali fluids occurred in Devonian.

另外,还从这些钠长岩体中首次获得全岩铷-锶等时线年龄为364.9±10.9Ma的资料。对研究整个秦岭造山带钠质流体热事件具有十分重要的意义。

Auriferous quartz veins of Dongping gold deposit are dated by fluid inclusion Rb-Sr isochron methed at 103±4Ma.

用石英流体包裹体Rb-Sr等时线法测得东坪金矿床含金石英脉的年龄为103±4Ma,比该矿的蚀变岩型矿体晚50-70Ma。

The Sm-Nd isochron age (1182±50Ma) of Kangshan metamorphic complex has first been presented in the paper, which deny the tranditional point that the complex is Archean Taihua group. It's suggested that the plagioclase-amphibolite originates from subcon tinantal lithospheric mantal, assimilating and hybridizing minor crustal materials.

首次提供康山变质杂岩的Sm-Nd等时线年龄(1182±50Ma),否定了康山变质杂岩是太华群的传统认识,并提出康山变质杂岩内斜长角闪岩原岩主要来源于大陆岩石圈地幔,同化混染了少量壳内物质。

The study on secondary isochron of anomalous lead is a very important problem in the common lead isotope geology.

异常铅二次等时线是普通铅同位素地质学研究中非常重要的一个课题。

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