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zircons相关的网络例句

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The CL characteristics and the ratio of ~ 232 Th/~ 238 U of zircons reveal that the former is formation age of amphibolite,and the later is its metamorphic age.

锆石CL图像和放射性同位素地球化学特征显示前者为岩浆结晶年龄,后者为构造-热事件年龄。

These zircons have nearly the same ~(204)Pb -corrected ~(207)Pb/~(206)Pb ages, with weighted mean age of ca 2.5Ga, interpreted as forming or anatexis age of protolith of the rutile ores.

这两期锆石的~(204)Pb校正的~(207)Pb/~(206)Pb年龄值几乎一致,加权平均值位于2.5Ga左右,可解释为金红石矿石的原岩形成年龄或者深熔年龄。

LA-ICPMS U-Pb Dating of Zircons from Two Types of Leucosomes in North Dabie Unit: Evidences for Paleoproterozoic Anatexis and Triassic Subduction?

篇名 北大别两类浅色体的锆石LA-ICPMS年龄-古元古代深熔作用和三叠纪俯冲证据?

According to the isotopic age data of inherited zircons in igneous and metamorphic rocks which occur at the surface and are derived from deep crust of the North China, Yangtze blocks and Qinling-Dabie orogenic belt, the paper is mainly reports some new information of Archean rocks and briefly discusses its geological significance.

本文根据华北和扬子陆块及秦岭大别造山带地表和深部出露的各种岩石中发现的继承性锆石的测年数据,报道了太古宙基底和岩浆事件的新信息,并简要地论述其地质意义。

The result is indistinguishable, within analytical uncertainties, from U-Pb ages of baddeleyite and zircons obtained by previous workers, suggesting that a rock-and ore-forming event did occur in Neoproterozoic in Jinchuan.

此结果也与前人报道的锆石和斜锆石的U-Pb年龄在误差范围内一致,说明了金川的新元古代成矿时代。

In the Cathodoluminescence images the zircons extracted from the dioritic gneiss show good crystal morphology and clear oscillatory zoning, as is the case of magmatic zircon.

在阴极发光图像中,片麻岩中的锆石具有较好的晶形,并显示出清晰的岩浆锆石韵律环带结构。

The Mesozoic volcanic rocks are mainly located in Huoshiling Formation and Yingcheng Formation. The former consists of basaltic andesite, trachyandesite and dacite, the latter is composed of basaltic trachyandesite, trachyandesite and rhyolite. The cathodoluminesence images and high Th/U ratios of the zircons suggest their magmatic origin.

松辽盆地南部中生代含火山岩地层主要包括火石岭组和营城组,其中火石岭组火山岩由玄武安山岩-粗安岩-粗面英安岩组成,营城组火山岩由玄武质粗面安山岩-粗面安山岩-流纹岩组成。

The LREE enrichment may partly be caused by the presence of microscale LREE-bearing mineral inclusions (such as apatite, monazite or epidote) in the zircons.

对于具有普遍提高的LREE、Th、U、HREE和HFSE含量的海绵状变质锆石,不可能仅仅与常见的热液流体有关。

This implies a major stage of crustal growth in Proterozoic time and remelting of the crustal material in Early Jurassic time;(5) The Oligocene-Miocene adakites contain magmatic zircons that show similar Hf isotope compositions to the Cretaceous-Paleogene Gangdese batholiths, providing a key constraint that allows evaluation of the nature and timing of crustal thickening in southern Tibet owing to the India-Asia collision; and (6) As a whole, the Hf isotope information observed in zircons from the above Transhimalayan rocks demonstrates a temporal variation in εHf values, and thus TDMC ages, that suggests multiple stages of orogenic or crustal formation events.

五、渐新世、中新世的埃达克岩,其岩浆锆石的铪同位素特徵与白垩纪、古第三纪冈底斯岩浆相似,因而为藏南在印亚碰撞以后,地壳增厚的时间与机制提供了关键性的制约;六、综观上述藏南火成岩中的锆石,它们与时变化的铪同位素初始值及其对应的模式年龄记录了拉萨地块多阶段的造山与地壳形成历史。

Combined with previous studies, we suggest that the 1100-2200 Ma zircons perhaps originate from the China North Craton, while the zircons of 520 Ma may stem from Jiamusi massif.

根据目前有关年代学研究成果,推断1100~2200 Ma碎屑锆石可能来源于华北克拉通,而样品中的520 Ma的碎屑锆石则可能来源于佳木斯地块。

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