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沉积岩

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This section of eroded sedimentary rock on Elgol Beach on the Island of Skye, Scotland, mimics bone.

这个剖面的被侵蚀沉积岩在Elgol海滩在斯凯岛上,苏格兰,模仿骨骼。

This paper presents time temperature index method of judging hydrocarbon source condition by fluid inclusion in sedimentary rock.

本文探索性地运用沉积岩中包裹体测试数据计算烃源岩主要生烃时期的时间温度指数,对沉积盆地的烃源条件进行判别。

After comparing the model result with the record of prehistoric earthquakes along the Shanchiao fault and the depth of Tertiary basement, we suppose that the seismism of Shanchiao fault should have left-lateral slip portion and it was more active in the north fault section in the Taipei basin.

另外,我们将模拟的结果与古地震的错位记录和台北盆地第三纪沉积岩的基盘深度分布相比较,结果显示过去以来山脚断层的活动在台北盆地西北侧或更北方的断层面上有较大的滑移量,且具有左向滑移的分量。

Early thousands years ago, the probability of biological process of soda ash from sodium sulfate was revealed in Egyptian Wadi Naturn sediments. Every year the crude sesquioxide alkali crystallized and collected from the lakes was roughly the amount of the sulphate brought and reduced by the incoming river water.

早在几千年前的埃及Wadi Naturn沉积岩中便向人们揭示了芒硝生物制碱的可能性,每年从这些湖里结晶和采收的粗倍半碱与进水带入并产生还原的硫酸盐的量大致相当。

There are three main melting regimes in metasedimentary rocks:(1) melting at water-saturated solidus;(2) muscovite dehydration melting; and (3) biotite dehydration melting reactions.

变质沉积岩中的熔融作用主要有三种机制:饱和水固相线上的熔融、白云母脱水熔融和黑云母脱水熔融。

In this paper, we have studied the basin evolution stages from the aspects of sedimentary tectonics and sedimentary phase.

本研究从沉积构造和沉积岩相的角度对盆地演化的叠合特征进行了解析。

The feature of earth chemistry of volcanic rock in Xiangshan Group reflects that it belongs to the series of oceanic tholeiite in oceanic spreading tectonic environment.

结果 香山群的时代划归为中晚寒武世较合适;香山群主体是一套由板岩、细、粉砂岩和砂岩组成的浊积岩系,其砂岩类型主要是长石石英砂岩、细粒石英砂岩和粉砂质石英砂岩,前寒武纪变沉积岩和花岗片麻岩为主要碎屑来源和物源区组成;砂岩的岩石地球化学特征指示香山群属发育在被动大陆边缘斜坡环境中的沉积物,火山岩岩石地球化学特征反映其应属大洋扩张构造环境下的大洋拉斑玄武岩系列。

The greenstone belt is a typical volcanic-sedimentary formation formed by metabasic-acid volcanic rocks and partly metasedimentary rocks. The bimodal volcanic rocks are mainly tholeiite, which transforms upward into calc-alkali volcanic rock series.

绿岩带为典型的变质基性-酸性火山岩及部分变质沉积岩系构成的火山-沉积建造,火山岩以拉斑玄武岩为主,向上过渡为钙碱性火山岩系列,表现为双峰态型特点。

The protoliths of the chlorite-actinolite schist were mainly volcanic-sedimentary rocks enriched in basalt. The chlorite-actinolite schist and the altered pillowbasalt are characterized by high contents of TiO5, P2O5 and MgO, LREE-enriched patterns with negative Eu anomalies, and "tumescence" patterns for trace elements with enrichment in Nb, Ta and Ti; these are typical characteristics of "OIB-type" alkaline basalt.

绿泥阳起石片岩的原岩主要为富含玄武岩的火山-沉积岩系,绿泥阳起石片岩和蚀变枕状玄武岩具有TiO2、P2O5、MgO含量较高和LREE富集型、无Eu异常,以及"大隆起"微量元素配分模式和富集Nb、Ta、Ti元素等地球化学特征,显示为较典型的洋岛型碱性玄武岩性质。

The ultrabasic rocks form a complex of large tectonic slice s with intercalated slice s of Sebakwian sedimentary rocks.

超基性岩与塞巴奎沉积岩岩片相间构成一巨大的构造岩片的杂岩体。

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