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The contact - metasomatic iron deposit, which emerges between intermediate - acid magmatic rock and carbonate rock, is controlled by geologic structure.

产于中酸性岩浆岩与碳酸盐岩接触带的接触交代型铁矿,受地质构造条件的控制,在安林地区形成了两条成矿带,包含8个矿田。

The main characteristics of the skarn are as follows:(1)occurring as bedded,para-bedded in the contact zone between carbonate and microclastic rock,and its occurrence being accordance to the strata;(2)cut by later vein rock,so having no relation with the magmatic rock on genesis;(3)metasomatic skarn having replacement remnant texture,pseudobreccia structure,while depositional skarn,particulate crystall...

研究表明该夕卡岩的主要特征为:(1)呈层状、似层状赋存于碳酸盐岩和细碎屑岩接触带,产状与地层一致;(2 )被后期脉岩穿切,成因上与岩浆岩无关;(3)喷流交代夕卡岩具交代残余结构和假角砾状构造,而喷流沉积夕卡岩具微粒状结构、雏晶结构和层纹、条纹、条带状构造,反映了二者不同的喷流成因;(4)发育典型的低温夕卡岩矿物组合,其形成温度小于30 0℃;(5 )夕卡岩的稀土配分型式与围岩的一致。

According to the lithologic correlation,the feature of basic sequence,fossil assemblages and isotope assaying ,mass formation within Hercynian period in Hongliuhe area is composed of Hongliuhe Group made up of detrial and volcanic rocks of marine facies , carbonate and continental molasse.

据岩石组合、基本层序特征,结合生物化石鉴定和同位素测年结果,红柳河地区海西期物质建造由红柳河群海相碎屑岩、碳酸盐岩、火山岩建造和陆相磨拉石建造组成,主期变形形成主干褶皱———红柳河向斜及伴生构造,变形机制为纵弯褶皱作用兼具一定压扁特点,总挤压收缩率达 40 %~ 70 %,反映了造山后强烈陆内收缩变形特点。

Introduce the numerical well test and reservoir model combination function into the study, realized the efficient description of the seep cell dynamic percolation model of slot and hole type carbonatite reservoir, such as "moniliform","compound" and so on.

本文针对塔河缝洞型碳酸盐岩油藏特殊的储层、油藏地质特征,以及现行解析试井解释方法在缝洞型油藏试井资料解释中面临的主要问题,开展了有限元数值试井新技术应用研究。

So the seismic facies analysis method was used to classify the seismic facies of the igneous rock. The result shows that the igneous rock is characterized by slabby, bow, mushroom and moundy in profiles.

在英买力地区,火成岩与碳酸盐岩为共生状态,两种地层的速度十分接近,用常规速度分析方法难以将它们区分。

In Phanerozoic neritic carbonate environments, syndepositional dissolution proceeded at least largely independent from aragonite seas or calcite seas, and appears mainly controlled by site-related factors.

在显生宙浅水碳酸盐环境中,同沉积溶解作用独立于文石海和方解石海,主要有局部环境控制(site-related factors)。

Geochemical characteristics of 36 Tertiary mudstone samples from Kuqa depression show that the content of CaO is very high, which can somewhat dilute other major elements, trace elements and rare elements. Some reliable indicators for provenance analysis show the source rock nature of noncarbonate sediments. The REE distribution pattern is similar to that of the upper continental crust, characterized by enrichment of LREE and negative Eu anomalies. Some trace element ratios show that the source rocks are mainly felsic.

对库车坳陷第三系36件泥岩样品的地球化学特征分析表明,主量元素中CaO的含量很高,对其他主量元素以及微量和稀土元素有稀释作用,一些可靠的物源分析指标主要指示了非碳酸盐沉积物的源区性质;REE分布模式与上地壳相似,轻稀土元素富集,Eu负异常,微量元素比值显示源岩以长英质岩石为主。

This section includes the nonindustrial preparation, purication, and reactions of inoganic substances:elements; inorganic acids, bases, and salts; synthetic minerals; inclusion compounds;charge-transfer complexes; coordination compounds containing inoganic and organic ligands;nonmetal and metalloid compounds; and carbon-containing compounds such as the carbon oxides, metal carbonyls, carbonates and transition metal carbonxylates.

这一章节涵盖了无机物的非工业制备、提纯、及反应:元素;无机酸、基团和盐类;合成矿物质;包藏复合物;转移电荷复合物;包含了无机和有机配合基的配位化合物;非金属与非金属化合物;以及含碳化合物,如碳氧化物、金属羰基、碳酸盐和含有羰基的过渡金属等。

The method was applied to extract gravity and magnetic data in some carbonate area; then Parker Oldenburg method was used in every polygon to inverse base depth of every unit t finally the basement interface of the whole area was obtained through splicing.

应用该方法,对某碳酸盐岩地区的重磁数据进行了多边形分区提取;然后在每个多边形内应用Parker-Oldenburg法反演出各单元的基底深度;最后通过拼接,获得了丰富个区域的基底界面。

Many methods for sample preparation have been applied in stable isotope measurements of ostracode shells from lake sediments.

在总结目前常用的湖泊生物碳酸盐稳定同位素测试样品处理方法的基础上,通过对青海湖现代和古代沉积物中介形虫的测定,讨论各种处理方法对介形虫壳体稳定同位素测试结果(δ13C和δ18O)的影响。

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