玄武岩的

I read Claus Sendlinger's editorial in Choupana Hills, a Design Hotel in Madeira that makes no special claim to greenness, though its light bulbs are low-energy, its toiletries come in recycled packaging and its decor involves products from the island: basalt and wickerwork from the nearby village of Camacha, one of the many local industries tangentially dependent on tourism.

森德林格的一篇社评Choupana Hills酒店是Design Hotels酒店在马德拉群岛的成员酒店，并没有刻意标榜绿色环保，尽管安装有低能耗照明灯，卫生用品使用的是再循环包装，装饰材料产品也都来自岛上：玄武岩制品和柳条制品来自附近的Camacha村当地许多行业都多少要依赖旅游业

I read Claus Sendlingers editorial in Choupana Hills, a Design Hotel in Madeira that makes no special claim to greenness, though its light bulbs are low-energy, its toiletries come in recycled packaging and its decor involves products from the island: basalt and wickerwork from the nearby village of Camacha, one of the many local industries tangentially dependent on tourism.

我曾在Choupana Hills读过克劳斯·森德林格的一篇社评。Choupana Hills酒店是Design Hotels酒店在马德拉群岛的成员酒店，并没有刻意标榜绿色环保，尽管安装有低能耗照明灯，卫生用品使用的是再循环包装，装饰材料产品也都来自岛上：玄武岩制品和柳条制品来自附近的Camacha村。当地许多行业都多少要依赖旅游业。

The sharp difference suggests that they have different origins: the former comes from allochthonous sapropel-type organisms of the lower strata and is the remains of crude oil, and the latter is autochthonous humic-type organic matter of sedimentary rocks between the basalt layers.

玄武岩中铜矿石沥青的δ13CV-PDB为-27.3‰～-33.2‰，平均-31.97‰，沉积岩中铜矿石碳质的δ13Cv-PDB为-20.2‰～-23.2‰，平均-22.11‰，表明二者无明显成因联系，前者属腐泥型，为石油的遗迹，来自下部地层；后者为腐植型，来自原地沉积的陆生高等植物。

An interbedded sliding zone with fault-slip cleavage in an amygdaloidal basalt thin layer made up the embryo of the main sliding zone and the coupling chemical weathering with physical weathering based on lateral unloading made the interbedded sliding zone get a material prone to slide finally.

褶皱运动产生的构造裂隙与柱状节理的叠加使滑体玄武岩呈现碎裂—镶嵌结构，而沿结构面发生的化学风化形成的腐岩壳使岩体进一步转变为&石夹土&结构，加剧了坡体的时效变形。

The Tertiary basaltic rocks are discontiously distributed from the west to the northeast of Sudan, in the Sahara Desert, overlying the Cretaceous clastic rocks. The authors of this paper found a kind of columnar jointing in the Cretaceous clastic rocks in the Mellit area, western Sudan.

笔者在苏丹西部Mellit地区白垩系碎屑岩中发现一种罕见的柱状节理，经研究认为是沉积岩层受到中新世喷发的玄武岩熔岩流的烘烤而失水收缩形成的。

The actual chemical make-up of rocks is complex, so the conventions of petrological analysis pretend that these metals are present in basalt as their oxides.

然而构成这种岩石的化学元素十分的复杂，因此根据常规的岩石分析得出出现在玄武岩里的金属都是其氧化产物。

The plan is that instead of being released, the gas will be redissolved in cooler water and injected to a depth of up to 800 metres, into suitable basalt formations where, the hope is, it will react to form calcite or dolomite.

这次实验的目标就是将这些原本被释放二氧化碳溶解到冷却的水中，然后注入到800米以下的玄武岩层，并希望通过一系列的反应将玄武岩变成方解石和白云石。

The SiO2 content of the dike swarms varies from 50.22% to 61.10% and they are basic-intermediate rock series, mainly basic. The Al2O3 content is generally higher than 15% and they are high aluminum basaltic rocks. The lower magnesium index (Mg#=42.77~62.28) and TiO2 content (0.97~2.41%) illuminate that they suffered magnesium-iron minerals' fractional crystallization and that they did not crystallize from original basaltic magma. The values of Na2O/K2O are all above 1, indicating lower K character. Chemically discriminated, these dike swarms are sub-alkaline rock series.

岩墙群的SiO2含量为50.22~61.10%，属于基性和中基性岩类，以基性为主；它们的A12O3含量普遍高于15%，属高铝玄武岩类；具有较低的镁指数（Mg#=42.77~62.28）及TiO2含量（0.97~2.41%），说明它们经历了镁铁质矿物的结晶分异作用，也指示它们不是由原始玄武岩浆结晶；Na2O/K2O都大于1，显示出低钾的特点；岩石化学判别，岩墙群岩石属亚碱性系列。

Based on the field investigation,laboratory experiment and data processing,the basalts are regard as the source rock of ore.

通过野外实地考察、室内实验及资料的分析研究，认为玄武岩在表生水的循环作用下可以带出多种成矿元素而成为矿源体，并在不同的古地理环境条件下形成不同类型的矿床。

It may indicate that the Martian mantle is wetter than Earth's or that younger lavas melted at different temperatures or pressures than the older basalts.

或许代表火星的地函比地球的更潮湿，或是较年轻的熔岩与较古老的玄武岩是各在不同的温度或压力下熔化。

In the United States, chronic alcoholism and hepatitis C are the most common ones.

在美国，慢性酒精中毒，肝炎是最常见的。

If you have any questions, you can contact me anytime.

如果有任何问题，你可以随时联系我。