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basalt相关的网络例句

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与 basalt 相关的网络例句 [注:此内容来源于网络,仅供参考]

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 peak metamorphic minerals are garnet, omphacite,phengite and rutile with temperature of~500℃,pressure of~2.3Gpa.On the basis of geochemical analysis,the content of SiO2 in the eclogite ranges from 46.68%to 50.24%,Na2O+K2O 3.10~4.21%,and high REE with enriched LREE, LREE/HREE of 2.83~6.06.The REE pattern and trace element spidergram are similar with those of ocean island basalt,according with the blueschist from Longmucuo -Shuanghu suture zone.The protolith of the eclogite and blueschist are OIB,and they aremaybe the result of subduction of Permian OIB in central Qiangtang area.

对棉辉岩的地球化学分析显示,榴辉岩SiO_2含量在46.68—50.24%之间,Na_2O+K_2O含量在3.10—4.21%之间,稀土元素总量较高,轻稀土富集,重稀土相对亏损,LREE/HREE比值在2.83—6.06之间,稀土元素球粒陨石标准化曲线呈向右倾斜的样式,微量元素原始地幔标准化蛛网图OIB类似,这些特征和龙木错—双湖高压变质带的蓝片岩类似,它们的原岩为均为洋岛型玄武岩,形成环境类似于现在太平洋中的夏威夷,榴辉岩、蓝片岩很可能是羌塘中部地区出露的二叠纪洋岛型岩石俯冲消减的产物。

Towards the east a layer of pleistocenic basalt rests on top of the limestone and about 100 m below the plain that forms the summit there runs a vein of flintstone.

这座山的西边是石灰岩层,其下层是黏土层,在南边和东边是neocenich,接近东边的是pleistocenic 玄武岩层,其余的上面则是石灰岩,以及在像山峰的旷野形状底下约有100公尺的燧石的矿脉。

Towards the east a layer of pleistocenic basalt rests on top of the limestone andabout 100 m below the plain that forms the summit there runs a vein of flintstone.

这座山的西边是石灰岩层,其下层是黏土层,在南边和东边是neocenich,接近东边的是pleistocenic 玄武岩层,其余的上面则是石灰岩,以及在像山峰的旷野形状底下约有100公尺的燧石的矿脉。

There are three genetic types of mineral deposits in the Beiya ore district:① Cu-Au polymetallic deposits related to alkaline porphyries, comprising porphyritic Cu-Au deposits and polymetallic skarn deposits related to quartz-albite porphyry and quartz-K-feldspar porphyry;② Fe-Au deposits related to gabbro or basalt magma, consisting of magmatic Fe-Au deposits and sedimentary polymetallic deposits formed in caves and lakes; and ③ palaeo-placers formed at the weathering surface, in lakes and in karsts.

北衙金矿有3种成因不同的矿床:①与碱性斑岩有关的铜金多金属矿,包括与石英钠长斑岩和石英正长斑岩有关的斑岩型铜金矿床和矽卡岩型多金属矿床;②与辉长-玄武岩浆有关的铁金矿床,包括熔浆型铁金矿床和喷流沉积型多金属矿床,后者又有洞穴和湖相沉积环境之分;及③古砂矿,有古风化壳型砂矿、河湖相古砂矿和洞穴沉积古砂矿。

The two early Carboniferous fragments are composed of Basalt and ash-black, fuchsia radiolaria silicalite, siliceous mudstone, tuff .

早石炭世两个断片由玄武岩和灰白色、紫红色放射虫硅质岩、硅质泥岩、凝灰岩组成。

It is inferred that the Cretaceous rhyolitic rocks developed widely in Zhejiang Province probably originated by partial melting of the basement metamorphic rocks. Continuous underplating of basalt resulted in significant increase of introduced mantle-derived materials with time.

推测浙江省广泛发育的白垩纪流纹质火山岩可能是基底变质岩部分熔融形成,由于持续的玄武岩底侵作用,造成幔源物质的加入量显著地随时间增加。

The volcanic rock research of Yixian Formation shows that Yixian Formation during the Early Cretaceous( 135 - 120Ma ) is mainly composed by basalt and sanukite which are non adakite.

义县组火山岩的研究表明,早白垩世(135~120 Ma)的义县组主要由玄武岩和赞岐岩组成,并非埃达克岩。

Geological and geochemical characteristics of the Early Ordovician volcanic rocks from North Qilian Mountain show that they are of the basalt-andesite association with no acid rocks or volcanic rocks of the shoshonite series.

早奥陶世阴沟群火山岩的地质-地球化学特征的研究结果表明,该期火山岩的岩石组合为玄武岩-安山岩组合,缺乏酸性火山岩和橄榄玄粗岩系列火山岩。

Studies of petrology and petrochemistry indicate that such suit of volcanic rocks dominated by lattite belongs to shoshonite series to potassic alkali basalt series. Considering the stability of rocks and their associations, gentle stratum occurrence, fresh degree of rocks and comparatively clarity of horizons. this potassic volcanic stratum distributed over the Sailipu area is named as Sailipu Formation, and the age of which is early middle Pleistocene of Quaternary.

岩石学、岩石化学研究表明,这套火山岩是以安粗质熔岩为主的钾玄岩系列-钾质碱性玄武岩系列火山岩,岩石类型及岩石组合稳定,岩层产状平缓,岩石新鲜,层位相对清楚,故将其命名为赛利普组,属第四纪早-中更新世。

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