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volcanic bomb相关的网络例句

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与 volcanic bomb 相关的网络例句 [注:此内容来源于网络,仅供参考]

The theme of volcanic presented by Li Gang has the character of multiple powerful perception, not only the quiet state of brewing but also the unrest after breaking out, even the floweriness after the volcanic congealed.

李岗的火山主题具有着多重的力量感,既有酝酿积蓄的沉静状态,也有爆发后所袒露出来的动荡、肆虐,还有火山凝固后幻化出的绚烂与奇屈。

One is a bimodal volcanic assemblage, which formed during the rifting stage of the continental breakup theother is represented by flysch rocks, formed when the passive margin becomes stable. The composition of mafic rocks in the volcanic margin reflect their mantle origin and their crustal contamination. High temperature and low-pressure metamorphism can occur during the rifting stage and reflects a temporal trend of increasing temperature and decreasing pressure during the continental breakup.

被动陆缘的沉积建造由两套沉积物组成,一套是大陆解体的裂谷阶段所形成的陆相沉积物和双模式火山岩组合,另一套是稳定陆缘的复理石组合;岩装作用中基性岩类反应了物质直接源于上地慢的主要特点,并有部分受到地壳混染的特征;变质作用中高温低压环境主要发生在裂谷作用阶段,其特点反映了大陆解体过程中随着时间的增温和减压过程,而拆离伸展阶段则被脆性变形所代替。

Meanwhile, they show high abundances of Sr and Ba and high Sr/Y and La/Yb. The volcanic rocks have varied and enriched Nd isotopic compositions ε(subscript Nd=-11~-17, which plot intermediately between the field of the ancient continental crust and the field of the enriched subcontinental lithospheric mantle. These geochemical signatures indicate that the volcanic rocks of the Tiaojishan and Donglingtai Formations were originated from a process of hybridization between the enriched mantle-derived mafic magma and the lower continental crust.

火山岩的钕同位素成分变化大,且相当富集ε(下标 Nd=-11~-17,都分布在古老下地壳和富集地幔之间,因此推断北京西山地区髫髻山组火山岩和东岭台组火山岩的形成与富集地幔起源的基性岩浆与古老下地壳组分相互作用有关。

Rare samples of mother rock 'kimberlite', from Siberia, South Africa and Australia, displayed as an introduction to the geological section of the museum,- how diamonds originate from a volcanic magma, formed in the earth's mantle, 100 - 200 km below the earth's surface, and are transported through volcanic pipes to the earth's surface.

陈列了来自西伯利亚、南非和澳大利亚的罕见的金伯利岩样本。通过对它们的地质解理面的介绍,来说明钻石在火山岩浆中的形成过程,即钻石是在100~200公里的地幔中形成,随着火山爆发被喷射到地球表面。一个显示全世界钻石产量的模型(0.4立方米大小)是博物馆的精粹,就这0.4立方米的钻石,养活着全球200多万钻石业人。

The lateral variation in Tengchong volcanic area is larger than that in Wudalianchi volcanic area.

腾冲火山区的横向速度结构变化比五大连池火山区更为显著。

Silicalites, predominated by pelitic silicalite, occur in collisional zones and back-arc basins. In the collisional zones, they occur as rock sheet as an important part ofophiolitic mé lange, belonging to ophiolitic mélange type silicalite. In the back-arc or interarc basin, they occur as pelitic silicalite intercalation varying in thickness, characteristic of "silica merl",and belonging to abyssal back-arc basin type or carbonate type silicalite. In the magmatic arc, they occur as intercalation related to volcanic hydrotherm or volcalic exhalation, belonging to volcanic arc type silicalite.

在硅质岩方面:冈底斯构造带侏罗系硅质岩主要属泥质硅质岩,在各个碰撞结合带和弧后盆地中均有产出,主要的产出状态有:①在碰撞结合带中呈岩块产出,构成蛇绿混杂岩的重要组成部分,属蛇绿混杂岩型硅质岩;②在弧后或弧间盆地中呈厚度不等的泥质硅质岩夹层产出,常具"硅灰泥"特征,属弧后深水盆地型硅质岩;③呈夹层状产于弧火山岩系中,属火山热液或火山喷气型硅质岩。

Based on field work in fourteen typical ore districts of China, the author made experiments on contact metasomatism of ultrabasic-acid intrusive rocks with carbonate rocks, interaction between volcanic pneumatolyto-hydrothermal solution and volcanic rocks, and metasomatism in the process of sedimentary metamorphism and migmatizatiun.

本文作者在全国14个典型矿区的野外工作基础上,进行了超基性-酸性侵入岩与碳酸盐岩的接触交代实验;火山气热液与火山岩的相互交代实验;区域沉积变质和混合岩化过程中的交代作用实验。

The raw and processed materials of AD brand cosmetic give priority to Caucasian volcanic mud and volcanic cold mineral spring of Russia.

AD品牌化妆品的原材料主要以俄罗斯高加索火山泥和火山冷矿泉为主。

Moho in Tengchong volcanic area is deeper than that of Wudalianchi volcanic area.

腾冲火山区的莫霍界面与五大连池火山区的莫霍界面的埋藏深度有一定的差异,壳幔界限不十分清楚。

Northeastwards younging of rocks along the northern coast suggests a gradual migration of the volcanic centers in King George Island, which correspond to the regularly distributed time space pattern of the volcanic activities on the South Shetland Islands.

岩石的年龄由南西向北东依次变新,表明乔治王岛的火山活动中心在不断迁移,与整个南设得兰群岛火山岩的时、空分布规律相符。

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