火山作用的

Lightning and firestorms from falling walls of flaming petrochemicals, formed during the interaction of gasses with volcanic heat and continuous lightning, cannot be predicted.

着火的石油化学物质形成了闪电和火风暴大片地掉落下来：它们是在气体与火山热度，以及持续的闪电的交互作用下形成的，且是不可预测的。

And that the timing of subduction of the paleo-ocean basin represented by the Guanzizhen ophiolite and formation of the volcanic-magmatic island arc is Late Cambrian to Early Ordovician.

反映以关子镇蛇绿岩为代表的古洋盆的俯冲作用和形成火山-岩浆岛弧的时限可能为晚寒武世或稍早。

She did not dream of the volcanic convulsions of love, its scorching heat and sterile wastes of parch ed ashes

她从未梦想过火山爆发大地抽搐式的爱情，从未想到过它的熊熊烈焰，它的破坏作用，它能烧成一片片焦土。

That seriously affect the quality of the latter, which is formed as a result of geological vicissitudes including diastrophic movement, eruption of volcano, sedimentation, glaciation and weathering etc.

没有什么比矿石中本身固有的杂质更影响成品的品质，杂质是包括地壳运动，火山喷发，沉淀，冰川和风化作用等的地质变迁而导致形成的。

It is nothing else than impurities prenatally inherent in ore that seriously affect the quality of the latter, which is formed as a result of geological vicissitudes including diastrophic movement, eruption of volcano, sedimentation, glaciation and weathering etc

矿石是随着诸如地壳运动，火山喷发，沉淀、冰河以及风化作用等地质运动而形成的。然而，对于矿石本身影响最严重的莫过于其本身所含有的杂质。

Combined with available data, it is comidered that the sourcerock of biotite--leptynite might be intermediate-acid volcanic material of ca.2.7 Ga, and that of migmatized leptite and quartzite might come from granitic crust older than 3.0 Ga. The iron formation was formed on the continental crust base at about 2.7 Ga, and was immediately metamorphosed for the first time.

结合已有的研究资料可以认为，黑云变粒岩的原岩来自2.7 Ga左右的中酸性火山物质，浅粒岩和石英岩的原岩来自3.0 Ga以上的花岗质地壳物质；含铁建造形成于陆壳基底之上，形成时间约2.7 Ga，并于2.5—2.7 Ga之间发生首次变质作用。

We analyzed the tectonic differences and deep geodynamic characteristics based on the tomographic results, which show high velocity anomalies at the uppermost mantle beneath the northeast SCS, and depict the lithospheric mantle extension from South China continent to marginal sea. Because of the low temperature and thick lithosphere beneath the northeast SCS, it seems no magma intruded from mantle, so we inferred that the rift may only occur in the crust rather than extend to the upper mantle, which shows the nature of nonvolcanic continental margin.

结果表明：南海东北部表现出陆架地区的岩石层特性，属于华南大陆向海区的延伸，岩石层厚度较大，现今不存在大规模的地幔热流活动，推测大陆边缘张裂作用仅限于地壳内部而没有延伸进入上地幔，具有非火山型大陆边缘的深部特点。

When the shockwave energy weakened, mountain collapse often occurs in the ringed mountain, particularly in the previously steeper inside, while plagioclase slope slide (primary meteorite-stricken slope slide) occurs in the outside mountain, and the mountain structure is constantly adjusted in aftershocks to achieve the gravity balance; during the long geological ages after the formation of meteorite crater, under the action of erosive transit and dryness and humidity of hydrosphere and air current, volcano and earthquake activities, etc., the physiognomy gradually reverts to the original state.

在冲击波能量减弱时，环形山原来较陡峭的内侧多发生山体崩塌，外侧山体发生斜岩滑坡，在余震中山体构造不断调整以达到重力平衡；在漫长的地质年代里，陨击坑成型以后，在水圈、大气环流的侵蚀搬运、寒暑燥湿、火山和地震等因素作用下地貌逐步趋于还原。

When the shockwave weakened, landslides often occurs in the ringed mountain, particularly in the previously steeper inside, while plagioclase avalanche (primary meteorite strike landslide) occurs in the outside mountain, and the mountain structure is constantly adjusted in aftershocks to achieve the gravity balance; after the formation of meteorite crater, during the long geological ages, under the action of hydrosphere, erosive transit and dryness and humidity of air current, volcano and earthquake activities, etc., the landform gradually reverts and returns to the original state.

在冲击波能量减弱时，环形山原来较陡峭的内侧多发生山体崩塌，外侧山体发生斜岩滑坡，在余震中山体构造不断调整以达到重力平衡；在漫长的地质年代里，陨击坑成型以后，在水圈、大气环流的侵蚀搬运、寒暑燥湿、火山和地震等因素作用下地貌逐步趋于还原。

Geochemical characteristics indicate S-type granites and volcanic rocks depleted in sodium and enriched in potassium, with 62.42%～78.02% w(SiO2), 7.66%～9.13% w(K2O+Na2O), 1.18～2.62 w(K2O)/w(Na2O), and Rittmann index δ of 1.67～3.78. They are enriched in LREE with an average LREE/HREE ratio of 10.94×10-6, and generally depleted Eu with an minimum δEu less than 0.31 especially in the ignimbrite and biotite granite, which have experienced a significant process of separation and crystallization of plagioclases.ΣREE at the main stage of the magmatic activity decreases with time.

地球化学特征显示矿区火山——侵入岩属于贫钠富钾的S型花岗岩，其w(SiO2)值为62.42%～78.02%、w(K2O +Na2O)值为7.66%～9.13%、w(K2O)/w(Na2O)比值为1.18～2.62、里特曼指数δ为1.67～3.78；矿区岩石LREE/HREE比值平均为10.94×10-6，属于轻稀土富集型；Eu普遍亏损，特别是熔结凝灰岩、黑云母花岗岩δEu＜0.31，表明经历了显著的斜长石的分离结晶作用；自早至晚主阶段岩浆活动稀土总量逐渐降低。

But we don't care about Battlegrounds.

但我们并不在乎沙场中的显露。

Ah! don't mention it, the butcher's shop is a horror.

啊！不用提了。提到肉，真是糟透了。