- 更多网络例句与拉斑玄武岩相关的网络例句 [注：此内容来源于网络，仅供参考]
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The former petrochemical and geochemical characteristics show that it is similar to island are tholeiitic rocks and andesite. It is comparable with the geochemical pattern of the typical island arc basalt in the world, indicating thatisland arc environment is dominnant in the diagenetic process.
其中前者岩石化学、地球化学特征表明，具类似于岛弧拉斑玄武岩及安山岩的特点，并与世界典型的岛弧玄武岩地球化学型式具可比性，反映出岩石在成岩过程中具育相当于岛弧环境为主的演化趋势。
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On the basis of the study on the petrology, Trace element, and isotopic geochemistry, the primary magma of volcanic rocks can be divided into two series according to their originated rocks and degree of partial melting. One is the basanite-alkaline basalt-Olivine tholeiite magma series, which are generated by partial melting from spinel Iherzolite; the other is nephelinite magma-alkaline picritic basalt magma, which are generated by partial melting of the garnet Iherzolite.
岩石化学、微量元素、同位素地球化学证据都表明，华北、华南地区的火山岩根据源岩和局部熔融程度的不同，可以分为两个原生岩浆系列：一个是源岩为尖晶石二辉橄榄岩，随着局部熔融程度的增加，形成的碧玄岩岩浆-碱性玄武岩岩浆-橄榄拉斑玄武岩岩浆；另一个是源岩为石榴石二辉橄榄岩，随着局部熔融程度的增加形成的霞石岩岩浆-碱性苦橄玄武岩系列。
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In this paper, the petrology, mineralogy and geochemistry of basic-ultrabasic volcanic rock, granite and skarn related to the Sn-Cu skarn-type ore and the vein-type ore in Laochang ore field have been researched systematically, some conclusions are summarized as follows:In Gejiu tin-polymetallic district, the middle Triassic volcanic rocks belonging to calc-alkaline basalt-tholeiite serie, mainly consist of pyroxene, hornblende, feldspar, chlorite and phlogopite; All the granites are peraluminous granites related to the Yanshanian collision-orogeny. Laoka granite closely related to the tin-polymetallic deposits emplaced in the post- orogenic.The metal elements show obviously vertical zones with the variety of skarn types in dimensional extension; The occurrence of garnet skarn and diopside skarn alternately developed in the horizontal zones of the contact between granite and carbonatite are mainly related to two factors: one factor is the infiltration metasomatism of post-magmatic hydrothermal solution, the another is the metrical strata of marble and calcic-dolomite developed in country rocks.
本文重点以老厂矿田中的接触带锡铜矿床和脉状矿床为研究对象，采用化学分析、ICP-MS、X射线粉晶衍射分析、电子探针等测试手段，对本区与成矿相关的基性-超基性火山岩、花岗岩、夕卡岩、电气石-石榴石等进行了系统的地质地球化学研究，研究表明：个旧矿区中三叠纪个旧组地层中的火山岩为钙碱性玄武岩-拉斑玄武岩系列，岩石为辉石-角闪石-长石-绿泥石-金云母组合；本区的花岗岩为过铝质花岗岩，主要与燕山期碰撞造山作用有关，锡多金属成矿与形成时代最晚、分异较好的花岗岩关系密切；本区夕卡岩中的有用共生组份随着夕卡岩类型及其矿物组合的不同具有明显的分带性。
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This paper deals mainly with the characteristics of the petrology, mineralogy, petrochemistry and geochemistry for the basic volcanics. The above result has indicated that these volcanic rocks are mainly a suite of eruptive pillow basic lava from the sea-floor, which have the characteristics of the continental and oceanic tholeiites and belong to the evolutionary products of the Liaohe rift from continental crust to oceanic crust.
重点討论了基性火山岩的岩石学、矿物学、岩石化学和地球化学特徵，结果表明，这些基性火山岩主要为一套海底喷发的基性枕状熔岩，具有大陆拉斑玄武岩和大洋拉斑玄武岩的双重特徵，是辽河裂穀由大陆壳向大洋壳演化过程中的產物。
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The compositions of major elements from the rocks are consistent with those of basalt and have evolutional current of tholeiite.
岩石的主量元素组成和玄武岩一致，并且具有拉斑玄武岩演化趋势。
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Basic suite consists of tholeiite and alkali-basalt.
基性岩套由拉斑玄武岩-碱性玄武岩组成。
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The second faulting activity during late period of early Cretaceous, controls the formation of a series of faulting bounded basins with dustpan shape, as well as the formation of interlayer between tholeiite and alkaline basalt bearing olivine existed in red layer.
早白垩世晚期的第二次断陷，则控制了赣杭带沿线—系列箕状断陷盆地以及红层中拉斑玄武岩和碱性橄榄玄武岩夹层的形成。
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Metabasic volcanic rocks are a transitional type between island-arc tholeiite and mid-oceanic tholeiite.
而变质基性火山岩属于岛弧拉斑玄武岩与大洋拉斑玄武岩的过渡类型，它们形成于拉张盆地。
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The basalt is belong island arc tholeiite and series of the calc-alkaline,and have character of island arc in rare earth element and trace element.
玄武岩属岛弧拉斑玄武岩和钙碱性系列，属太平洋型钠质类型，稀土、微量元素显示具岛弧特征，大地构造位置为岛弧中心靠近大洋一侧，与南侧那拉提晚泥盆—早石炭世侵入岩共同组成火山弧，同为古亚洲洋向北俯冲的产物。
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Basalts plot in tholeiite in A.I-Al〓O〓 diagram. They have enriched LREE patterns without negative Eu anomaly. Their Zr/Y=4.4～6.5,〓=0.70790～0.70146, Th＞＞Ta,εNd values are between -1.8 and +3.7, indicating continental contamination. Pb isotope characteristics are close to that of typical tholeiitic flood basalt in the world.
Al〓O〓图上落入拉斑玄武岩区；稀土配分为LREE富集型，均无负Eu异常，Zr/Y＝4.4-6.5，〓＝0.70790～0.70146；Th＞＞Ta，ε〓介于-1.80～+3.7之间，都显示了陆壳混染的影响，Pb同位素与世界上典型拉斑质溢流玄武岩比较接近。
- 更多网络解释与拉斑玄武岩相关的网络解释 [注：此内容来源于网络，仅供参考]
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tholeiitic dolerite：拉斑玄武岩质粒玄岩
tholeiitic basalt 拉斑玄武岩 | tholeiitic dolerite 拉斑玄武岩质粒玄岩 | tholeiitic gabbro 拉斑玄武岩质辉长岩
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olivine tholeiite：橄榄拉斑玄武岩
olivine nephelinite 橄榄霞石岩 | olivine tholeiite 橄榄拉斑玄武岩 | olivine 橄榄石
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tholeiite：拉斑玄武岩
流纹英安岩(rhyodacite)可用于36和4区的岩石9区和 10区- 这两个区包括玄武岩(basalt)和安山岩(andesite),暂时用颜色指数以40%重量百(highalutnina basalt)一般局限在10区,拉斑玄武岩(tholeiite)位于10和10'区,碱性玄武岩(alkalibasalt)一般在10,
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oceanic tholeiite：海洋性拉斑玄武岩
oceanic rise 大洋中隆 | oceanic tholeiite 海洋性拉斑玄武岩 | oceanic water 大洋水
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oceanic tholeiite：大洋拉斑玄武岩
大洋环流|ocean circulation | 大洋拉斑玄武岩|oceanic tholeiite | 大洋区|oceanic zone
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ridge tholeiite：洋脊拉斑玄武岩
ridge segment 海岭块段 | ridge tholeiite 洋脊拉斑玄武岩 | ridge 脊
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low-K tholeiite：低钾拉斑玄武岩
low-interest loan 低息贷款 | low-K tholeiite 低钾拉斑玄武岩 | low-key 低调,低音键,深调影像
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bytownite sakalavite：倍长玻英玄武岩;钠钙玻英玄武岩
"bytownite anorthosite","倍长斜长岩;钠钙斜长岩" | "bytownite sakalavite","倍长玻英玄武岩;钠钙玻英玄武岩" | "bytownite-tholeiite","倍长拉斑玄武岩;钠钙拉斑玄武岩"
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bytownitite：倍长岩;钠钙长岩
"bytownite-tholeiite","倍长拉斑玄武岩;钠钙拉斑玄武岩" | "bytownitite","倍长岩;钠钙长岩" | "bytownorthite","倍钙长石"
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trachyandesite basalt：粗安质玄武岩
580 THOLEIITIC PICRITE BASALT拉斑苦橄玄武岩 | 590 TRACHYANDESITE BASALT 粗安质玄武岩 | 600 TRANSITIONAL BASALT 过渡玄武岩