- 更多网络例句与橄榄相关的网络例句 [注:此内容来源于网络,仅供参考]
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There are two types of peridotites within this UHP belt.(1) Garnet peridotite consists of garnet lherzolite, garnet-bearing dunite, garnet-free dunite and garnet pyroxenite, which could be considered as one of the critical rock types in a continental-type subduction zone.
根据岩石学特征,我们确定柴北缘超高压带中发育有两种类型的橄榄岩:(1)石榴橄榄岩,岩石类型包括石榴二辉橄榄岩、石榴方辉橄榄岩、纯橄岩和石榴辉石岩,是大陆型俯冲带的标志性岩石。
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There are two types of peridotites within this UHP belt.(1) Garnet peridotite consists of garnet lherzolite, garnet-bearing dunite, garnet-free dunite and garnet pyroxenite, which could he considered as one of the critical rock types in a continental-type subduction zone.
根据岩石学特征,我们确定柴北缘超高压带中发育有两种类型的橄榄岩:(1)石榴橄榄岩,岩石类型包括石榴二辉橄榄岩、石榴方辉橄榄岩、纯橄岩和石榴辉石岩,是大陆型俯冲带的标志性岩石。
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The mineral chemistry, trace elements and Sr-Nd isotopic geochemistry of different types of deep-seated inclusions indicate that Group Ⅰinclusions in western Shaudong could be the relicts of high degree of partial melting of the mantle-derived peridotites and then subjected to mantle metasomatism; the dunite and harzburgite in Group Ⅱ inclusions could be resulted from the metasomatism of silica-rich melts in the upper mantle; the olivine-pyroxenite and pyroxenite in Group Ⅱ and Group Ⅲ inclusions could be magmatic cumulates derived from magma underplating in the upper mantle.
不同结构类型深源岩石包体的矿物化学、元素和同位素地球化学研究表明,鲁西具有变质变形结构特征的橄榄岩类岩石包体为岩石圈地幔橄榄岩部分熔融后的残留体,其后又遭受了地幔交代作用的改造;具有变质变形结构,并叠加有矿物反应结构的纯橄岩和方辉橄榄岩类包体为古老岩石圈地幔被富硅质熔体改造的结果;具有残留岩浆结晶结构的橄榄岩、橄辉岩类岩石包体以及具有变晶结构或堆晶结构的辉石岩类包体为地幔更早期岩浆作用的在上地幔的堆积体。
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The meta-peridotite consists of dunite, harzburgite, lherzolite, feldspar-bearing lherzolite and garnet-bearing lherzolite and contains residual spinel with Cr#s [100*Cr/] of 30-57 and Mg#s [100*Mg/(Mg+Fe2+)] of 50-75, indicating an Al- and Mg-rich series.
变质橄榄岩主要为纯橄岩、方辉橄榄岩、二辉橄榄岩、含长二辉橄榄岩和含石榴石二辉橄榄岩,岩石中残余尖晶石的Cr'值=100×Cr/(Cr+Al为30~57,Mg'值=100×Mg/(Mg+Fe2+为50~75,指示一个富Al和Mg成分系列。
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Rock types of lithospheric mantle beneath Eastern-North China platform include harzburgite, garnet and/or chromite lherzolite, dunite, wehrlite, pyroxenite, phlogipitite, eclogite, and metasomatic rocks.
华北地台东部古老地幔岩石类型包括方辉橄榄岩、石榴石/铬尖晶石二辉橄榄岩、纯橄榄岩、异剥橄榄岩、各种类型的金云母岩和辉石岩、榴辉岩及交代岩石。
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HPLC, and its chemical structure elucidated on the basis of spectral analysis. A new method of RP-HPLC was established for the analysis of the contents of oleuropein, which is the main effective constituent. The contents of oleuropein in different positions of Syringa pubescens Turcz.
建立了测定橄榄苦甙含量的RP-HPLC法,并且利用这种方法测定了小叶丁香的不同部位——花、叶、茎和根之中的橄榄苦甙的含量;测定了不同条件下培养所得的培养物中橄榄苦甙的含量;测定了伴生菌培养物中橄榄苦甙的含量。
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Heat flows derived from garnet, chromite/chromium-spinel and pyroxene of xenoliths, xenocrysts in Mengyin and Fuxian kimberlites are higher than 40mW/m〓 calculated from the pyroxene inclusions in diamonds, and the range of pressure is 20~40kb (equivalent to 65~130km). Metasomatism (as indicated by yimengite and lindsleyite in Mengyin) is very strong in this depth range. Lherzolite, wehrlite, and diamond-free high-Ca harzburigite around the world are derived from this depth also. The observation suggests that the low-Ca harzburigitic environment for diamond stability had been changed significantly when the kimberlitic magmas erupted. This resulted from fluid interaction with harzburigite. The geotherm of the Cenozoic lithospheric mantle beneath Eastern-North China platform is higher than oceanic one. The temperature from the interior of the Tan-Lu faults is higher than that from apart off the fault.
除金刚石中的辉石温压投点落于40m W/m〓占地温线上外,捕虏体及捕虏晶中石榴石,铬尖晶石及单斜辉石的投点均偏离该地温线,显示较高的地温特点,而且捕虏体及捕虏晶的压力范围多在20-40kb(相当于65-130km)间,该深度范围内地幔的交代作用特别发育,如蒙阴大量发育的沂蒙矿、钛钾铬石等就发育于该深度范围,世界范围内不含金刚石的高钙方辉橄榄岩、二辉橄榄岩、异剥橄榄岩也分布于该区中,一方面表明捕虏体的主要取样位置已不在金刚石稳定区中,另一方面也表明金刚石稳定的橄榄岩环境,在金伯利岩侵位并捕虏他们时已发现了明显的改造,这种改造作用主要是通过长期的熔流体与先存的橄榄岩相互作用的结果。
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For Southwestern Margin of Aqikekule Lake ophiolite, their field geological, petrological, minerological, petrochemical and geochemical characteristics show that:① it outcropped as tectonic slices along the near west-to-east strike Kunzhong fault and is composed of metamorphic perodotties, cumulates and volcanic rocks, in which, chromites are distributed in the upper part of metamorphic peridotites as pods, or in the lower part of cumulates as near-strata;② metamorphic peridotites include serpentinites, chromite-bearing serpentinites, chlorite-epidote schists and chromitites, of which, chromitites have nodular and orbicular structure, and cumulates include pyroxenits, serpentinites, chromite-bearing serpentinites, chromites and metamorphically mafic rocks and only basalts are seen in volcanic rocks;③ Cr# of chromites suggest that they formed in the SSZ and Al〓O〓 and TiO〓 of metamorphic peridotites also suggest SSZ environment;④ metamorphic peridotites have V type and enriched LREE patterns, cumulates have from strongly depleted LREE, flat REE to enriched LREE patterns with universally striking positive Eu anomalies and basalts show flat REE or slight enriched LREE patterns with no Eu anomalies;⑤ trace element and Sm-Nd isotope characteristics of metamorphic peridotites imply their strikingly heterogeneous mantle character ε〓(t+4.39~+26.20 and later Nb, Ta fertilization;⑥ trace element characteristics of basalts and their tectonic diagrams show they probably formed in the rifted island arc or back-arc basin environment.
对阿其克库勒湖西南缘蛇绿岩,野外地质、岩石学、矿物学、岩石化学以及地球化学等特征表明:①该蛇绿岩以近东西向、沿昆中断裂呈构造岩片出露,由变质橄榄岩、堆晶岩和火山岩三个单元组成,其中见铬铁岩呈豆荚状产于变质橄榄岩的上部,或呈似层状产于堆晶岩的下部;②变质橄榄岩包括蛇纹岩、含铬铁矿蛇纹岩、绿帘绿泥片岩和铬铁岩等类型,其中,豆荚状铬铁矿具有结核状构造和球状构造,堆晶岩包括辉石岩、蛇纹岩、含铬铁矿蛇纹岩、铬铁岩和变质基性岩等类型,火山岩仅见玄武岩;③铬铁矿的Cr#表明其形成在俯冲带,变质橄榄岩的Al〓O〓和TiO〓成分也指示了SSZ环境;④变质橄榄岩的稀土配分型式见V型和LREE富集型两种型式,堆晶岩表现出从LREE强烈亏损、REE平坦分布到LREE富集的配分特征,并且普遍具有醒目的正Eu异常,玄武岩的稀土配分型式表现为平坦型或LREE略富集,无Eu异常;⑤变质橄榄岩的微量元素及Sm-Nd同位素特征指示了其地幔的显著不均一性ε〓(t为+4.39~+26.20以及Nb、Ta在后期的富集;⑥玄武岩的微量元素特征及构造图解表明其可能形成在裂谷岛弧或不成熟的弧后盆地环境。
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Olive is a holy tree, which always stands for power, longevity, peace and richness. The planter takes the traditional measures to plant olive in Provence and Provence Highland and show their respect to olive in harvest season. Olive oil abstracted from olive of Fashion Life Element is as cherish as nectar. And it's famous for its delicate fragrant, firm and anti-oxidating efficacy.
橄榄树是一种神圣的树木,向来是力量、长寿、和平及富庶丰沃的象征;数百年来,种植者抱着尊敬的态度,沿用传统方法,在普罗旺斯及普罗旺斯高地种植橄榄树,并在每年收割橄榄的时节,表达对橄榄树的敬意;橄榄可提炼出珍贵的橄榄油,如同琼浆玉液般的橄榄油,因拥有细致的芳香及紧肤、抗氧化的功效非常驰名。
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Peridotite xenoliths from Nüshan, Hannuoba and the Subei basin of the North China block have much lower water contents than those from other localities of the world (South Africa craton, New Mexico, Colorado plateau and basin and Range province of USA, South Mexico, French Central Massif and West Kettle of Canada). This difference is probably induced by the thermal erosion of asthenosphere during Mesozoic-Cenozoic period in the North China block.
结合已经发表的安徽女山和河北汉诺坝的橄榄岩数据,对比世界上其他地区橄榄岩的数据来看,华北的岩石圈地幔具有低的水含量:华北橄榄岩的单斜辉石水含量多<200×10^(-6),而世界上其他地区(包括南非克拉通、美国新墨西哥地区、美国Colorado高原、美国盆岭省地区、墨西哥南部、法国中央地体以及加拿大West Kettle地区)橄榄岩的单斜辉石水含量多>200×10^(-6);华北的斜方辉石水含量多<100×10^(-6),而世界上其他地区多>100×10^(-6);华北的橄榄岩全岩水含量多<50×10^(-6),而世界上其他地区多>100×10^(-6)。
- 更多网络解释与橄榄相关的网络解释 [注:此内容来源于网络,仅供参考]
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olivine diabase:橄榄辉绿岩
橄榄玄武岩 olivine basalt | 橄榄辉绿岩 olivine diabase | 橄榄辉长岩 olivine gabbro
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olive growing:橄榄栽培
olive 橄榄 | olive growing 橄榄栽培 | olive tree 橄榄树
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kimberlite:角砾云母橄榄岩
火山柱的岩石是一种名叫角砾云母橄榄岩(kimberlite)的高碱性岩石,呈深绿色. 地表风化的角砾云母橄榄岩成为一种黄棕色泥土,由地表向下采掘,则泥土转变为蓝色,表示尚未经过剧烈风化作用. 其下则是未经风化的角砾云母橄榄岩.
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loden coat:深橄榄色防水大衣. -- 橄榄
Princess Coat:公主大衣,紧身连衣裙式大衣. 重点是对襟. -- 对襟 | Loden Coat:深橄榄色防水大衣. -- 橄榄 | Hunting Jacket:猎装茄克. -- 猎装
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olivine nephelinite:橄榄霞石岩
olivine leucitite 橄榄白榴岩 | olivine nephelinite 橄榄霞石岩 | olivine tholeiite 橄榄拉斑玄武岩
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olive yellow:橄榄黄 橄榄黄
olive green 橄榄绿 橄榄绿 | olive yellow 橄榄黄 橄榄黄 | olive 深黄 深黄
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olivine tholeiite:橄榄硅质玄武岩
橄榄岩 olivine rock | 橄榄硅质玄武岩 olivine tholeiite | 橄榄岩 olivinefels
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Canarium:橄榄属(橄榄科)
香水树 Canangium odoratum Bail. | 橄榄属(橄榄科) Canarium | 橄榄(开宝);青果(南京);白药;绿榄(台) Canarium album Raeusch;Chinese loive
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Canarium album:橄榄
[目录] 不存在 [原文] 橄榄(Canarium album)又名白榄、青榄、青果. 为橄榄科(Burseraceae)橄榄属植物,常绿大乔木,原产于中国南部地区,海南、四川西昌地区都发现有原始野生橄榄. 橄榄在我国已有2000多年的栽培历史,是世界上
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olivary nucleus:橄榄下核
olivary body 橄榄体 | olivary nucleus 橄榄下核 | olive 橄榄,橄榄色,橄榄树,橄榄体,油橄榄