有趣的英语语法

【英语单词】彻底解释“lepidote”！ 含义、用法、例句、如何记忆

【英语单词】彻底解释“lepidote”！ 含义、用法、例句、如何记忆

简单汉语中“lepidote”的意思

形容词

生物学 lepidote 覆盖着鳞片、鳞状叶子或斑点


含义：[鳞翅目]

lepidote是一个英语单词，有几个不同的含义。 让我们用例句来解释每个的含义和用法！

Distribution of metamorphic rocks subjected to Albite- Epidote -hornfels facies contact metamorphism described in this site.
本网站描述的经历了 钠长石绿帘角岩 相接触变质作用的变质岩分布。
The radial group of green prisms is epidote .
绿 帘石 是绿色柱状晶体的 放射状集合体 。
Recovered from siliceous shale, a matrix of accretionay complex, near a bedded manganese deposit subjected to Albite- Epidote -hornfels facies contact metamorphism.
来自 硅质页岩， 是层状锰矿床附近增生杂岩的基质，经历了钠长石-绿帘石角岩相的接触变质作用。
The brown basement is a limonite crust.Recovered from a meteoric oxidation zone of the Besshi Massive Sulfide deposit subjected to Epidote -Amphibolite facies metamorphism.
来自别子型块状硫化物矿床的陨石氧化带，经历了 变质作用， 形成绿帘角闪岩相。
Recovered from tuff subjected to Albite- Epidote -hornfels facies contact metamorphism by I-type (Magnetite-series) quartz diorite.
由经过 I 型石英闪长岩（磁铁矿系列）接触变质到 亚硫酸绿帘石角岩相的 凝灰岩形成。
Recovered from a bedded manganese deposit subjected to Epidote -Amphibolite facies regional metamorphism and contact metamorphism by granite.
来自燧石中的 层状 锰矿床，经历了绿帘角闪岩相的广泛变质作用和与花岗岩的接触变质作用。
Takemori “No Trespassing” sign was erected OccurrencePneumatolytic deposit Alpine fissure in hornfels, shale of the Shimanto accretionary complex subjected to Albite- Epidote -hornfels facies metamorphism by the late Miocene (10 Ma) Tokuwa Granite.
竹森 禁止入内 出现风动沉积角岩 角岩是四万十增生杂岩的页岩在中新世晚期（1000万年前，10 Ma）由德和花岗岩从 钠长石绿帘 石角岩相变质而形成的。里面看到的。
The green parts are aggregate of fine epidote crystals, and the white parts are crystalline limestone.
绿色部分是 绿帘石 细晶体的集合体，白色部分是结晶石灰石。
Hitachi Mine SynonymAkazawa Mine OccurrenceBesshi massive sulfide deposit Besshi Massive Sulfide Deposit of the upper Akazawa Formation subjected to Epidote -Amphibolite facies metamorphism in the Late Cretaceous (100 Ma) Abukuma metamorphic belt.
日立矿山 又名赤泽矿山（赤泽红山） 产状：别子型块状硫化物矿床 由于白垩纪（100 Ma、100 Ma） 结束的 阿武隈变质作用，绿帘石角闪岩相发生了广泛的变质作用。位于赤泽组上部。
The surrounding fine prismatic transparent crystals are quartz.Recovered from an open space of an alpine fissure in hornfels, shale of an accretionary complex subjected to Albite- Epidote -hornfels facies metamorphism by I-type (Magnetite-series) granite.
角岩中高山脉的空隙中，是一种增生复合页岩，经历了 钠长石绿帘石角岩 相与 I 型（磁铁矿系）花岗岩的接触变质作用。
Recovered from slate near a chert-hosted bedded manganese deposit subjected to Albite- Epidote -hornfels contact metamorphism.This slate is a matrix of the accretionary complex in which the deposit-host chert block is included.
来自板岩，它是含有燧石块的增生杂岩的基质，它是层状锰矿床的主岩，经历了白化 绿帘石 角岩相的接触变质作用。
Albite- Epidote -hornfels facies metamorphic rocks are observed as contact metamorphic rocks aroud intrusions of plutonic rocks.
它被视为深成岩周围的接触变质岩。
Reported Minerals ThuliteEpidoteQuartz Beta quartz Mineral Assemblages Thulite Epidote – Quartz Rhyolite(Host) – Beta quartz Details of the mine Production of thulite has been known since 1900’s.
发现矿物：绿帘石、绿帘石、水晶、高温石英 矿物组合： 绿帘石、绿帘 石-水晶 流纹岩（主岩）-高温石英 概述 自明治时代以来就为人所知。
These are sand from near the Great Lakes, and you can see that it’s filled with minerals like pink garnet and green epidote , all kinds of amazing stuff, and if you look at different sands from different places, every single beach, every single place you look at sand, it’s different. Here’s from Big Sur, like they’re little jewels.
这个沙子是来自大湖的，里面充满了矿石，粉红色的石榴石， 绿色的绿帘石， 所有这些奇妙的东西。如果你看不同地方的不同沙子，每个海滩，每个地方，沙子都是不同的。大湖的沙子苏尔看起来像一颗宝石。
High-T Hydrothermal Deposit SynonymHigh-T Hydrothermal Vein Deposit, High-T Hydrothermal Ore Deposit, Hypothermal deposit Index MineralsMolybdenite, Cassiterite, Scheelite Required Geological SettingPlutonic rocks Associated metasomatic zonesHigh-T silicified zone, Epidote -Actinolite zone OccurrenceVein-type deposit formed by 300-500 degree hydrothermal fluid originated from Acidic (I-type Granite) or Neutral (Granodiorite, Diorite) I-type (magnetite-series) magmatic activities.
高温热液矿床 又称高温热液矿脉矿床、深部热液矿床、低温矿床 指示矿物 辉钼矿、锡石、白钨矿 形成所需的地质环境 深成岩 伴生蚀变带 高温硅化带、 绿帘石-放线 石带 A由于I型（磁铁矿系列）岩浆活动，由300-500度热水形成的脉型矿床，范围从酸性（I型花岗岩）到中性（花岗闪长岩、闪长岩）。
Illite-Chlorite zone Chemical Process (Alteration) – Open system under ground (Neutral metasomatism) Correlated: Prehnite-Pumpellyite facies, Albite- Epidote -hornfels facies SynonymIllite zone, Chlorite zone, Propylite zone, Sericite zone Index MineralsIllite, Chlorite, Adularia, Albite Required Geological SettingMetasomatic rocks (Neutral) OccurrenceMetasomatic zone formed by neutral hydrothermal fluid of 220-300 degree associated with Andesitic magma activities.
伊利石-绿泥石带 又称伊利石带、绿泥石带、绿泥石带、绢云母带 指示矿物 伊利石 、绿泥石、冰晶石、钠长石 形成所需的地质环境 同蚀变岩（中性） 产状安山岩 由中性热液流体形成的蚀变带由于岩浆活动，温度为220-300摄氏度。
It is part of the epidote group.
它是 绿帘石族 的石头。

听听“ lepidote ”的土声（发音）！

读法是【ˈlɛpɪˌdəʊt】。 听下面的视频并大声发音【ˈlɛpɪˌdəʊt】。

【必听】美国人解释“lepidote”的含义

简单汉语中“lepidote”的意思

形容词

生物学 lepidote 覆盖着鳞片、鳞状叶子或斑点


含义：[鳞翅目]

lepidote是一个英语单词，有几个不同的含义。 让我们用例句来解释每个的含义和用法！

Distribution of metamorphic rocks subjected to Albite- Epidote -hornfels facies contact metamorphism described in this site.
本网站描述的经历了 钠长石绿帘角岩 相接触变质作用的变质岩分布。
The radial group of green prisms is epidote .
绿 帘石 是绿色柱状晶体的 放射状集合体 。
Recovered from siliceous shale, a matrix of accretionay complex, near a bedded manganese deposit subjected to Albite- Epidote -hornfels facies contact metamorphism.
来自 硅质页岩， 是层状锰矿床附近增生杂岩的基质，经历了钠长石-绿帘石角岩相的接触变质作用。
The brown basement is a limonite crust.Recovered from a meteoric oxidation zone of the Besshi Massive Sulfide deposit subjected to Epidote -Amphibolite facies metamorphism.
来自别子型块状硫化物矿床的陨石氧化带，经历了 变质作用， 形成绿帘角闪岩相。
Recovered from tuff subjected to Albite- Epidote -hornfels facies contact metamorphism by I-type (Magnetite-series) quartz diorite.
由经过 I 型石英闪长岩（磁铁矿系列）接触变质到 亚硫酸绿帘石角岩相的 凝灰岩形成。
Recovered from a bedded manganese deposit subjected to Epidote -Amphibolite facies regional metamorphism and contact metamorphism by granite.
来自燧石中的 层状 锰矿床，经历了绿帘角闪岩相的广泛变质作用和与花岗岩的接触变质作用。
Takemori “No Trespassing” sign was erected OccurrencePneumatolytic deposit Alpine fissure in hornfels, shale of the Shimanto accretionary complex subjected to Albite- Epidote -hornfels facies metamorphism by the late Miocene (10 Ma) Tokuwa Granite.
竹森 禁止入内 出现风动沉积角岩 角岩是四万十增生杂岩的页岩在中新世晚期（1000万年前，10 Ma）由德和花岗岩从 钠长石绿帘 石角岩相变质而形成的。里面看到的。
The green parts are aggregate of fine epidote crystals, and the white parts are crystalline limestone.
绿色部分是 绿帘石 细晶体的集合体，白色部分是结晶石灰石。
Hitachi Mine SynonymAkazawa Mine OccurrenceBesshi massive sulfide deposit Besshi Massive Sulfide Deposit of the upper Akazawa Formation subjected to Epidote -Amphibolite facies metamorphism in the Late Cretaceous (100 Ma) Abukuma metamorphic belt.
日立矿山 又名赤泽矿山（赤泽红山） 产状：别子型块状硫化物矿床 由于白垩纪（100 Ma、100 Ma） 结束的 阿武隈变质作用，绿帘石角闪岩相发生了广泛的变质作用。位于赤泽组上部。
The surrounding fine prismatic transparent crystals are quartz.Recovered from an open space of an alpine fissure in hornfels, shale of an accretionary complex subjected to Albite- Epidote -hornfels facies metamorphism by I-type (Magnetite-series) granite.
角岩中高山脉的空隙中，是一种增生复合页岩，经历了 钠长石绿帘石角岩 相与 I 型（磁铁矿系）花岗岩的接触变质作用。
Recovered from slate near a chert-hosted bedded manganese deposit subjected to Albite- Epidote -hornfels contact metamorphism.This slate is a matrix of the accretionary complex in which the deposit-host chert block is included.
来自板岩，它是含有燧石块的增生杂岩的基质，它是层状锰矿床的主岩，经历了白化 绿帘石 角岩相的接触变质作用。
Albite- Epidote -hornfels facies metamorphic rocks are observed as contact metamorphic rocks aroud intrusions of plutonic rocks.
它被视为深成岩周围的接触变质岩。
Reported Minerals ThuliteEpidoteQuartz Beta quartz Mineral Assemblages Thulite Epidote – Quartz Rhyolite(Host) – Beta quartz Details of the mine Production of thulite has been known since 1900’s.
发现矿物：绿帘石、绿帘石、水晶、高温石英 矿物组合： 绿帘石、绿帘 石-水晶 流纹岩（主岩）-高温石英 概述 自明治时代以来就为人所知。
These are sand from near the Great Lakes, and you can see that it’s filled with minerals like pink garnet and green epidote , all kinds of amazing stuff, and if you look at different sands from different places, every single beach, every single place you look at sand, it’s different. Here’s from Big Sur, like they’re little jewels.
这个沙子是来自大湖的，里面充满了矿石，粉红色的石榴石， 绿色的绿帘石， 所有这些奇妙的东西。如果你看不同地方的不同沙子，每个海滩，每个地方，沙子都是不同的。大湖的沙子苏尔看起来像一颗宝石。
High-T Hydrothermal Deposit SynonymHigh-T Hydrothermal Vein Deposit, High-T Hydrothermal Ore Deposit, Hypothermal deposit Index MineralsMolybdenite, Cassiterite, Scheelite Required Geological SettingPlutonic rocks Associated metasomatic zonesHigh-T silicified zone, Epidote -Actinolite zone OccurrenceVein-type deposit formed by 300-500 degree hydrothermal fluid originated from Acidic (I-type Granite) or Neutral (Granodiorite, Diorite) I-type (magnetite-series) magmatic activities.
高温热液矿床 又称高温热液矿脉矿床、深部热液矿床、低温矿床 指示矿物 辉钼矿、锡石、白钨矿 形成所需的地质环境 深成岩 伴生蚀变带 高温硅化带、 绿帘石-放线 石带 A由于I型（磁铁矿系列）岩浆活动，由300-500度热水形成的脉型矿床，范围从酸性（I型花岗岩）到中性（花岗闪长岩、闪长岩）。
Illite-Chlorite zone Chemical Process (Alteration) – Open system under ground (Neutral metasomatism) Correlated: Prehnite-Pumpellyite facies, Albite- Epidote -hornfels facies SynonymIllite zone, Chlorite zone, Propylite zone, Sericite zone Index MineralsIllite, Chlorite, Adularia, Albite Required Geological SettingMetasomatic rocks (Neutral) OccurrenceMetasomatic zone formed by neutral hydrothermal fluid of 220-300 degree associated with Andesitic magma activities.
伊利石-绿泥石带 又称伊利石带、绿泥石带、绿泥石带、绢云母带 指示矿物 伊利石 、绿泥石、冰晶石、钠长石 形成所需的地质环境 同蚀变岩（中性） 产状安山岩 由中性热液流体形成的蚀变带由于岩浆活动，温度为220-300摄氏度。
It is part of the epidote group.
它是 绿帘石族 的石头。

听听“ lepidote ”的土声（发音）！

读法是【ˈlɛpɪˌdəʊt】。 听下面的视频并大声发音【ˈlɛpɪˌdəʊt】。

【必听】美国人解释“lepidote”的含义

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