- 更多网络例句与二长闪长岩相关的网络例句 [注：此内容来源于网络，仅供参考]
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Research for ore-controlling factors indicates that the mineralization is associated closely with the emplacement of quartz monzonite diorite.
对矿区控矿因素的研究表明，成矿与石英二长闪长岩的侵入密切相关。
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Calidonian granites are widely developed in the Yema Nanshan area in the western segment of the Qilian orogenic belt. The geochemical characteristics of most of the granites are similar to those of adakites: SiO2≥56%, Al2O3≥15.0%, low MgO (average 2.04%), high Sr (257-889μg/g, average 546.42μg/g), low Y (7.1-25.3μg/g,average 16.67μg/g), average Sr/Y=5.89, no pronounced Eu anomaly and Sr positive anomaly. Adakites in this area have five rock types, quartz diorite, quartz monzodiorite, quartz monzonite, monzogrannite and hornblende granite. These rocks commonly contain hornblende, belonging to I-type granites.
提要：祁连西段野马南山一带发育大量的加里东期花岗岩，其中大部分花岗岩具有与adakite岩相似的地球化学特征，SiO2≥56%， Al2O3≥15.0％，低MgO（平均2.04％），高Sr(257～889μg/g，平均值546.42μg/g)，低Y（7.1～25.3μg/g，平均16.67μg/g），Sr/Y平均为35.89μg/g，Eu无明显负异常，Sr正异常，Adakite岩石类型有石英闪长岩、石英二长闪长岩、石英二长岩、角闪花岗岩、二长花岗岩，岩石中普遍含有角闪石，属I型花岗岩，地球化学图解反映该花岗岩形成环境为板块碰撞前的岛弧型，锆石U-Pb同位素年龄为444+38/-33 Ma，处在祁连造山带板块俯冲收缩阶段，因此可以推断野马南山埃达克质Adakite花岗岩是俯冲板片部分融熔和壳幔岩浆混合形成的。
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The Dabie Mountains are unique among ultrahigh pressure metamorphic terranes in having the most profound post collisional plutonism The Mesozoic shoshonitic and calc alkaline intrusive rocks can be divided into three groups with different isotopic ages, rock assemblages and chemical features Group I consists of late Triassic (~ 210 Ma) mafic monzodiorites It could have been generated by partial melting of enriched subcontinental lithosphere mantle due to slab breakoff Group II consists ma...
第 I组，主要由晚三叠世（约210 Ma）二长闪长岩辉长岩体组成，它可能是在板片断离过程中富集的大陆岩石圈地幔部分熔融的产物；第I I组，由中侏罗世－早白垩世（160～120 Ma）的角闪石英二长岩、黑云母二长花岗岩和正长花岗岩组成，主要是由幔源岩浆的分离结晶与地壳混染共同作用的产物；第II I组，以白垩纪（125～95 Ma）的花岗岩和花岗斑岩为代表，是在热穹窿作用过程中大别杂岩深熔作用和高度演化的产物。
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The Indosinian granitoid belt in South Qinling, Central China, is lithologically composed of diorite, monzodiorite, tonalite, granodiorite and granite, as well as widely distributed mafic microgranular enclaves and dykes within the intrusions.
南秦岭印支期花岗岩带的岩石组合包括闪长岩、二长闪长岩、英云闪长岩、花岗闪长岩和花岗岩等，岩体内广泛存在镁铁质微粒包体和脉体。
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It indicated that, brecciated granodiorite was foemed mainly by chemical attack, brecciated ore and brecciated marble were hydraulic breccias which were formed mainly by mechanical process, and the energy when brecciated ore was formed is higher than the energy when brecciated marble was formed.During the research of tectono-geochemistry in the south part of Fenghuangshan copper deposit, it is discovered that the fractal character of Cu is multifractality, and different from each other according to the geological bodies.
凤凰山铜矿床南区构造地球化学取样分析中的Cu元素含量具有多重分形的特点，且不同的地质体中其分形特征不同，结合Cu元素在不同地质体中的分布特点，说明本区不同地质体所经历的成矿作用不同，其中以石英二长闪长岩所经历的成矿作用强度较大，较有利于成矿元素的富集。
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Chondrite-normalized REE patterns are right-inclined, and the REE distribution patterns for skarn and ores are similar to those of the Tongguanshan quartz monzodiorite, which indicates that the hydrothermal fluids of the skarn deposit in the study area were mainly derived from dioritic melt.
稀土元素球粒陨石标准化组成模式为右倾型，夕卡岩，矿石的稀土配分曲线类似于铜官山岩体石英二长闪长岩，故认为形成本区的夕卡岩型矿床的热液流体主要来源于闪长质熔体。
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The Xiaotongguanshan copper deposit located in the Tongguanshan copper field is related to the Tongguanshan quartz monzodiorite.
小铜官山铜矿床位于安徽铜陵铜官山矿田，侵入岩体为铜官山石英二长闪长岩。
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The Fenghuangshan pluton, which consists of granodiorite and quartz monzodiorite, is the main part of the Fenghuangshan ore field Zircon SHRIMP 206Pb/238U dating shows that the Fenghuangshan pluton formed at (144.2±2.3) Ma, belonging to the Late Jurassic era, which is in accordance with most of metallogenic plutons of the Tongling metallogenic cluster area.
凤凰山岩体为凤凰山矿田的主要组成部分，主要岩石类型为花岗闪长岩、石英二长闪长岩。根据精确锆石SHRIMP测年结果，凤凰山岩体206Pb/238U年龄为(144.2±2.3)Ma，是晚侏罗世形成的一个典型岩体，和铜陵矿集区主要成矿岩体的形成时代一致。
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Detailed geology- petrology-mineralogy study shows that late Triassic-early Jurassic granites can be divided into 4 groups: granodiorites, monzonitic-K syenogranites mainly, alkali feldspar-alkali granites and syenite, Middle Jurassic granites is composed of quartz diorites-granodiorites and monzonitic granites, the main rock type includes granodiorites and monzogranites; Early Cretaceous granites include alkali gabbro, alkali granites and granodiorites, and these rocks composed bimodal igneous rock group.
详细的地质-岩石矿物学研究表明，晚三叠-早侏罗世花岗岩可以划分成四种岩石组合，即花岗闪长岩组合、二长花岗岩—正长花岗岩组合、碱长花岗岩—碱性花岗岩组合和正长岩组合，其中以二长花岗岩—正长花岗岩组合为主；中侏罗世花岗岩由石英闪长岩-花岗闪长岩组合和二长花岗岩组合构成，岩石类型以花岗闪长岩和二长花岗岩为主；早白垩世出现了碱性辉长岩、碱性花岗岩和花岗闪长岩，构成双峰式火成岩组合。
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Based on isotopic ages and the cycle of magamtism, the ages of Yanbian granites can be subdivided into five periods:①late Permian granites (260-245Ma), the typical plutons are Liukesong and Liangbing plutons, and the main rock type include diorite-monzonitic-K syenogranites;②Triassic granites (225-200Ma), the typical plutons are Sandaogou, Chunyang, Qishiergedingzi, Dahuanggou, Naozhi, and Qinglinzi plutons, the main rock type include quartz dioritesgranodiorites-monzonitic-alkali granites;③early Jurassic granites (190-180Ma), which composed of quartz diorites-granodiorites - monzonitic ,and the typical plutons are Shimen, Miantian, Daxinggou and Yushuchuan rock;④Middle-Late Jurassic (170-150Ma), which composed of granodiorites- monzonitic- garnet-bearing muscovite granites, the typical plutons are Huangniling, Weizigou, Loutuoshan and Dongqing rock;⑤early Cretaceous (about 130Ma), the typical pluton is Zhongping pluton, and its rock type is paulite diorite.
另外，根据同位素年龄和岩石组合并考虑到岩浆的旋回性，将延边显生宙花岗岩进一步划分为五个期次：1。晚二叠世(260-245Ma)，代表性岩体为六棵松和亮兵，主体岩性为辉石闪长岩、二长花岗岩和钾长花岗岩；2。三叠世(225-200Ma)，代表性岩体为三道沟、春阳、七十二个顶子、大荒沟、闹枝、青林子，岩石组合为石英闪长岩—花岗闪长岩—二长花岗岩—碱长花岗岩，以花岗闪长岩和二长花岗岩为主；3。早侏罗世(190-180Ma)，石英闪长岩—花岗闪长岩—二长花岗岩组合，主体岩性为花岗闪长岩，代表性岩体有石门、棉田、大兴沟、榆树川等；4。中侏罗世(170-150Ma)，主体岩性为花岗闪长岩和含石榴石花岗岩，代表性岩体有黄泥岭、苇子沟、骆驼山、东清5。
- 更多网络解释与二长闪长岩相关的网络解释 [注：此内容来源于网络，仅供参考]
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nepheline syenite：霞石正长岩
高的副长石矿物名称作前缀,例如霞石正长岩(nepheline syenite),方钠石正长岩(sodalite syenite)等,13 区- 本区有两个基本名称,它们是副长石二长闪长岩(foidm onzodiorite)和副长石二长辉长区所述.
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dioritic：闪长岩状的
diorite 闪长岩 | dioritic 闪长岩状的 | dioxyanthraquinone 二羟蒽醌
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maenaite：富闪二长霏细岩
macrovariolitic 粗球粒玄武岩的 | maenaite 富闪二长霏细岩 | mafic rock 镁铁质岩石
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maenaite：角闪二长霏细岩;钙质歪正细晶
大漩涡 maelstrom | 角闪二长霏细岩;钙质歪正细晶 maenaite | 角闪二长霏细斑岩;钙质歪正细斑岩 maenaite porphyry
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maenaite porphyry：角闪二长霏细斑岩;钙质歪正细斑岩
角闪二长霏细岩;钙质歪正细晶 maenaite | 角闪二长霏细斑岩;钙质歪正细斑岩 maenaite porphyry | 麦斯楚风 maestrale
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monzodiorite：二长闪长岩
6区和 7 区- 这两个区岩石的基本名称分别为碱长正长岩(alkali-feldspars yenite)和正长岩9区- 本区有两个基本名称,即二长闪长岩(monzodiorite)和二长辉长岩(monzogabbro),可根据为二长闪长岩;如斜长石An大于50%并主要含辉石时,
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monzogabbro：二长辉长岩
6区和 7 区- 这两个区岩石的基本名称分别为碱长正长岩(alkali-feldspars yenite)和正长岩9区- 本区有两个基本名称,即二长闪长岩(monzodiorite)和二长辉长岩(monzogabbro),可根据为二长闪长岩;如斜长石An大于50%并主要含辉石时,
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quartz monzogabbro：石岩二长辉长岩
quartz monzobiorite 石英二长闪长岩 | quartz monzogabbro 石岩二长辉长岩 | quartz oscillator 石英晶体振荡器
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syenodiorite：正长闪长岩
而正长闪长岩(syenodiorite)和正长辉长岩(syenogabbro)分别是正长岩和闪长岩或正长岩与辉长岩之间的过渡岩石,亦即包括二长岩10 区- 本区岩石有三个基本名称,即闪长岩(diorite),辉长岩(gabbro)和斜长岩(anorthosite),以斜长石(PI)、辉石(Px),
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syenogabbro：正长辉长岩
而正长闪长岩(syenodiorite)和正长辉长岩(syenogabbro)分别是正长岩和闪长岩或正长岩与辉长岩之间的过渡岩石,亦即包括二长岩10 区- 本区岩石有三个基本名称,即闪长岩(diorite),辉长岩(gabbro)和斜长岩(anorthosite),以斜长石(PI)、辉石(Px),