- 更多网络例句与岩石学的相关的网络例句 [注：此内容来源于网络，仅供参考]
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The classification of igneous rocks is an old topic in the long history of igneous rocks petrography.
火成岩的分类命名问题，在火成岩岩石学的研究历史中是一个比较古老的话题。
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The first method is not related to petrogenesis, but welcomed by its benefit in field work and basic petrology research; the second method reflects magma sources and tectonic environment, which has always been considered to be very important since proposed, especially a steady flow of A-type granite result in recent years; the third method, often used by researchers, consists of information about mineralogy, petology and magma source; the last method is characterized for its simple and uniform classification criterion, as well as strong operability.
矿物学－岩石学分类不涉及成因信息，比较适用于野外工作以及最基本的岩石学研究；ISMA分类的标准反映的是岩浆源区和构造环境，自提出后备受重视，尤其是A型花岗岩的研究成果近来大量涌现；Barbarin的综合性分类包含了矿物学、岩石学和岩浆源区的信息，也受到一定的推崇；Frost的地球化学分类标准统一，具有很强的操作性。
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In this paper the author discusses the petrography feature of the rock in the scale ductile shear zone and the characteristics of the shear belt.
本文主要从岩石学的角度论述了两条韧性剪切带内的岩石岩相学特征，讨论了韧性剪切带以及剪切带内岩石的特征。
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The branch of petrology that deals with the origin of rocks, especially igneous rocks.
岩石成因说，岩石发展学研究岩石成因的岩石学的一个分支，尤其是火成岩的成因
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Study on the lithology and petrology (fine-grained cold-quenching ring of the enclaves, the reverse vein, the complex enclaves, the plagioclase phenocryst from both host rock and enclaves that is consist on the crystal form, composition and light, et al.), petrogeochemistry (Y/Nb=2.77～6.82, La/Nb=0.91～4.33, Ba/Nb=0.13～37.86, et al.), Sr and Nd isotope most ISr between 0.7031～0.7041,εNd(t=5.2～7.1 and LA-ICP-MS zircon U-Pb dating (the host rock age is 311±12Ma, and enclaves is 306±7Ma), believe the Huangyangshan pluton is crust-mantle hybrid genesis.
通过岩石学和岩相学（包体细粒淬冷边，反向脉，复合包体以及寄主岩石和包体中斜长石斑晶在形态、成分、光性上的一致性等），岩石地球化学（Y/Nb=2.77～6.82，La/Nb=0.91～4.33，Ba/Nb=0.13～37.86等），Sr和Nd同位素（ISr多数在0.7031～0.7041，εNd在5.2～7.1之间）以及LA-ICP-MS锆石U-Pb测年（寄主岩石为311±12Ma，包体为306±7Ma）综合研究认为黄羊山花岗岩是壳-幔源岩浆混合成因的。
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This study wants to perform researches on the Kangjinla chromitite and its host rock-mantle peridotite, to determine the existence of special mantle minerals, to discuss the origin of the chromtite and mantle peridotite together with the genetic relation between them.
本论文拟开展罗布莎地幔橄榄岩体中的康金拉铬铁矿床及其围岩地幔橄榄岩的研究，查明该铬铁矿矿体，尤其矿体围岩的地幔橄榄岩中是否也存在金刚石等特殊地幔矿物；通过详细的矿物学和岩石学的研究，探讨铬铁矿和地幔岩的成因，以及两者之间的成因联系。
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This thesis studies the volcanic tectono-petrofacies, petrology, mineralogy, geochemistry, isotopic chronology, stratum and high-precision SHRIMP zircon U-Pb datings of the Mt.Yandangshan volcano-intrusive complex, and concludes that: Yandangshan volcanic rock units belong to high-K calc-alkaline acid rock associations, mainly ryholitic and trachytic dacitic in composition. They have A/CNK values of 0.9-1.2 (i.e., aluminium saturation and supersaturation), enriched LREE and LILEs and depleted HFSE. Their 8Eu values are 0.11-0.32, indicating a evident fractional evolution of plagioclase crystallization. Their ∑REE varied very limitedly,(87~Sr/(86)Sri ratios and eNd values are 0.7086～0.7095 and -10.20～-9.96 for volcanic rocks, and 0.7087~0.7095 and -7.6～6.92 for the central intrusive facies syenite, which means that all the igneous rocks from Mt. Yandangshan are evolutional products of magmas with the same source, and that they derived mainly from crust, but mixed with mantle components.
本文从火山构造岩相学、岩石学、矿物学、地球化学、同位素年代学、地层学等方面出发，同时结合高精度SHRIMP锆石U-Pb定年，对雁荡山火山岩进行了系统的研究，确定雁荡山火山岩为一套以流纹质和粗面英安质为主体的高钾钙碱性酸性岩石组合，A/CNK值集中在0.9～1.2之间，为铝饱和或铝过饱和类型；富轻稀土元素和大阳离子亲石元素、相对亏损高场强元素：负铕异常明显，δEu值为0.11～0.32，表明岩浆经历了以斜长石为主的强烈结晶分异作用：岩石样品的∑REE变化有限，火山岩样品的~(87Sr/~(86)Sr_i为0.7086～0.7095，εNd为-10.20～-9.96，中央侵入体石英正长岩~(87Sr/~(86)Sr_i为0.7087～0.7095，εNd为-7.6～-6.92，表明它们是同源岩浆分异演化的产物，物质来源主要为陆壳，但有地幔物质参与。
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In addition to available data, we can conclude that crust contamination of Lutao arc magma has resulted in low helium ratios, high strontium ratios and low neodymium ratios of Lutao lavas.
配合上岩石学的观察，本研究推论绿岛火成岩曾受到地壳混染作用影响，而产生低3He/4He比值、高锶同位素及低钕同位素比值的地化特性。
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The rapakivi granites have a number of petrological peculiarities.
环斑花岗岩具有若干岩石学的特征。
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Basaltic underplating has deepened the CMB from 32 km to 42 km. The lower crust beneath Hannuoba consists mainly of two-pyroxene granulites, with minor felsic granulites, noritic granulites, spinel pyroxenites and spinel lherzolites.
该地温梯度线表明，华北克拉通北缘的岩石学壳幔边界很可能位于约42km处，与地震莫霍面近于一致。32-35km处的尖晶石二辉橄榄岩层可能反映了古岩石学壳幔边界的位置，玄武质底垫作用造成岩石学壳幔边界的深移。
- 更多网络解释与岩石学的相关的网络解释 [注：此内容来源于网络，仅供参考]
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petrochemistry：岩石化学
在防护性能方面,岩石化学 岩石化学(petrochemistry)又称化学岩石学(chemical petrology). 岩石学的一个分支. 主要研究各种岩石的化学成分和有成因联系的岩石在化学上成分方面的相
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petrology：岩石学
构造岩石学(Structural Petrology)是构造地质学(Structural Geology)与岩石学(Petrology)之间的一门交叉边缘学科,岩组分析(Petrofabric Analysis)可看作构造岩石学的同义语,30.40年代,这一领域的学术代表在西方主要是B.Sander和E.Cloos,
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sedimentary petrology：沉积岩石学
2, 沉积岩石学 (Sedimentary petrology)是研究沉积岩(包括沉积矿产)的特征、成因、及其在时间和空间上分布规律的一门地质学科,它是"岩石学"的一支独立分科.
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descriptive petrology：描述岩石学
描述岩石学(descriptive petrology)又称岩相学(petrography)、岩类学. 岩石学的一个分支. 研究岩石的物质成分、结构、构造,分类命名以及产状、伴生关系和分布规律等. 研究方法包括野外实地调查和观察及室内鉴定,如薄片研究及化学分析等[1]
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petrosal：岩石的
petrology 岩石学 | petrosal 岩石的 | petrous 岩石的
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ichnolithology：遗迹岩石学
ichnolite 含化石足迹的岩石 | ichnolithology 遗迹岩石学 | ichnological 足迹化石的
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micropetrography：显微岩石学
microperthite 微纹长石 | micropetrography 显微岩石学 | microphanerocrystalline 微显晶质的
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petrographic：岩石分类的; 岩相学的; 岩石记载学的 (形)
petrochemistry 石油化学, 岩石化学 (名) | petrographic 岩石分类的; 岩相学的; 岩石记载学的 (形) | petrography 岩石分类学 (名)
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petrologic：岩石学的 (形)
petroleum 石油 (名) | petrologic 岩石学的 (形) | petrologist 岩石学家 (名)
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Gemology：宝玉石学
珠宝玉石学(gemology)是研究珠宝玉石的科学,是以矿物学和岩石学为基础,并与材料学、工艺美术学等一些学科互相渗透发展起来的一个新的学科. 它研究珠宝玉石的化学成分、矿物组分、结构和构造、物理性质、化学性质和成因机制、产生规律及其资源开发、人工宝石制造、宝石改善、珠宝玉石款式设计与加工工艺、珠宝玉石市场规律与