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Within the granite particularly its eastern part, it is frequently met that gneiss which has its original occurrence, and granulite and amphibolite enclaves as well.

岩体中还广泛分布着各种类型的变质基性岩石包体和岩片,在东部具有明显的"成群成带"分布特点,边缘地带也较为多见。

The strata inside and outside the cave are argillaceous bedded limestone and wormkalks of late Cambrian, that is, 490—500 million years before present.

洞内外地层为距今4.9亿年—5亿年的晚寒武世泥质条带灰岩和竹叶岩状灰岩,它们都是在浅海中生成的,说明当时鱼谷洞地区曾是一片大海。

According to the research of the paper, the "migmatite" of the Sizishan Formation, Xingdong Group distributed in northern Xiao Hinggan Mountains should be a suit of gneissic quartz monzonitegranite intrusions. Their whole rockmineral Rb-Sr isochronic dating is (482±19) Ma, indicating that an Caledonian magmatic events existed in the giant granitic belt of the Xiao Hinggan Mountains.

研究表明,分布于小兴安岭北部金林林场的兴东群四子山组"混合岩"为一套片麻状石英二长岩-花岗岩侵入体,岩石全岩-矿物Rb-Sr等时线年龄为(482±19) Ma,这表明小兴安岭巨型花岗岩带中存在早古生代岩浆事件。

Luobusa ophiolite in southern Xizang is one of the best outcrop and the most study in east segment of Yarlung Zangbo ophiolite belt.

罗布莎蛇绿岩是雅鲁藏布江蛇绿岩带东段出露较好,也是研究程度较高的蛇绿岩片之一。

The Sr Nd Pb isotopic compositions of crust lavas are characterized by higher initial Sr isotopic ratios,lower Nd isotopic ratios,large εNa and enrichment in radiogenic lead.

罗布莎蛇绿岩是雅鲁藏布江蛇绿岩带东段出露较好,也是研究程度较高的(蛇绿岩片之一,其壳层熔岩的Sr,Nd,Pb同位素组成具有较高的ISr值,较低的Isd值,大的εNd值和富集放射性成因铅的特征。

Microstructural studies of three types of tectonites from eastern Liaoning area with different deformation characteristics (gneissic, banded and mylonitic structures) by means of microstructural analysis, transmission electron microscope analysis shows us they have different microstructures and Submicrostructures.

通过显微和亚微分析揭示出辽东地区三种变形特点的角闪质岩石(片麻状斜长角闪岩、条带状斜长角闪岩和糜棱状斜长角闪岩)具有差异的显微及亚微构造。

According to the research of the paper, the "migmatite" of the Sizishan Formation, Xingdong Group distributed in northern Xiao Hinggan Mountains should be a suit of gneissic quartz monzonitegranite intrusions. Their whole rockmineral Rb-Sr isochronic dating is (482±19) Ma, indicating that an Caledonian magmatic events existed in the giant granitic belt of the Xiao Hinggan Mountains.

研究表明,分布于小兴安岭北部金林林场的兴东群四子山组&混合岩&为一套片麻状石英二长岩-花岗岩侵入体,岩石全岩-矿物Rb-Sr等时线年龄为(482±19) Ma,这表明小兴安岭巨型花岗岩带中存在早古生代岩浆事件。

The original Seluohe Group contains at least four parts: Late Archean metamorphic rocks (zircon SHRIMP protolith ages 2517~2534 Ma), Late Paleozoic metamorphosed volcanic-sedimentary strata (zircon SHRIMP 252 Ma), Permian gneissic granitic complex (zircon SHRIMP 260 Ma), and Jurassic mylonitized granites (zircon SHRIMP 168 Ma).

原划分的色洛河群至少由4部分组成:新太古代变质火山-沉积地层(锆石SHRIMP年龄为2517~2534 Ma)、晚古生代变质火山-沉积地层(英安岩锆石SHRIMP年龄为252 Ma)、二叠纪片麻状杂岩体(锆石SHRIMP年龄为260 Ma)和侏罗纪糜棱岩化花岗岩(锆石SHRIMP年龄为168 Ma)。

Petrological and geochemical characteristics of alkali-rich porphyries suggest that magmas might not be generated from subducted oceanic slab, but likely from the base of thickened crust, corresponding to eclogite-facies.

富碱斑岩产出的地质背景及岩石学和地球化学特征表明,富碱斑岩并非起源于俯冲的大洋板片,而是源于加厚地壳的底部,源区为榴辉岩相岩石。

The shape of cuttings is related with the drilling parameters. The cuttings often appear in irregular flakes during air hammer drilling, and in spindle shape during cone bit drilling.

岩屑的形状与钻井参数有关,空气锤破碎岩石的岩屑形状呈不规则片状,牙轮钻头破碎岩石的岩屑形状呈纺锤形。

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