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长石石英
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  feldspar-quartz
     The protoliths of quartz jadeitite include metamorphosed granite, trondhjemite, acidic volcanic rocks and feldspar-quartz sandstone.
     石英硬玉岩原岩包括正变质的花岗岩和奥长花岗岩、副变质的酸性火山碎屑岩和长石石英砂岩。
短句来源
     There exist two gold mineralization stages in the Wulashan deposit. K feldspars from the major K feldspar-quartz veins are characterized by higher K-2O and higher formation temperatures of 307~379℃ with an average of 353℃.
     乌拉山金矿床的成矿作用分为两个阶段,主要的含金钾长石石英脉中的钾长石富K2 O ,形成温度为30 7~379℃,平均为35 3℃;
短句来源
     on the other hand,water-bearing sand boies of Huanhe-Huachi Formation,composed of feldspar-quartz fine-sand of bar and lakefront,occurs isolated lens and has charateristics of poor aquosity,complex pore-throat texture,strong corrosion and high mineralization degree.
     环河华池组含水砂体,由三角洲水下分流河道以及滨湖滩坝相长石石英细砂岩组成,呈孤立透镜体状,含水性差,孔喉结构复杂,水溶蚀作用强,矿化度高;
短句来源
  feldspathic quartz
     The pore structure characteristics of reservoir in the north Melut Basin,Sudan,including the effect of lithology,diagenesis,pore types and clay minerals on pore structure,show that the reservoir's lithology is mainly lithic quartz arenite and feldspathic quartz arenite,and has middle textural and compositional maturity.
     对苏丹Melut盆地北部油田储集层孔隙结构研究结果表明,该油层储集层以岩屑石英砂岩及长石石英砂岩为主,结构成熟度、成分成熟度中等;
短句来源
     The rocks, white or light yellow-white in color, is intercalated in the feldspathic quartz sandstone, siltstone and conglomerate.
     该类岩石呈白色、黄白色,夹于浅海相黄白色长石石英砂岩、粉砂岩和砾岩中。
短句来源
     Folding of the middle-upper Proterozoic Jianshan Formation of Baiyunebo Group is very complex in Huaguoshan area of southeast Baiyunebo, northern margin of North China Platform. In order to study the shapes of folds and their deformation mechanism, 1/2000 scale geological mapping has been made in an area of 1 km 2. Two stages of folding have been defined based on distribution of metamorphic feldspathic quartz sandstone.
     华北地块北缘中上元古界的白云鄂博群尖山组 ,在白云鄂博群东南花果山一带褶皱变形十分复杂 ,为了研究其褶皱形态、变形机制 ,在原 1∶ 5万填图的基础上选近 1 km2的范围进行1∶ 2 0 0 0大比例尺地质填图 ,以变质长石石英砂岩为标志层 ,确定了两期褶皱构造。
短句来源
     THE TEST STUDY ON THE KAISER EFFECT OF THE FELDSPATHIC QUARTZ SANDSTONE UNDER TRIAXIAL COMPRESSION
     三向应力下长石石英砂岩凯塞尔效应试验研究
短句来源
     Its main rocks is the metamorphic pelitic siltstone, the feldspathic quartz wacke,the fine sandial feldspathic quartz siltstone,the feldspathic wacke and the sericite quartz phyllite etc.
     主要岩性有变泥质粉砂岩、长石石英杂砂岩、细砂质长石石英粉砂岩、长石杂砂岩、绢云石英千枚岩等。
短句来源
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  “长石石英”译为未确定词的双语例句
     Quartz cementation characterizes the sandstones of Taiyuan Formation,causing the lose of primary pores.
     太原组石英砂岩以石英增生与胶结作用为主; 山西组长石砂岩及长石石英砂岩以长石及石英增生、碳酸盐胶结交代作用为主;
短句来源
     ADSORPTION MECHANISM OF DODECYL AMINE-HYDROCHLORIDE ON FELDSPAR AND QUARTZ AND EFFECT OF pH
     十二胺盐酸盐在长石石英表面的吸附机理及pH值对吸附的影响
短句来源
     The reservoir of upper Triassic Xujiahe formation in northwest Sichuan is mainly feldspar quartz sandstone and feldspa lithic quartzite sandstone.
     川西北部上三叠统须家河组储集岩主要为长石石英砂岩、长石岩屑石英砂岩。
短句来源
     According to macroscopic, microscopic, geochemical, and isotopic geochemical data, the authors hold that the grey brecciated silicified rock and black silty tuffaceous shale were formed under the influence of volcano_seismic event, thus serving as a kind of event message_bearing rock, whereas the overlying yellow feldspar_bearing quartz sandstone was formed in a normal littoral environment.
     宏观、微观特征、地球化学和同位素地球化学分析数据表明 :泰陵剖面大红峪组的灰色角砾硅化岩和黑色粉砂凝灰页岩是受火山 -地震事件影响形成的沉积岩 ,而覆盖其上的黄色含长石石英砂岩形成于正常滨海环境中。
短句来源
     Type D has only one sample, which comes from the metamorphosed arkose sandstone.
     D型是变质的长石石英砂岩。
短句来源
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  feldspar-quartz
According to this classification, the petrochemical types A-E may be correlated with monomictic (A'), oligomictic (B'), and mesomictic (C') sandstones, feldspar-quartz graywacke (D') and graywacke proper (E'), respectively.
      
Aggregates of black-colored minerals are not the products of the fractionation of the initial magma or immiscibility effects, because the structure of the albite-potassium feldspar-quartz-mica matrix is the same both in black and light granites.
      
The ores are underlain by comformable alteration zones characterized by albite-gedrite-quartz and biotite-muscovite-plagioclase-K-feldspar-quartz +/- garnet assemblages.
      
In augite-hornblende monzodiorite, alteration progressed from a hematite-stained alkali feldspar-quartz-calcite assemblage and quartz-molybdenite-pyrite veins to a late reduced sericite-dolomite-albite assemblage.
      
Garnet-biotitesillimanite-K feldspar-quartz relations combined with the partial melting data suggest a decrease in water activity from near 1.0 in the lower grade zones to 0.5±0.2 in the Broken Hill - Little Broken Hill part of the two pyroxene zone.
      
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松辽盆地下白垩统下部地层中所发现的浊沸石,产于由长石、石英及酸性喷发岩岩屑所组成的混杂砂岩之中,呈胶结物形式,是一种典型的自生矿物,其埋藏深度多在3000米以上。它的出现,在勘探初期,对于粗略评价生储层,研究其纵向演变规律,具有重要的地质意义。

The meso-epithermal uranium deposit described in this paper is closely related to the“multiple-staged”composite quartz-syenite body, It is a new of uranium type deposit in our country. The mineral association of this deposit is relatively simple. The pitchblende is the chief industrial mineral. The main paragenetic minerales are: uranophane, uranium blacks, autunite, meta-torbernite, microquartz, quartz, ankerite, calcite, fluorite, hydromica, pyrite, galena, sphalerite, and chalcopyrite. The mineralization...

The meso-epithermal uranium deposit described in this paper is closely related to the“multiple-staged”composite quartz-syenite body, It is a new of uranium type deposit in our country. The mineral association of this deposit is relatively simple. The pitchblende is the chief industrial mineral. The main paragenetic minerales are: uranophane, uranium blacks, autunite, meta-torbernite, microquartz, quartz, ankerite, calcite, fluorite, hydromica, pyrite, galena, sphalerite, and chalcopyrite. The mineralization period may be divided into eight stages. Results of the isotopic researches indicate that most of the uranium forming the uranium deposit is derived from the magmatic solutions and the rest is from the wall rocks, the feldspar-quartz-sandsstone of the Jurassic system. The radiometric age of pitchblende is 109—108 m. y. It is considered to be promising to search for this kind of uranium deposits in the vicinites.

本文介绍的中-低温热液轴矿庆与一个多阶段复式石英正长岩体密切有关。它是我国新的一种轴矿床类型。本矿床的矿物组合不很复杂。沥青轴矿是主要工业矿物。主要伴生矿物有:硅钙铀矿、铀黑、钙铀云母、准钢铀云母、微晶石英、石英、铁白云石、方解石、萤石、水云母、黄铁矿、方铅矿、闪锌矿及黄铜矿等。矿化作用共可分为八个阶段,同位素研究结果表明,矿床中的铀主要来自岩浆溶液,部分轴来自围岩——侏罗系长石石英砂岩。沥青铀矿的同位素年龄为108—109百万年。应当注意在邻区内寻找与上述类型相同的铀矿床。

The meso-epithermal uranium deposit described in this paper is closely related to the "multiple-staged" composite quartz-syenite body. It is a new of uranium type deposit in our country. The mineral association of this deposit is relatively simple. The pitchblende is the chief industrial mineral. The main paragenetic minerales are: uranophane, uranium blacks, autunite, meta-torbernite, microquartz, quartz, ankerite, calcite, fluorite, hydromica, pyrite, galena, sphalerite, and chalcopyrite. The mineralization...

The meso-epithermal uranium deposit described in this paper is closely related to the "multiple-staged" composite quartz-syenite body. It is a new of uranium type deposit in our country. The mineral association of this deposit is relatively simple. The pitchblende is the chief industrial mineral. The main paragenetic minerales are: uranophane, uranium blacks, autunite, meta-torbernite, microquartz, quartz, ankerite, calcite, fluorite, hydromica, pyrite, galena, sphalerite, and chalcopyrite. The mineralization period may be divided into eight stages. Results of the isotopic researches indicate that most of the uranium forming the uranium deposit is derived from the magmatic solutions and the rest is from the wall rocks, the feldspar-quartz-sandsstone of the Jurassic system. The radiometric age of pitchblende is 109—108 m.y. It is considered to be promising to search for this kind of uranium deposits in the vicinites.

本文介绍的中一低温热液铀矿床与一个多阶段复式石英正长岩体密切有关。它是我国新的一种铀矿床类型。本矿床的矿物组合不很复杂。沥青铀矿是主要工业矿物。主要伴生矿物有:硅钙铀矿、铀黑、钙铀云母、准铜铀云母、微晶石英、石英、铁白云石、方解石、萤石、水云母、黄铁矿、方铅矿、闪锌矿及黄铜矿等。矿化作用共可分为八个阶段,同位素研究结果表明,矿床中的铀主要来自岩浆溶液,部分铀来自围岩——侏罗系长石石英砂岩。沥青铀矿的同位素年龄为108—109百万年。应当注意在邻区内寻找与上述类型相同的铀矿床。

 
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