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1)  Xialu chert
下鲁硅岩
1.
Xialu chert is named for a Late Jurassic to Early Cretaceous siliceous sequence on the southern side of the Yarlung Zangbo ophiolite belt in Xigaze area,southern Tibet.
下鲁硅岩为藏南日喀则地区雅鲁藏布蛇绿岩南侧的晚侏罗世—早白垩世硅质岩系。
2)  Silicalite
硅岩
1.
The origin of the Shitoukoumen silicalite,Jilin province and its structural setting;
吉林省石头口门硅岩之成因及构造环境
2.
Lithogenesis Research of Silicalite and Limestone of Silurian in the Uranium Metallogenic Belt in Western Qinling;
西秦岭铀成矿带中志留系硅岩灰岩的成因研究
3)  chert [英][tʃə:t]  [美][tʃɝt]
硅岩
1.
Geochemistry and Origin of Late Paleozoic Cherts in Guangxiand Their Explanation of Tectonic Environments;
广西晚古生代硅岩的地球化学及其形成的大地构造环境
2.
The chert was formed in rift fault basin between Yangtze continental and Huaxia continental.
通过野外与室内的研究工作 ,认为皖南浙西地区晚震旦纪至早寒武纪的硅岩是复合成因的产物 ,其物源类型比较复杂 ,包括热水来源、生物来源及陆源输入 ,但以热水来源的SiO2 为主。
3.
Cherts are widely distributed on the surface of the earth and are a special type of sedi-mentary rocks.
回顾了国外硅岩的研究历史,概述了当今的研究现状和未来的发展趋势,并与我国同一领域的研究状况作了对比分析,提出了改变国内硅岩研究落后现状的几点建议。
4)  siliceous rocks
硅岩
1.
Geochemical characteristics and origin of the Permian siliceous rocks in Xuanhan region of Sichuan Province
四川宣汉地区二叠系硅岩地球化学特征及成因研究
2.
Stratiform tuffaceous siliceous rocks are widely exposed in the Nomhon ?Xiangride area of the mid-dle part of East Kunlun, mostly occur within volcanic lava and above it.
东昆仑中段诺木洪—香日德一带,大量出露层状、块层状凝灰质硅岩,主要产于火山熔岩之中及其上部,岩石致密,成层性好,具有独特的地球化学特征。
5)  siliceous rock
硅岩
1.
It mainly consists of dolomite interbeded with siliceous rock.
北京西山地区雾迷山组发育硅质条带白云岩,在硅质条带中发育典型的风暴硅岩沉积。
6)  Ludian Granite
鲁甸花岗岩
补充资料:二氯二甲基硅烷与二氯二苯基硅烷、三氯甲基硅烷、三氯苯基硅烷和三氯苯基硅烷的聚合物
CAS:28630-33-3
分子式:(C12H10Cl2Si·C6H5Cl3Si·C2H6Cl2Si·CH3Cl3Si)x
中文名称:二氯二甲基硅烷与二氯二苯基硅烷、三氯甲基硅烷、三氯苯基硅烷和三氯苯基硅烷的聚合物
英文名称:Silane, dichlorodimethyl-, polymer with dichlorodiphenylsilane, trichloromethylsilane and trichlorophenylsilane silane, dichlorodimethyl-, polymer with dichlorodiphenylsilane, trichloromethyl
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