水井沱组,Shuijingtuo Formation
1)Shuijingtuo Formation水井沱组
1.Study on the Ontogeny of Eodiscoid Trilobites Tsunyidiscus Acutus and Sinodiscus Changyangensis from the Shuijingtuo Formation, Lower Cambrian in Eastern Yangtze Gorge Area, Hubei;湖北峡东地区下寒武统水井沱组古盘虫类三叶虫Tsunyidiscus acutus和Sinodiscus changyangensis个体发育研究
2.The microfossils described and illustrated in this paper were discovered in the black chert of the lower Cambrian Shuijingtuo Formation at Baiguoping, Hefeng, Hubei Province.湖北省鹤峰白果坪剖面下寒武统水井沱组底部黑色燧石的岩石薄片中,发现有丰富的保存完好的微化石,包括球形藻、刺球藻、丝状藻类及一些分类不明的微化石。
英文短句/例句

1.ON THE DISCOVERY OF A STAR-SHAPED FOSSIL FROM THE LOWER CAMBRIAN OF THE CHANGYANG DISTRICT OF HUBEI湖北长阳下寒武统水井沱组中星状动物化石的发现
2.New Acknowledgement of Nantuo Formation Sedimentary Facies in Liujing,Zunyi对遵义县六井南沱组沉积相的新认识
3.The rain fell in torrents, so much that we were ankle-deep in water.大雨滂沱,水深没膝。
4.Research of Well Test Interpretation for SAGD Process by Using the Combination of Vertical and Horizontal Wells直井与水平井组合SAGD试井解释方法研究
5.Miocene Wudaoliang Formation Magnetostratigraphy and Paleoenvironmental Evolution in the Tuotuohe Area of the Qinghai-Tibetan Plateau;青藏高原沱沱河地区中新世五道梁组磁性地层与古环境演变研究
6.Sedimentary characteristics of the Miocene Wudaoliang Formation in Tuotuohe Basin of Qinghai-Tibet Plateau and palaeoenvironment analysis青藏高原沱沱河盆地中新统五道梁组沉积特征及古环境分析
7.Rock Magnetism of the Carbonates in Doushantuo Formation in Yichang, South China;宜昌陡山沱组碳酸盐岩岩石磁学研究
8.Analyses on the Phosphor-bearing Character of Doushantuo Formation in Machang Area,Guiyang贵阳马场地区陡山沱组含磷特征分析
9.Research on Sub-sea BOP Arrangement for Deepwater Drilling深水钻井水下防喷器组配置选型研究
10.Many drops make a shower.许多小水点就造成滂沱大雨。
11.Design Features of the Generator of Wujiang Shatuo Hydropower Station in Guizhou贵州乌江沙沱水电站发电机设计特点
12.Private wells account for nearly all new irrigation capacity in the country.新增灌溉几乎都由私有水井组成。
13.CBM Hosting Factor Analysis in Xiaoyutuo Minefield, Songzao Mining Area, Chongqing City重庆市松藻矿区小鱼沱井田煤层气赋存因素分析
14.Drainage Gas Recovery Technique of Combing ESP and Gas Lift for Gas Wells with Large Water Production大水量气井电潜泵—气举组合排水采气工艺设计
15.Studies of water source determination method of mine water inrush based on Bayes' multi-group stepwise discriminant analysis theory矿井突水水源判别的多组逐步Bayes判别方法研究
16.Artificial groundwater recharge with reclaimed water using enhanced direct injection well recharge system再生水补给地下水的新方式——组合式强化井灌
17.Enrichment of Yunnan Bowl Tea to Ce(Ⅳ) Ion in Aqueous Solution云南沱茶自水溶液中对铈(Ⅳ)离子的富集作用
18.Study of Adsorption Characteris Characteristics of Yunnan Bowl Tea to Ce(Ⅳ) Ion in Aqueous Solution云南沱茶自水溶液中吸附铈(Ⅳ)离子的特性研究
相关短句/例句

the Totohe formation沱沱河组
1.The sporopollen assemblage found from the upper part of the Totohe formation are characterized by the dominace of angiospermous pollen,most of the sporopollens being the common elements of Paleogene.沱沱河组上部的孢粉化石组合以被子植物花粉为主,且主要为三沟和三孔沟类,包括栎粉属(尤其是小栎粉和小亨氏栎粉)、楝粉属、坡氏粉属和三孔沟粉属等,具孔类花粉很少,大部分属种为古近纪常见分子;组合中出现少量鸡爪勒粉属、唇形三沟粉属、山萝卜粉属、管花菊粉属等草本植物花粉;并含有零星古老类型的成分,如克拉梭粉属、五边粉属和江汉粉属;裸子植物花粉含量低,蕨类植物孢子零星。
3)Doushantuo formation陡山沱组
1.Macroscopic Algae from the Ediacaran Doushantuo Formation in Northeast Guizhou, South China;黔东北伊迪卡拉纪陡山沱组的宏体藻类
2.Geochemistry and petrogenesis of the cap dolostones at the bottom of the Doushantuo Formation in northwestern Fanjing Mountains,Guizhou;贵州梵净山西北陡山沱组底部白云岩帽地球化学特征及成因探讨
3.Sedimentary Successions and Environment of the Sinian Doushantuo Formation in Jiangkou,Guizhou Province;贵州江口震旦系陡山沱组沉积层序和沉积环境分析
4)Liantuo Formation莲沱组
1.On the correlation between the Liantuo Formation of the Yangtze Gorge and the Banxi Group of Hunan;对峡东莲沱组与湖南板溪群对比问题的一点浅见
2.Chemical Index of Alteration(CIA)values of argillites,from the middle and upper parts of the Liantuo Formation exposed in Yichang region,Hubei province,range from 60 to 70,suggesting that they were deposited under frigid climate.湖北宜昌地区出露的莲沱组中上部细屑岩的化学蚀变指数(CLA)介于60~70之间,表明是在寒冷干燥的气候条件下沉积的。
5)Nantuo Formation南沱组
1.The glacigenous rocks from the Sinian Nantuo Formation in the Xiushui district, Jiangxi;江西修水地区震旦系南沱组冰成岩研究
6)water quality of Tuojiang Ricer沱江水质
延伸阅读

水井水井well在地层中凿孔洞或埋设管筒汲取地下水的建筑物。是开采地下水的主要形式。按井管(筒)是否穿透整个含水层分为完整井和非完整井。按井深分为浅井、中深井和深井。当水井开凿在承压含水层中,而承压水头又高于地面时称承压井或自流井。按结构主要分为:①管井。井径较小,井深较大,以金属、塑料或混凝土等井管加固井壁的井型,也是使用最广泛的井型。因其一般以机械施工建成,以水泵抽水,故常称机井。其结构自上而下为:为安全方便地与水泵或泵管联接,并保护井口,避免污物、杂物掉入水井而修建的井头;严密封闭非开采段的井壁管,又称井身;在含水层开采段中安装的滤水管;沉淀井内沙粒的沉淀管。②筒井。井径较大,井深较浅,用于开采浅层地下水的井型,也是最古老的井型。多用人工开挖,结构为井头、井筒、进水部分和沉沙部分,多以砖石砌筑或用混凝土管修建。筒井和管井并无严格区别。中国于1986年颁布的《机井技术规范》已不使用筒井一词。③大口井。井径一般在2~8米,井深不超过20米的井型。④辐射井。由垂直集水井和沿集水井辐射分布的水平集水管(辐射管)构成。辐射管多用穿孔的钢管或竹管等。此井型特别适用于富水性差的粉细砂含水层、黄土含水层或粘土裂隙含水层。