上奥陶统,Upper Ordovician
1)Upper Ordovician上奥陶统
1.Hydrocarbon Expulsion History of Middle-Upper Ordovician Source Rocks in Tarim Basin;塔里木盆地台盆区中上奥陶统烃源岩排烃史
2.Genesis of the Guanyinqiao Member of Upper Ordovician Wufeng Formation in southern China:"Shallow water shelly facies" or deep-water allogenic deposition?;中国南方上奥陶统五峰组观音桥段成因讨论:是“浅水介壳相”,还是深水异地沉积?
3.Reservoir types and favorable oil-gas exploration zone prediction of the Upper Ordovician Lianglitage Formation in Tazhong No.1 fault belt of Tarim Basin;塔里木盆地塔中地区Ⅰ号断裂带上奥陶统良里塔格组储集层类型及有利区带预测
英文短句/例句

1.CONTACTINC RELATIONSHIP BETWEEN THE UPPER一AND MIDDLE ORDOVICIAN SEQUENCES TO THE SOUTH OF XINGDI FAULT IN KULUKTAK AREA,XINJIANG库鲁克塔格地区兴地断裂以南中奥陶统与上奥陶统的接触关系
2.UPPER ORDOVICIAN CONODONTS FROM THE CENTRAL HIGH,TARIM BLOCK,NW CHINA塔里木中央隆起区上奥陶统的牙形刺
3.THE CHARACTERISTICS AND EVALUATION OF MIDDLE & UPPER ORDOVICIAN REEF & SHOAL RELELATED CARBONATE RESERVOIR IN TAZHONG NORTH SLOPE, TARIM BASIN塔中中上奥陶统礁、滩相储层的特征及评价
4.Sedimentary environment analysis of Sangtamu Formation of Upper Ordovician in the south of Tarim River,Xinjiang,China塔河南上奥陶统桑塔木组沉积环境分析
5.INTERNAL-TIDE DEPOSITS OF THE MIDDLE AND UPPER ORDOVICIAN IN WELL TZ 32, TARIM BASIN塔里木盆地塔中32井中上奥陶统内潮汐沉积
6.THE SEDIMENTARY AND PALAEOGEOGRAPHIC CHARACTERISTICS OF THE UPPER ORDOVICIAN IN THE TARIM BASIN塔里木盆地上奥陶统沉积及古地理特征
7.STUDY ON THE MIDDLE-UPPER ORDOVICIAN SUBTLE TRAPS OF REEF-BEACH FACIES IN TAZHONG AREA塔中地区中上奥陶统礁、滩相隐蔽圈闭研究
8.An Analysis of Sedimentary Environment of Jiancaogou Formation of Upper Ordovician Series in Northern Guizhou and Its Adjacent Areas黔北及邻区上奥陶统涧草沟组沉积环境分析
9.SOME UPPER ORDOVICIAN GRAPTOLITES FROM SOUTHERN ANHUI WITH COMMENTS ON THE GENUS AMPLEXOGRAPTUS ELLES ET WOOD安徽南部上奥陶统的笔石并论围笔石属
10.Research on Upper Ordovician Reservoir Characteristics of Reef Bank in Tazhong62 Well Area;塔中62井区上奥陶统礁滩体储层特征研究
11.The Depostional Facies and Facies Models of the Middle-Upper Ordovician Carbonate Rocks in the Southern Margin of Taibei Uplift, Tarim Basin;塔北南缘中、上奥陶统碳酸盐岩沉积相及相模式
12.Analysis on Seismic Facies of Middle and Upper Ordovician of Tanggubasi Sag,Tarim Basin塔里木塘古巴斯坳陷及中上奥陶统地震相分析
13.ONCOLITES FROM THE LIANGLITAG FORMATION(KAITIAN,UPPER ORDOVICIAN),TAZHONG,TARIM BLOCK,NW CHINA塔里木板块塔中上奥陶统良里塔格组的核形石
14.Study on Category and Forming Environment of Upper Ordovician Carbonate Rock Calcite Cement in Tazhong District塔中上奥陶统方解石胶结物类型及其形成环境
15.Palaeo-environment restoration of Upper Ordovician-Lower Silurian hydrocarbon source rock in Middle-Upper Yangtze area中上扬子地区上奥陶统—下志留统烃源岩发育的古环境恢复
16.Discovery of distal calcareous tempestites of upper ordovician age from Tianzhu, Gansu甘肃天祝斜壕地区上奥陶统远源钙质风暴岩的发现
17.ORDOVICIAN CONODONTS FROM KALPIN OF XINJIANG AND PINGLIANG OF GANSU ACROSS THE BASE OF UPPER ORDOVICIAN SERIES新疆柯坪和甘肃平凉上奥陶统底部附近的牙形刺(英文)
18.Research on Deposition Characteristics and Sedimentary Facies of Upper Ordovician Reef-beech Complex in TaZhong 24-82 Well Areas;塔中24-82井区上奥陶统礁滩体沉积特征及沉积相分布研究
相关短句/例句

Middle and Upper Ordovician中上奥陶统
1.Analysis on Seismic Facies of Middle and Upper Ordovician of Tanggubasi Sag,Tarim Basin塔里木塘古巴斯坳陷及中上奥陶统地震相分析
2.The margin of the carbonate platform of the Middle and Upper Ordovician, Tazhong area, Tarim Basin is characterized by a well-developed rimmed depositional system which consists of various types of grain banks and organic reefs.塔里木盆地塔中地区中上奥陶统碳酸盐岩台地边缘以发育良好的多种粒屑滩和生物礁组成的镶边沉积体系为特征。
3)Upper Ordovician Yuqian Formation上奥陶统于潜组
1.The Upper Ordovician Yuqian Formation, a rhythmic unit composed of silty to fine sandstones and mudstones with different thickness, is widely developed in the aera from Lingan to Jiande in western Zhejiang Province.在概述了浙江西部上奥陶统于潜组的沉积学特征,并进而描述了发现的14个遗迹化石属基础上,从4个方面对Spirodesmos为代表的遗迹组合进行了环境分析:(1)14个遗迹属中仅3个属为穿相型分子,其余占遗迹总属2/3以上的遗迹化石均为典型的深水型分子,它们都是Nereites遗迹相的主要成员,因此该遗迹组合可归属于深海Nereites遗迹相中;(2)大部分遗迹化石呈复杂规则弯曲的形态,这种形态的遗迹化石是深海环境的遗迹化石标志;(3)14个遗迹属均为觅食迹和牧食迹,它们的行为习性,尤其是牧食迹主要分布于深海环境;(4)多数遗迹属的水深分布均在200m以下。
4)Upper Cambrian-Lower Ordovician上寒武统-下奥陶统
5)Upper Ordovician-Lower Silurian上奥陶统-下志留统
6)Upper-Ordovician to Silurian上奥陶统一志留系
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统汉峰下(一作过降户至统漠烽)【诗文】:统汉峰西降户营,黄河战骨拥长城。只今已勒燕然石,北地无人空月明。【注释】:【出处】:全唐诗:卷283_89