威远震旦系白云岩层是年代老、结构复杂的储集层。
The sinian dolomite in Weiyuan is an old reservoir rock of complex structure.
威远震旦系气藏为块状含水，储层是裂缝-洞孔型。
The Senian pool in weiyuan gas field is a large massive one with water, it is fracture-vug and pore type.
上震旦统灯影组前震旦系康定群是本区有利矿源层。
The favorable source beds in this district are Presinian Kangding Group and DengyingFormation of upper Sinian series.
冕宁西部是康滇地区前震旦系出露较集中的地段之一。
The Pre-Sinian Darezha Formation is widely exposed in west Mianning.
其层序，岩性岩相特征均可与湘潭锰矿地区震旦系对比。
Its stratigraphic sequence, lithology and sedimentary facies can be correlated to the Sinian System in Xiangtan manganese mine area.
在中国东部广泛发育一套巨厚碳酸盐岩地层（震旦系至三迭系）。
Widespread in East China is a suite of well-developed and very thick carbonate formations(from Sinian to Triassic).
金沙厂铅锌矿床是赋存于震旦系灯影组中的密西西比河谷型矿床。
The Jinshachang Pb-Zn deposit occurs in Dengying Formation (Sinian), belonging to Mississippi valley type.
下构造层由震旦系—泥盆系构成，所谓阿-满低梁主要即发育于该构造层。
The lower structure layer consists of the Sinian to the Devonian, in which the A-Man low ridge is observed.
同时，威远寒武系洗象池群后期的震旦系穿层井也证实该地质模型的正确性。
At the same time, the validity of this geological model had been approved by the new wells penetrated Cambrian Xixiangchi Group of Weiyuan Structure.
本文简要地回顾了威远震旦系气藏发现之后对其它构造震旦系进行勘探的历史。
This paper briefly reviews the exploration history of Sinian gas pool in a number of structures since Wei - yuan gas field was found.
出露地层为震旦系、泥盆系、二叠系、三叠系以及侵入的花岗岩脉和花岗伟晶岩脉。
Emergence stratums are of Sinian, Devonian, Permian, Trias and intrusive granite dike and coarse - grained granite dike.
库鲁克·塔格地区震旦系发育三层冰碛岩，分别是贝义西组、特瑞爱肯组、汉格尔·乔克组。
Three layers of tillites are developed in the Beiyixi formation, Teriaikan formation and Hangeerqiaoke formation of the Neoproterozoic in Quruqtagh region.
本文在简述震旦系沉积概况的基础上，对川西南震旦系灯影组的生、储、盖层条件进行了分析。
Based on briefly describing the general situation of Sinian depositions, the conditions of source bed, reservoir and capping rock of Dengying Formation.
本文运用现代沉积学和地层学理论，对区内震旦系岩石地层进行了基本层序研究与沉积环境分析。
On the basis of modern theory of sedimentology and stratigraphy, the paper analyses the stratigraphic sequence and sedimentary environment of Sinian system in the area.
在分析变质岩的含金性及地球化学性质的基础上，认为与金成矿有关的主要元素均源自前震旦系。
Based on analysis of auriferous and geochemical properties of the meta morphic rocks, the authors hold that the major elements related to gold mineralization were derived from the Pre-Sinian System.
震旦系—志留系是川东南地区油气勘探的新层系、新领域，具有较好的勘探前景，但勘探程度极低。
The strata from Sinian to Silurian system are new formations and fields with better exploration potential in southeast area in Sichuan province, but the degree of prospecting is quite low.
结果表明，震旦系-下古生界(下组合)主要为一套浅海陆棚相碎屑岩与台地相碳酸盐岩沉积序列。
The results indicate that there mainly develop a set of shallow Marine shelf clastic sedimentary rocks and platform carbonate rocks during the Sinian-Lower Paleozoic (Lower Assemblage) period.
矿床赋存于震旦系C组地层中，中型规模，矿床类型为岩浆作用形成的白云母钠长石伟晶岩铌钽矿床。
It is hosted in the stratum of the group C of the Sinian system. Its deposit type belongs to the Niobium-Ta...
碧口韧性剪切带沿康县—碾坝—麻子坝一带呈连续带状展布，发育于泥盆系及震旦系关家沟组上岩段内部。
Bikou ductile shear zone distributing along Kangxian county-Nianba-Maziba developed in the Devonian System and the upper Guanjiagou Formation of Sinian System.
两组微古植物各具特色，但也存在一些共同分子，表现为连续演化的特点，说明震旦系和寒武系的沉积是连续的。
The microfossil plants of the two formations have their own peculiarities, but have some common elements too. This shows that the deposition of the Sinian and Cambrian were continuous.
两组微古植物各具特色，但也存在一些共同分子，表现为连续演化的特点，说明震旦系和寒武系的沉积是连续的。
The microfossil plants of the two formations have their own peculiarities, but have some common elements too. This shows that the deposition of the Sinian and Cambrian were c...
本文采用GC＿MS、ICP＿MS、形态硫分析、硫同位素、物相分析等方法综合研究了湘西晚震旦世-早寒武世黑色岩系的地球化学特征和形成条件。
This paper deals with the formation conditions of black shales based on such analytical techniques as ICP_MS, GC_MS, isotope, organic carbon, element facies and micropetrology.
盆地周围为前震旦纪变质岩系及古生代灰岩、页岩组成的高丘、低山。
Of, belonging to, or being the geologic time, system of rocks, and sedimentary deposits of the sixth period of the Paleozoic Era, characterized by the development of coal-bearing rock formations.
库鲁克·塔格震旦纪火山岩构成一个典型的双峰值火山岩系，主要由酸性火山岩与基性火山岩组成，缺少中酸性火山岩。
The Sinian volcanics are typical bimodal volcanic rocks in Kuruktag area, which are consisted of acidic and basic volcanic rocks but with rare medium acidic one.
其中海相地层中的主力烃源岩层为上震旦统和上古生界石炭—二叠系。
The stratum of main source rock among the Marine facies is the upper Sinian and the Paleozoic group.
其中海相地层中的主力烃源岩层为上震旦统和上古生界石炭—二叠系。
The stratum of main source rock among the Marine facies is the upper Sinian and the Paleozoic group.
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