The Lower Paleozoic reservoir mainly by corrosion pore, intercrystalline pore and the crack are composed.
下古生界储层主要由晶间孔、溶孔和裂缝组成。
The forming mechanism of dolomite reservoir space of Lower Paleozoic in Zhuanghai region, Jiyang Depression;
在侏罗系的中统和上统下部广泛发育白云岩 ，并构成最具潜力的油气储层。
The Lower Paleozoic reservoir is Majiagou formation's putty crystal dolomite and powder crystal dolomite primarily.
下古生界储层主要以马家沟组的泥晶白云岩和粉晶白云岩为主。
The Lower Paleozoic carbonates of Tarim Basin were marbleized locally due to the thermal effects of magma intrusions.
在岩浆侵入体热作用下，塔里木盆地下古生界碳酸盐岩局部发生了大理岩化作用。
Limestone and dolomite in North Chinamainly occur in the Lower Paleozoic and those in South China in the Devonian - Triassic.
灰岩、白云岩在华北主要产于下古生界，在华南主要产于泥盆系-三叠系。
Abstract: the Lower Paleozoic carbonates of Tarim Basin were marbleized locally due to the thermal effects of magma intrusions.
摘要：在岩浆侵入体热作用下，塔里木盆地下古生界碳酸盐岩局部发生了大理岩化作用。
In plane view, the fractures and vuggs in the Lower Paleozoic carbonate reservoirs are in zonal distribution in the study area.
进而认识到，平面上桩海地区下古生界碳酸盐岩储层缝洞分布呈条带状。
Based on a description and clasification of the hydraulic fracturing in the Lower Paleozoic strata in Xiushui, Jiangxi, and on an.
本文简要阐述了水力破裂的基本原理和工作方法。
The sources of the Lower Paleozoic natural gases in central gas field in Erdos are an important problem that has not been resolved by now.
鄂尔多斯中部气田下古生界天然气藏的气源是目前尚未解决的重要问题。
The reservoir type is Ordovician weathering crust in the Lower Paleozoic, and the main gas layer is in the fifth member of Majiagou Formation.
储集层类型为下古生界奥陶系古风化壳型，其主力含气层为马家沟组第五段。
The content and the distributing law of the microelements in lower Paleozoic era stone coal in South Qinling have been systematically studied.
对南秦岭早古生代石煤的微量元素含量、分布规律等进行了详细系统的研究。
The main structure of Futai oilfield is composed of the Lower Paleozoic Chegu 20 buried hill and the overlying Eogene Che 3 nose-like structure.
富台油气田的主体构造由下古生界车古20潜山和其上覆的下第三系车3鼻状构造两部分组成。
Reservoir rocks of lower Paleozoic mainly include dolomite and limestone; reservoir rocks of upper Paleozoic mainly include sandstone reservoir.
下古生界白云岩和灰岩为主要的储集岩类，上古生界则主要以砂岩储层为主。
Unconformity between the Upper and Lower Paleozoic is absent from Leping of Jiangxi all the way upward, on the southeastern margin of the Yangtze platform.
扬子(地台)东南缘，自江西乐平向北一直缺少上、下古生界之间角度不整合接触关系的报道。
The former is a continuing preserving unit, beneficial to hydrocarbon preservation, which is the target area for the Lower Paleozoic oil & gas exploration.
前者属持续型保存单元，为有利的油气保存单元，是下古生界油气勘探的目标区。
The scheelite orebody of the Yangjingou mining area occurred in the contact zone of the lower Paleozoic Wudaogou Group strata and the Indo-Sinian adamellite.
杨金沟矿区白钨矿体产于下古生界五道沟群地层与印支期二长花岗岩内外接触带中。
Nowadays, at the western slope and the northern and southern uplifts the Lower Paleozoic source formations are still in the active oil generation Rold ( R o< 1.3%).
下古生界烃源岩在西部坡折带及南北隆起区现今仍处于有效生油窗内（镜质组反射率小于1.3 % ）。
In the southern North China, the lower Paleozoic source rocks reached primary maturation at late Triassic and the secondary hydrocarbon generation did not occur at the Cenozoic.
南华北地区下古生界烃源岩在晚三叠世达到早成熟阶段，新生代基本未发生二次生烃作用。
However, the previous sequence stratigraphic division of the Lower Paleozoic carbonates is not suitable for target selection and development strategy optimization, influencing production.
然而按照经典模式划分的碳酸盐岩层序，在生产中与目标优选及开发方式结合并不紧密，进而影响了实际生产。
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.
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。
Generally, the basin is a superimposed basin formed by foreland depression of the Late Paleozoic in the lower, and the piedmont depression of the Meso-Cenozoic in the upper.
它是由晚古生代前陆坳陷和中新生代山前拗陷迭加而成的复合型盆地。
Vertically, 3sets of source rocks including the Lower Cambrian, the Middle-o-Upper Ordovician-Lower Silurian and the Permian were developed in Chinese Paleozoic Marine basins.
研究认为中国古生代海相盆地在纵向上主要发育下寒武统、中上奥陶统—下志留统和二叠系3套烃源岩。
Vertically, 3sets of source rocks including the Lower Cambrian, the Middle-o-Upper Ordovician-Lower Silurian and the Permian were developed in Chinese Paleozoic Marine basins.
研究认为中国古生代海相盆地在纵向上主要发育下寒武统、中上奥陶统—下志留统和二叠系3套烃源岩。
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