Oolitic dolostone is a vital type of carbonate reservoirs.
鲕粒灰岩是重要的碳酸盐岩油气储层。
Petrologic and geochemical features of these four kinds of dolostone are generalized.
总结了四种不同成因的白云岩的岩石特征及地球化学特征。
The vugs-filling degree and types control the reservoir quality of dolostone reservoirs.
溶蚀孔洞的充填程度和充填类型明显地控制着储层的储集性。
Siliceous dolostone, lime dolostone, moyite and volcanic detrital rocks are the mainhostrocks of the mineral water.
本矿泉水赋存岩石为硅质白云岩、灰质白云岩、钾长花岗岩和火山碎屑岩。
In light colour dolostone abound with carbonification blackly non-stromatolite ecologic system cyanobacteria dolostone.
在浅色白云岩地层中富含炭化的黑色非叠层石生态系兰细菌白云岩。
The gas of central gas field of Shan-Gan-Ning basin is produced from paleo-weathered crust dolostone reserviors of Majiagou formation on top Ordovician.
陕甘宁盆地中部气田的天然气产于奥陶系顶部古风化亮马家沟组白云岩储层中，储集空间的形成是不同期次溶蚀作用和充填作用相互作用的结果。
In the same conditions of temperature, pressure and specific surface area, the start - up dissolution velocity of limestone sample is more than the dolostone 's one.
在相同温压、相同比表面积的条件下，灰岩类岩石样品的启动溶蚀速率大于白云岩类岩石样品的启动溶蚀速率。
In this paper, the straticulate dolostone and spatulate dolostone in Lower Ordovician strata of Well Tazhong 1 were studied using petrologic and geochemical methods.
本文选择塔中地区塔中1井下奥陶统藻纹层白云岩与夹层竹叶状白云岩作为对象，应用岩石学与地球化学方法对其成因问题进行了研究。
Limestone deposited in the whole inner shelf basin, including the swell belt, excepting a small mass of dolostone or dolomitic limestone could deposit in the center of basin.
包括隆起带上，仅（内）陆架盆地风暴浪基面之下中心位置有少量灰质白云岩和白云岩沉积。
In addition, dissolution of grain dolostone also occurs and shows the characteristics of hypergene dissolution in some places, which may contribute to the development of reservoir space.
另外，局部可见颗粒白云岩发生溶蚀，有些地方具有表生溶蚀作用的特点，对白云岩储集空间的发育有一定贡献。
In addition, dissolution of grain dolostone also occurs and shows the characteristics of hypergene dissolution in some places, which may contribute to the development of reservoir space.
另外，局部可见颗粒白云岩发生溶蚀，有些地方具有表生溶蚀作用的特点，对白云岩储集空间的发育有一定贡献。
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