本文给出了在鄂尔多斯地区碳酸盐岩地层中的应用实例。
This paper gives the example of the technique applied to carbonate formations in the Ordos area.
本文用模型实验研究了声波在致密碳酸盐岩地层井中的传播特性。
The propagation characteristic of acoustic wave in borehole that penetrates compact carbonate formation is analysed by doing model experiment.
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).
与砂泥岩地层相比，碳酸盐岩地层常以高电阻率、深浅双侧向大幅度差异为特征。
Carbonate formation is characterized by higher resistivity and bigger difference of Dual and Shallow lateral logging compared with clastic formation.
通过在塔里木盆地奥陶系碳酸盐岩地层中的应用表明，该方法具有较好的应用效果。
This method has been applied in the Ordovician carbonate reservoir located in the middle of the Tarim Basin of China with good results.
分布特点是：（1）与碳酸盐岩地层的分布相一致，是强岩溶化地区或剧烈水土流失区；
Its characteristics are: (1) Distributing in the region of Carbonate rock, where karst intensively develops and loss of water and soil erosion happens acutely;
酸化压裂是低渗透碳酸盐岩地层进行增产改造的一项重要措施，酸液向地层大量滤失受多种因素控制。
The acid fracturing is an important measure which increases the output of the low-permeability carbonate formation. The leaking into reservoir of acid is controlled by many factors.
本文还对碳酸盐岩地层的核磁共振测井响应特征进行了分析：核磁共振测井对裂缝响应不明显，对孔洞的响应较明显。
An analysis of characteristics of NMR logging response of the formation of carbonate rocks shows that the influence of NMR logging on crack response is less apparent than that of cavern response.
伊朗盆地第三系地层沉积了巨厚的碳酸盐岩，且分布广泛。
The Tertiary stratum of Iran basin has thickly and broadly deposited great carbonate sediments.
为提高碳酸盐岩地区地层规律性认识提供了经验。
Providing experience for rising strata regularity recognition in carbonate area.
鄂尔多斯盆地中部大气田是发育在奥陶系顶碳酸盐岩古风化壳中的地层油气藏。
The giant central gas field in E′erduosi Basin is a stratigraphic gas reservoirs developed in the ancient weathered crust of carbonate rocks on the top of the Ordovician.
碳酸盐岩台地广泛发育及其淹没事件是南海新生代地层的重要特征之一。
Development of Cenozoic carbonate platforms is one of the most spectacular stratigraphic features in the South China Sea.
烃源岩—地层水相互作用生成的有机酸促使烃源岩中矿物、特别是碳酸盐矿物溶解。
The interaction of hydrocarbon source rocks and formation water produces organic acid that can dissolve minerals, especially carbonate minerals.
四川盆地侏罗纪的湖相碳酸盐岩主要分布于早侏罗世自流井组地层之中。
The lacustrine carbonates mainly distribute in the early Jurassic Ziliujing Formation in the Sichuan basin.
充分考虑到碳酸盐岩剖面孔隙性地层和裂缝性地层中岩石抗张强度对地层破裂的影响，建立了地层破裂压力测井计算模型。
The effects that the rock tensile strength is in pore formation and the fracture formation are sufficiently considered, the formation fracture pressure is established.
辽河盆地曙光古潜山以碳酸盐岩和砂页岩为主的古潜山地层一直划归到中、新元古界。
The strata with carbonate rock, sandstone and shale in Shuguang buried hills of Liaohe basin were considered as Mesoproterozoic and Neoproterozoic.
利用层序地层学研究可将碳酸盐岩储层分为层序内部储层和层序界面储层。
Carbonate reservoirs can be divided into intra-sequence reservoirs and sequence boundary reservoirs based on study of sequence stratigraphy.
据角砾灰岩的岩石学特征及其与围岩地层的组合关系，该角砾岩主要属岩屑流和浊流沉积的深水碳酸盐岩。
According to their petrological characteristics and relations with surrounding rocks, we can regard them as deep water carbonate rocks of the debris flow and turbidity current sediments.
该方法应用于辽河盆地大民屯凹陷变质岩和碳酸盐岩潜山地层流体类型识别，效果良好。
The method were applied to fluid type identification of metamorphics and carbonate reservoirs of Liaohe Basin, and obvious geological effect was obtained.
中生代晚期地温梯度高，是古生界碳酸盐岩及煤系地层的主要生气期和运移期。
The Late Mesozoic characterized by higher temperature gradient is main period of gas generation and migration of Paleozoic coal series and carbonates.
在压力梯度悬殊的碳酸盐岩破碎地层中钻井，井漏是损失钻机月的重要因素。
Drilling a well in the broken carbonate strata where the pressure gradient is widely different, lost circulation is an important factor that makes the rig time losed.
碳酸盐岩台地广泛发育及其淹没事件是扬子地区晚奥陶世地层的重要特征之一。
The drowning of the carbonate platform is one of the most spectacular geological processes in the Late Ordovician on Yangtze block.
研究表明该夕卡岩的主要特征为：（1）呈层状、似层状赋存于碳酸盐岩和细碎屑岩接触带，产状与地层一致；
The main characteristics of the skarn are as follows:(1)occurring as bedded, para-bedded in the contact zone between carbonate and microclastic rock, and its occurrence being accordance to the strata;
早奥陶世马家沟期，在鄂尔多斯东部的陕北地区沉积了近千米厚的碳酸盐岩-蒸发岩地层。
During the Early Ordovician, a suit of carbonate-evaporites had deposited in the east part of the Ordos, which is now known as the Majiagou Formation and up to approximately 1000 meters in thickness.
早奥陶世马家沟期，在鄂尔多斯东部的陕北地区沉积了近千米厚的碳酸盐岩-蒸发岩地层。
During the Early Ordovician, a suit of carbonate-evaporites had deposited in the east part of the Ordos, which is now known as the Majiagou Formation and up to approximately 1000 meters in thickness.
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