carbonate reservoir rock 中文意思是什麼

carbonate reservoir rock 解釋
碳酸鹽儲集巖
  • carbonate : vt. 1. 使與碳酸化合；給…充碳酸氣。2. 使碳化，使化合成碳酸鹽[脂]；把…燒成炭。3. 使活潑[活躍]。n. 碳酸鹽[脂]；黑金剛石。
  • reservoir : n. 1. 貯藏所；貯氣筒；貯水池，水庫；貯水槽，水槽；貯存器；貯油器，油筒，油箱；貯墨管；【解剖學】貯液囊。2. （知識、精力等的）貯藏，蓄積。vt. 貯藏；在…設貯藏所[貯水槽]。
  • rock : n 1 巖，巖石，磐石，巖壁；卵石；〈常 pl 〉〈美口〉石子兒；暗礁，巖礁。2 〈the R 〉直布羅陀 （Gibr...
  1. The rock types comprise the delta front subfacies subaqueous distributary channel, channel - mouth bar and distal bar microfacies, and delta plain subfacies subaerial distributary channel microfacies sandstones and siltstones. as for the reservoir quality, the subaqueous ( subaerial ) distributary microfacies channel sandstones are the first, the channel - mouth bar microfacies sandstones come second, the distal bar microfacies sandstones is the third, and the last one is the interdistributary bay microfacies sandstones. the intense compaction, pressure solution and late carbonate cementation are responsible for the reduction of the porosity and permeability of the reservoir rocks

    三角洲前緣水下分流河道、河口砂壩、遠砂壩及三角洲平原水上分流河道微相決定了儲集巖的發育，分佈及原始物性條件；水下（上）分流河道微相砂體厚度大、物性和孔隙結構好，次之為河口砂壩微相砂體，遠砂壩微相砂體儲集性較差，而分流伺灣微相砂體物性和孔隙結構最差。
  2. The favorable reservoir spaces in the carbonate rock could be divided into five types according to their origin, configuration and size, i. e., solution fissure, solution hole, cave, erosional fissure and structural fissure, which form five different reservoirs including cave - type reservoir, erosional fracture reservoir, structural fissure reservoir, and solution pore marginal beach grainstone reservoir

    而下奧陶統灰巖段儲集和生產油氣的有效儲滲空間按成因、形態及大小可劃分為溶蝕孔隙、溶蝕孔洞、大型洞穴、風化裂隙、構造裂隙等5類，構成5種性質有別的儲層，即洞穴型儲層、風化裂隙型儲層、構造裂隙型儲層、臺緣灘相顆粒灰巖溶蝕孔隙型儲層和地表殘積物裂隙孔隙（洞）型儲層。
  3. Tianjin is located at north part of northern china plain, where is rich in thermal water in sedimentary basin. the main reservoir is carbonate rocks of the paleozoic and upper and middle proterozoic group, which contain thermal waters with temperature of more than 90. the cap rock is cenozoic sedimentary rocks with thickness of more than 1000m, which contains thermal water with temperature from 25 to 70 in 13 sandstone layers. the temperature of thermal water is steady growth along with the deepen of basin. all thermal waters in different aquifers are medical mineral waters, which is conducive to good health

    天津位於華北平原的北部，那裡的沉積盆地含有豐富的地下熱水。主要的熱儲層為古生界和上中元古界的碳酸鹽巖層，所含熱水的溫度略高於90蓋巖層為新生界沉積層，在13個砂巖含水層中含有2570的熱水。熱水的溫度隨盆地深度的增加而增加。
  4. After synthetic evaluation to the permian reservoir, it was considered that there were deep lake facie in mazhong - heidun - shibandun structure zone, it was suitable to depositing thick carbonate rock. these cracks were developed in the zones where the stress was concentrated. these zones are fairly good oil and gas exploration areas.

    對三塘湖盆地二疊系儲層進行綜合評價后，認為：該區馬中?黑墩?石板墩一帶屬半深湖沉積亞相，有利於碳酸鹽巖的沉積，儲集體沉積比較厚，並且此帶屬于應力集中的變形強烈帶，故裂縫較發育，從而成為最有利油氣勘探區，其次有利區為牛圈湖構造帶，這主要是由牛圈湖地區的顆粒溶孔較發育所致。
  5. The hydrological condition of danjiang reservoir is very complex, where carbonate rock distribute in the canyon areas, and a series of funnels are formed

    丹庫區水文地質條件復雜，在峽谷庫段，碳酸鹽類巖石裸露，巖溶裂隙水活動形成一系列落水洞、漏斗和溶洞。
  6. The reservoir types in lucaogou formation is carbonate rock, clastic rock and tuff, while the reservoir types in tiaohu formation is mainly tuff and volcanic rock

    蘆草溝組儲層巖石類型主要有碳酸鹽巖、碎屑巖及沉凝灰巖，而條湖組則主要為火山巖和沉凝灰巖。
  7. Some conclusions have been made in the following. that the value of toc is 0. 2 % may be regarded the low evaluation value of marine carbonate souce rock at the stage of high to over mature. according to the content of bitumen in source rock and reservoir, gas generation quantity, the maximum absorption gas quantity and geology analogy

    通過對儲層和烴源巖中瀝青定量統計分析、烴源巖生氣熱模擬、最大吸附氣實驗測定及地質類比法等綜合研究認為在鄂爾多斯盆地有機碳為0 . 2可作為高?過成熟的海相碳酸鹽巖有機碳下限標準。
  8. The carbonate reservoir rock includes many influence factors that it is through many phases structure bursts and the ancient karst to act on jointly the formation and with which the rock karst gives first place. the complicated oil field of karst cave and crack are controlled by limestone reservoir and the crevices - cave system, which have many characteristics such as vivid and great in style, irregular distribution, the limestone cave in crack and unhomogeneity of rock etc. these kinds of reservoir belong to a world difficult and extreme problem on valuation and cognition

    它是經多期構造破裂與古風化巖溶共同作用形成的、以灰巖巖溶為主控因素、以儲集體控藏和縫洞系統控藏為主的溶洞?裂縫型復雜油氣藏，表現為其不規則形態和不均勻分佈、裂縫溶洞發育不均一、儲層非均質性極強等特點，認識和評價該類儲層屬世界性難題。
  9. In view of the main feature of strong anisotropism of reservoir stratum of the paleozoic era carbonate rock in the middle part of ortos basin gas field, mainly by means of random analog formation, this paper makes a quantitative tranformation on the geological study on the area and the descriptive results of the gas pool, and finishes the whole geological model of underground carbonate rock in ortos basin, including the structure model / phy - sical model and fluid distribution model

    摘要針對鄂爾多斯盆地中部氣田下古碳酸鹽巖儲層非均質性強的主要矛盾，以隨機模擬建摸為主要方法，對該區地質研究和氣藏描述成果進行定量化轉變，形成了包括構造模型、物性模型和流體分佈模型的鄂爾多斯盆地下古碳酸鹽巖整體地質模型。
  10. The author makes effort to the dynamic information in development, exploring the method to study and appraises the characteristic on carbonate rock. the major research is as follows. ( 1 ) combining tahe oil field information of static and dynamic state analysis and the practice, carbonate rock oil reservoir dividing making up the model for three kinds : crevices - cave system, double - crack system and crevices - pore system

    筆者力求充分利用各種開發生產的動態信息，探索研究和評價儲層特徵的方法及思路，主要研究成果如下： （ 1 ）結合塔河油田動靜態分析和實踐，將縫洞型碳酸鹽巖油藏劃分為三類組合模型：縫?洞系統、雙裂縫系統和縫孔系統。
  11. Ordovician carbonate rock bed of ordovician reservoir in qianmiqiao buried hill experienced two times of karst exposure and the post plaeogene deep - buried diagenesis

    摘要千米橋潛山奧陶系儲層經歷了兩次裸露巖溶及古近紀后的深埋藏成巖作用。
  12. Volcanic rock is quite different from sandstone and carbonate rock in diagenetic model, petrology and reservoir characterization

    火山巖在成巖模式、巖石學和儲集層特徵上，與砂巖、碳酸鹽巖有很大區別。
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