儲油巖 的英文怎麼說

中文拼音 [chǔyóuyán]
儲油巖 英文
oil-saturated reservoir rock
  • : Ⅰ動詞(儲藏; 存放) store up; save; keep [have] in reserve Ⅱ名詞1. (繼承人) heir 2. (姓氏) a surname
  • : Ⅰ名詞1 (脂肪; 油脂) oil; fat; grease 2 (姓氏) a surname Ⅱ動詞1 (用桐油、油漆等塗抹) apply t...
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • 儲油 : oil storage
  1. The basins in west china were downfaulted depression basins in jurassic and cretaceous, and foreland basins in cenozoic. these basins formed not only marine facies source rocks ( oil type ) and reservoirs but also continental facies source rocks ( coal type and oil type ) and reservoirs

    因此,中國類前陸盆地基本石地質條件與國外富氣前陸盆地相比,除海相烴源的質量不及後者外,其它方面並無明顯不足,且具有發育陸相烴源的優勢。
  2. The result is that this gas pool has simple structure, only forms a little nose - like structure at the district of fenghuangshan ; this pool belongs to delta front sub - facies sedimentary model, the underwater distributary channel and mouth bar is the better sedimentary microfacies ; the physical property of the reservoir is poor, the type of pore of the reservoir rock mostly are intergranular pore, intergranular solution hole and little are intercrystalline micropore ; the influential factors of pore structure and physical property are lithofacies, lithologic character and diagenesis ; the off - take potentia of all the testing well are deadly shortness, the wells have the worth of industrial recovery only under the condition of going through sand fracturing, and in the early of binging into production, the oil and sheath pressure drop rapidly, the production of the well drop rapidly

    研究認為該氣藏構造簡單,只在鳳凰山形成了一個小型的鼻狀構造;屬於三角洲前緣亞相沉積模式,水下分流河道和河口壩是有利的沉積微相;層物性差,石的孔隙類型主要有粒間孔、粒間(內)溶孔及少量晶間微孔;影響蓬萊鎮組氣藏層孔隙結構及集性的因素有相、性條件及成作用;所有測試井自然產能都極低,必須經加砂壓裂后才有工業開采價值,且投產初期,套壓下降較快,氣井產量下降迅速。
  3. And the shaly sandstone is the primary type of hydrocarbon reservoirs now. so it is the completely necessary and very significative task to study permeability of shaly sandstone reservoirs

    並且泥質砂層是當今石的主要石的類型,因此研究泥質砂集層的滲透率是十分必要而且非常有意義的工作。
  4. Several analysis methods such as casting slice, scanning electron microscope, porosity and permeability data, mercury injection data and density of fissures are used to study the reservoir properties of volcanic rocks in huang - yu - re area, the east sag of liaohe basin. volcanic rocks in this area are mainly composed of basalt, diabase, tuff and trachyte. the dominating type of volcanic reservoir space includes secondary solution pores and structural fissures

    通過火山的常規物性分析壓汞分析和裂縫密度分析,結合鑄體薄片和掃描電鏡,研究了遼河田黃于熱地區的火山層物性特徵,認為該區火山石類型主要有玄武輝綠凝灰和粗面,主要集空間類型為次生的構造裂縫和溶蝕孔縫。
  5. Based on cores analyses of coring well, studied are the " four properties " ( i. e., lithology, physical property, conductivity and oil bearing ) relationships between conglomerate and glutenite formation ; set up are the logging interpretation models of porosity, permeability and oil saturation in conglomerate and glutenite reservoirs with different lithologies

    以取心井心分析為基礎,分別研究礫、砂礫石的性、物性、電性及含性兩兩之間的關系,建立了分性的礫和砂礫孔隙度、滲透率、含飽和度測井解釋模型。
  6. The course mainly introduce the profession standard of petroleum, which including the standard of petroleum geology survey and exploration work, the technical standard of basin research, the detailed rules of trap description, the standard of reservoir description, the technical standard of seismic data interpretation, the technical standard of test well geological work, the standard of oil - bearing rock system ' s classification and correlation, the standard of oil and gas reserves, the criterion of reservoir evaluation, the schedule standard of exploration project design and so on

    本課主要介紹石天然氣行業標準,包括石天然氣地質調查與勘探工作規范、盆地研究技術規范、圈閉描述工作細則、藏描述規范、地震資料解釋技術規范、探井地質工作技術規范、含系劃分與對比規范、石與天然氣量規范、層評價標準以及勘探項目設計編制規范等內容。
  7. Abstract : yanchang series is a typical low permeability reservoir, and its favourable sandstone reservoir is delta facies. heavy compaction, cementation and heterogeneity exist in it. according to the analysis of the main control factors of forming the secondary pore, it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure. it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism. organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure, and a lot of secondary pore is produced in the runners. from the present exploration result, it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure

    文摘:陜甘寧盆地三疊系延長統是國內外典型的低滲特低滲田,集層主要為三角洲砂體,壓實作用和膠結作用強烈,層非均質性非常嚴重,因此預測次生孔隙發育帶是尋找氣聚集帶的關鍵.通過對陜甘寧盆地隴東地區延長統次生孔隙形成的主控因素分析,認為陜甘寧盆地延長統次生孔隙的形成除了受沉積有利相帶控制外,還與地層異常壓力的作用密切相關.研究認為隴東地區異常壓力的形成機理主要由於成過程中粘土礦物脫水作用.粘土礦物大量脫水時間正好與有機質脫羧期相一致,從而在異常壓力作用下將生中的大量有機酸及co2帶到與之相鄰的集層中,並沿著有利集相帶運移,在酸性水經過的地方形成大量的次生孔隙,為後期氣運聚提供有利通道及宿住空間,從現今的勘探結果來看,通過研究地層異常壓力縱橫向分佈特徵,並結合有利相帶研究預測次生孔隙育良帶是行之有效的方法
  8. Yanchang series is a typical low permeability reservoir, and its favourable sandstone reservoir is delta facies. heavy compaction, cementation and heterogeneity exist in it. according to the analysis of the main control factors of forming the secondary pore, it is held that the secondary pore in longdong area is controlled by both favorable facies belt and abnormal formation pressure. it is also held that the formation of the abnormal formation pressure is due to the dewatering of the clay mineral during diagenesis because the dewatering time is identical with the decarboxylation time of organism. organic acid and co2 are driven to adjacent favorable reservoirs under the abnormal formation pressure, and a lot of secondary pore is produced in the runners. from the present exploration result, it is useful to predicting the development of secondary pore to study the distribution of abnormal formation pressure

    陜甘寧盆地三疊系延長統是國內外典型的低滲特低滲田,集層主要為三角洲砂體,壓實作用和膠結作用強烈,層非均質性非常嚴重,因此預測次生孔隙發育帶是尋找氣聚集帶的關鍵.通過對陜甘寧盆地隴東地區延長統次生孔隙形成的主控因素分析,認為陜甘寧盆地延長統次生孔隙的形成除了受沉積有利相帶控制外,還與地層異常壓力的作用密切相關.研究認為隴東地區異常壓力的形成機理主要由於成過程中粘土礦物脫水作用.粘土礦物大量脫水時間正好與有機質脫羧期相一致,從而在異常壓力作用下將生中的大量有機酸及co2帶到與之相鄰的集層中,並沿著有利集相帶運移,在酸性水經過的地方形成大量的次生孔隙,為後期氣運聚提供有利通道及宿住空間,從現今的勘探結果來看,通過研究地層異常壓力縱橫向分佈特徵,並結合有利相帶研究預測次生孔隙育良帶是行之有效的方法
  9. 5. platform trough and basin with deep water and low energy are the favorable source rock zones, reef banks and reef cores are the profitable reservoir. and the strata which is dolomitized is the main gas yielding parts

    5深水低能沉積的臺溝、盆地相是有利的生相帶,淺水高能的礁灘、礁核相是有利的層,產氣段主要是生物礁內的白雲段。
  10. Abstract : the petrologic characteristic and the pore types of y8 y10 reservoir are studied by x - ray diffraction method, the quantitative mineral clay analysis method and thin - section analysis method. based on the study, the mistakes are corrected in the naming of the sandstone and in the composition of the pore filling substance. the pore characteristic of the sandstone and the main factors of controlling the pore development are discussed

    文摘:利用x衍射全分析方法、粘土礦物定量分析方法和薄片鑒定等方法研究了城華地區延8 -延10石學特徵和孔隙成因類型.綜合論述了城華地區延8延10組不同層砂的基本特徵,糾正了砂定名的錯誤和主要填隙物成份的錯誤,同時還論述了層砂的孔隙特徵和控制孔隙發育的主要因素
  11. The petrologic characteristic and the pore types of y8 y10 reservoir are studied by x - ray diffraction method, the quantitative mineral clay analysis method and thin - section analysis method. based on the study, the mistakes are corrected in the naming of the sandstone and in the composition of the pore filling substance. the pore characteristic of the sandstone and the main factors of controlling the pore development are discussed

    利用x衍射全分析方法、粘土礦物定量分析方法和薄片鑒定等方法研究了城華地區延8 -延10石學特徵和孔隙成因類型.綜合論述了城華地區延8延10組不同層砂的基本特徵,糾正了砂定名的錯誤和主要填隙物成份的錯誤,同時還論述了層砂的孔隙特徵和控制孔隙發育的主要因素
  12. On the basis of the study of high resolution sequence stratigraphy, this paper discusses the reservoir petrology ' s diagenesis and secondary pore of the chang 4 + 52 ~ chang 62 pay zones in detail by using the methods of analysis of mercury injection, cast section, popular section, scanning electron microscope, x - ray diffraction and etc. the reservoir rock is mainly composed of feldspar fine sandstone, which is characterized by low compositional maturity and relatively high textural mature

    本文在高解析度層序地層學研究的基礎上,通過15口井的常規物性、壓汞、鑄體分析、薄片鑒定、掃描電鏡、 x光衍射、陰極發光、粒度分析等多項測試手段,對坪北田延長組長4 + 52長62石學、成作用及次生孔隙進行了詳細研究。
  13. It shows that oil and gas moves from source rock to reservoir rock in continuous phase

    研究認為,氣是以連續相的形式從源運移到的。
  14. Studies on the combination of source rocks and reservoirs show that yuejin - dongchaishan, dafengshan and the front part of arjinshan area are the most favourable areas for oil and gas accumulation

    根據生儲油巖疊置組合關系,指出阿爾金山前地區、躍進東柴山地區、大風山地區是有利氣聚集區。
  15. Based on the research into sedimentary microfacies, source rocks and associations of source rock, reservoir rock and caprock, the paper discusses the formation mechanism of thick oil in detail and summarizes the transportation and accumulation regular of oil - gas in study area

    該文在對沾化凹陷羅家鼻狀構造沙四上段沉積微相、生條件和生蓋組合綜合研究基礎上,詳細論述了稠的形成機制,總結了該區氣運移和富集規律。
  16. Through analyzing rock feature, pore structure feature and physical feature of reservoir, it turns out that the oil and gas potential in most well intervals is bad and only a few well intervals are good

    通過對礦特徵、孔隙結構特徵和物性特徵分析,證明盆地的多數井段集層含、氣性較差,僅少數井段較好。
  17. Logging interpretation of conglomerate reservoir is very difficult in menggulin area with complex rock structure, strong heterogeneity and clear difference between layers

    摘要蒙古林礫石結構復雜,非均質性強,層間差異明顯,測井資料解釋難度較大。
  18. In the southwest and west parts of the nansha waters, the paleogene sediments have suffered from strike - slipping extension and compression, and are comprised of the main oil source rocks in numerous large traps over the area

    南沙西南及西部的下第三系受到走滑、拉張和擠壓的影響,構造復雜,圈閉多,規模大,是主要的生層。
  19. Orthogonal design of mechanical parameters of surrounding rock for underground petroleum storage caverns

    地下儲油巖庫圍力學參數的正交設計
  20. The distribution of the reservoir is controlled by the depositional environment and the faces which are mainly alluvial, delta and river. determined by the diagenesis and the latter reformation, the physical property of the reservoir in general is poor, ranked as class 3 - 4

    層分佈則受沉積環境、沉積相控制,主要有沖積扇、扇三角洲、河道砂等砂體,物性則受成作用及後期改造影響而較差,屬級。
分享友人