礦物儲量 的英文怎麼說

中文拼音 [kuàngchǔliáng]
礦物儲量 英文
mineral deposits
  • : 名詞1. (礦床) ore [mineral] deposit 2. (礦石) ore 3. (開采礦物的場所) mine
  • : 名詞1 (東西) thing; matter; object 2 (指自己以外的人或與己相對的環境) other people; the outsi...
  • : 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
  • : 量動1. (度量) measure 2. (估量) estimate; size up
  • 礦物 : mineral
  1. That offer very valuable referential material for future searching mineral. in recent years, many deposits were confronted with reserves crisis in yuebei region. so we studied the typomorphic feature of pyrites, galenite, sphalerite for deposit of yuebei region, and sum up the genesis of deposit and mineral and reseaching typmorphic feature, these have important value to forecast the deepth of deposit and reaserch the outside of deposit

    近幾年,粵北地區的許多床面臨危機,因而對粵北地區床黃鐵、方鉛、閃鋅的標型特徵進行研究,總結出凡口、紅巖、大寶山等的成因和找標型特徵,對于進行床的深部預測和外圍找工作具有十分重要的意義。
  2. Select a vital nonrenewable or exhaustible resource ( water, mineral, energy, food, etc. ) for which your team can find appropriate world - wide historic data on its endowment, discovery, annual consumption, and price

    選擇一個至關重要的,但不能再生或者用得盡的資源(水,質,能源,食品,等等) ,你的隊需要找到一些關於它的蘊藏,已發現,每年消費額和價格的數據,這些數據應該是適合世界范圍的、有歷史意義的。
  3. 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油田,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油氣聚集帶的關鍵.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巖過程中粘土脫水作用.粘土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油巖中的大有機酸及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的次生孔隙,為後期油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
  4. 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油田,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油氣聚集帶的關鍵.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巖過程中粘土脫水作用.粘土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油巖中的大有機酸及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的次生孔隙,為後期油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
  5. This paper has described the principle of the contact polarization curve method and the technique for measuring basic parameters, analyzed the influence of such factors as oxidation conditions of the ore deposits, arrangement of electrodes and structures of orebodies on the basis of studying some typical polarization curves, inferred several parameters such as independency of orebodies, reacted minerals, effective areas of reacted minerals, reserves of elements and grades of elements for some measured typical curves, and compared the inferences with the exploration results

    摘要介紹了接觸極化曲線法的原理及基本參數的測取方法;通過一些典型極化曲線,對床氧化狀態、電極排布、體結構等因素的影響作了分析;對所測得的部分典型曲線進行了體獨立性、反應、反應有效面積、元素、元素品位等參數的推斷,並將推斷與勘探結果進行了對比分析。
  6. 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衍射全巖分析方法、粘土分析方法和薄片鑒定等方法研究了城華地區延8 -延10層巖石學特徵和孔隙成因類型.綜合論述了城華地區延8延10油組不同巖相層砂巖的基本特徵,糾正了砂巖定名的錯誤和主要填隙成份的錯誤,同時還論述了層砂巖的孔隙特徵和控制孔隙發育的主要因素
  7. 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衍射全巖分析方法、粘土分析方法和薄片鑒定等方法研究了城華地區延8 -延10層巖石學特徵和孔隙成因類型.綜合論述了城華地區延8延10油組不同巖相層砂巖的基本特徵,糾正了砂巖定名的錯誤和主要填隙成份的錯誤,同時還論述了層砂巖的孔隙特徵和控制孔隙發育的主要因素
  8. It has been the research interest of many scientists to burn fuel clearly and have high efficiency at the same time

    地球上的燃料是一次性能源,它的有限,因此,如何高效清潔地燃燒各種燃料是許多科技工作者的目標。
  9. The store of weatherable minerals will control the limits of the effects of these changes.

    易風化將控制著這些變化所造成的影響的限度。
  10. There are various reservoir structure types of the insert salt layers non - sandstone reservoirs in jiangban oil region, mainly including porous type, porous - fracture type and fracture type, and high mineral contents of clay

    摘要江漢油區鹽間非砂巖層結構類型多,主要有孔隙型、孔隙裂縫型和裂縫型;粘土較高;這種層主要是泥巖,含盆和白雲石,裂縫發育,並且巖性變化大。
  11. For nutritional substance exists in organic state with weak process of mineralization, the available elements are low, especially a lack of available nitrogen and phosphorus, the soil condition can not meet the needs of plant growing

    。有機質含高,其總氮總磷和鉀的較豐富。由於化作用弱,營養質缺乏,特別是有效氮和有效磷的缺乏難以滿足植的生長。
  12. Multi - hierarchical, multimeans, comprehensive and deepened research on the macrofractures, microfractures system and pores system features, capacity of cbm storage and osmosis, adsorption characteristic, as well as physical properties of surrounding rocks of coal reservoirs have been made. furthermore, classifying standard and identifying characteristics for fractures - pores system of low coal rank coal reservoirs in zhungaer basin has been put forward as well. in this process, some routine instrument are used, such as viewing coal mine scene and hand specimen, observing polished section and surface which are made from lump coal and powder coal samples, observing and image analyses under the common microscope ' s transmitted light, reflection light and fluorescence

    通過井現場、鏡下觀察統計等常規手段,採用多種先進儀器和測試技術展開對煤層的裂隙系統與孔隙系統發育特徵、滲性能、吸附特性及煤層圍巖性特徵的多層次、多手段分析,並綜合室內外觀測及前人成果,提出了煤層裂隙與孔隙系統的劃分標準與識別特徵,分別從宏微觀尺度、定性與定層次對裂隙與孔隙系統特徵及其與煤滲性能關系的研究。
  13. Organic vegetables are rich in vitamins, minerals and cellulose with comparatively less moisture ; while freshwater fish are reared with healthy feed, therefore they are nutritious, tasty and durable

    有機蔬菜含豐富維生素質及纖維素,水份含較少而淡水魚是用健康飼料喂養因此營養高風味佳耐存。
  14. In china, it is more prominent, about 86 % amount of nickel, 90 % amount of platinum metals, 7. 3 % copper comes from nickel - copper sulfide magmatic deposits

    我國的情況更為突出,鎳金屬近86 、鉑90以上、銅約7 . 3均來源於銅鎳硫化巖漿床。
  15. Mining industry authority evaluates an object to include prospect authority and mining right, but no matter be, mining counterpoises, the corporeal carrier of the core that its evaluate is valuable ore body ( geological body ) the reserves of the different level of place correspondence

    業權評估對象包括探權和采權,但無論是探權還是采權,其評估的核心的質載體是有價值的體(地質體)所對應的不同級別的
  16. Soil quality - sampling and storage of soil samples in view of determination of mineral nitrogen on fresh soil

    土壤質.為測定新鮮土壤中氮含對土壤進行的取樣和樣品的
  17. But now it is realized that supplies of some of them are limited, and it is even possible to give a reasonable estimate of their “ expectation of life ”, the time it will take to exhaust all known sources and reserves of these materials

    可是現在人們意識到,其中有些質的藏是有限的,人們甚至還可以比較合理的估計出這些質「存在年數」 ,也就是說,經過若干年後,這些的全部已知源和將消耗殆盡。
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