石油巖資源 的英文怎麼說
中文拼音 [dànyóuyánzīyuán]
石油巖資源
英文
oil shale resources- 石 : 石量詞(容量單位, 十斗為一石) dan, a unit of dry measure for grain (= l00 sheng)
- 油 : 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...
- 巖 : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
- 資 : Ⅰ名詞1 (錢財; 費用) money; wealth; expenses 2 (資質) intelligence; endowment 3 (資格) quali...
- 源 : 名詞1. (水流起頭的地方) source (of a river); fountainhead 2. (來源) source; cause 3. (姓氏) a surname
- 石油 : [地質學] petroleum; fossil oil; oil; 瀝青基石油 asphalt-base petroleum
- 資源 : natural resources; resource
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Based on available data, the study on regional structure, sedimentary reservoir and source rock characteristics shows that the basins in south china sea had experienced sedimentary evolution in faulting period and depression period, deposited thick cenozoic formation, upwardly developed alluvial fan facies, river - lake facies coastal swamp facies coastal facies, neritic facies and bathyal deposit system, regionally had 3 source rocks of eocene, oligocene and miocene, 3 reservoirs of pre - cenozoic basement buried bill, oligocene sandstone and miocene reef, with pliocene and pleistocene neritic facies and bathyal shale as regional caprock
摘要以現有資料為基礎,通過對區域構造、沉積儲層、烴源巖特徵等基礎石油地質條件研究,認為南海海域各盆地經歷了斷陷期和坳陷期沉積演化,沉積了巨厚的新生代地層,自下而上發育了沖積扇相、河湖相、濱岸沼澤相、濱海相、淺海相、半深海相沉積體系,區域上存在始新統、漸新統和中新統3套烴源巖,前新生代基巖潛山、漸新統砂巖、中新統生物礁3套儲層,區域蓋層為上新統和更新統淺海半深海相泥巖。Based on the results of the third hydrocarbon resources evaluation in junggar basin, the amount of the hydrocarbon resources in carboniferous and permian are 1. 35 billion equivalent and 2. 56 billion equivalent respectively, among which the hydrocarbon resources in carboniferous occurs in volcanic rock, while the hydrocarbon resources in permian with one fourth distributed in the volcanic rock of jiamuhe formation
根據準噶爾盆地第三次油氣資源評價結果,蘊藏在石炭系和二疊系中的油氣資源量約分別為13 . 5億噸(當量)和25 . 6億噸(當量) ,其中石炭系的油氣資源量主要分佈在火山巖中,而二疊系的資源量約有1 / 4分佈在佳木河組的火山巖中。Associated with the study of lighter hydrocarbon constituent, carbon isotope, biomarker and inclusions, adopted the technique of oil source correlation on whole oil samples, it can be confirmed that the hydrocarbon source of viscous crude in permian, in the east slope of jimusaer depression, is pingdiquan formation mudstone ; carboniferous oil comes from carboniferous source rock. meanwhile, the causes of oil formation are investigated based on datum of reservior geochemistry : viscous crude of permian is the result of biodegradation and low maturity working together, and that lighter hydrocarbon constituent of carboniferous oil is missing. at last, the mode and mechanism of the oil pool formation are analysed in the study area according to the structure phylogeny, sedimentary history, and data of reservior geochemistry
本論文根據輕烴、碳同位素、生物標志化合物等資料,運用全烴地球化學油源對比方法進行油源對比,得出吉木薩爾凹陷東斜坡區二疊系的稠油來自平地泉組泥巖,石炭系的稀油來自石炭系本身源巖;同時,根據地化資料研究了原油的成因,認為二疊系稠油是生物降解和成熟度較低共同作用的結果,石炭系的稀油存在輕組分散失現象;最後,綜合構造、沉積、烴源巖和油藏地球化學資料,分析了吉木薩爾凹陷原油的成藏機制和模式。Located in the fixed place of shandong and henan, shenxian guyun economic development zone occupies 60 square kilometers and rich in petroleum, natural gas and rock salt
山東莘縣古雲經濟技術開發區位於魯豫兩省的交界處,規劃面積60平方公里,石油、天然氣、巖鹽等資源豐富。Based on the study of organic geochemistry and organic lithology, this paper mainly discussed the question of the hydrocarbon generating potential and contribution of hydrogen - rich maceral in liupanshui area, guizhou province
從有機巖石學與有機地球化學角度研究烴源巖有機質成烴演化和生烴作用是油氣資源評價的一個重要方面。Abstract : based on the study of organic geochemistry and organic lithology, this paper mainly discussed the question of the hydrocarbon generating potential and contribution of hydrogen - rich maceral in liupanshui area, guizhou province
文摘:從有機巖石學與有機地球化學角度研究烴源巖有機質成烴演化和生烴作用是油氣資源評價的一個重要方面。Under the guide of dynamic system for pool - forming and petroleum system, this research has fully taken advantage of every kinds of data from the area, applied the new idea, new technology, new methods to study tectonic, sedimentary and resource rock. the results suggest that the source rock of permo - carboniferous has undergone three evolution periods. the first gas generation occurs at the end of triassic and the generation stopped during jurassic - cretaceous
該文以成藏動力學系統和含油氣系統理論為指導,充分利用工區以及鄰區的各種資料,運用新思路、新技術、新方法,在構造、沉積、烴源巖評價等基礎地質研究的基礎上,認為石炭?二疊系烴源巖經歷了三疊紀末期以前的一次生氣階段、侏羅紀?白堊紀時期的演化停止階段和早第三紀至今的二次生氣階段等三個階段。In china, sediment trap of carbonate rocks is large, oil generation from carbonate rocks has been the focus which geologists and geochemists are - concerned about
我國碳酸鹽巖沉積區分佈面積廣闊,碳酸鹽巖烴源巖評價標準問題,事關油氣勘探方向和投資力度,一直是石油地質、地球化學家所關心的焦點問題之一。分享友人