嘉陵江組 的英文怎麼說

中文拼音 [jiālíngjiāngzǔ]
嘉陵江組 英文
t1j
  • 嘉 : Ⅰ形容詞1 （美好） good; fine 2 （吉慶; 歡樂） blessed; auspicious Ⅱ動詞（誇獎; 贊許） praise; com...
  • 陵 : 名1. （丘陵） hill; mound 2. （陵墓） mausoleum; imperial tomb 3. （姓氏） a surname
  • 江 : 名詞1. （大河） （large） river 2. （指長江） the changjiang [yangtze] river 3. （姓氏） a surname
  • 組 : Ⅰ名詞1 （由不多的人員組成的單位） group 2 （姓氏） a surname Ⅱ動詞（組織） organize; form Ⅲ量詞（...
  1. The paper adopts some methods such as gas composition, carbon isotope, systematical analyzing and testing of reservoir bitumen biomarker from high evolutional natural gas and quantitative calculation of mixed gas, illustrates that natural gas from the section of jialingjiang formation is mainly attributed to sapropel type organic matter gas of permian, comes from carbonatite hydrocarbon rocks permian which most of them are overmature, its main gas source has nothing to do with carbonatite hydrocarbon rocks of jialingjiang formation themselves, presents in geochemistry characteristics of oil type cracked gas

    摘要通過對川中川南過渡帶西部的磨溪潼南地區嘉二段天然氣組成、碳同位素組成、高演化天然氣儲層瀝青生物標志化合物的系統分析測試和混合成因氣的定量估算，闡明了該區嘉二段天然氣主要屬於二疊系腐泥型有機質成因氣，來源於二疊系過成熟為主的碳酸鹽巖烴源，主力氣源與嘉陵江組自身的碳酸鹽巖烴源無關，並具有油型裂解氣的地球化學特徵。
  2. Study on hydrocarbon sources of lower triassic jialingjiang formation in south of sichuan basin, china

    四川盆地南部嘉陵江組烴源研究
  3. Based on the analysis of sedimentary facies in individual wells and the correlation of three cross sections of sedimentary facies, it is elaborated that sedimentary facies of jianglingjiang formation are vertically and laterally developed within qianwei area. by the method of single - factor analysis, it is pointed out facies distribution of four key formations after thorough study of four geologic factors that could embody sedimentary environment and facies, that is the thickness of formation, grainstone and dolostone, and lithofacies. with the above results, combining with reservoir and structural features, of which the emphasis is the reservoir characteristics of different rock and microfacies types, it is pointed out favorable reservoir zones, by the method of multi - factors superposition

    採用單因素分析法，選取並研究地層厚度、顆粒巖厚度、白雲巖厚度和區域巖相等四種能反映沉積環境和沉積相的地質因素，指出了四個重點層段的沉積相平面分佈特徵；根據沉積相的研究成果，結合儲層特徵和構造發育特徵，著重討論了不同巖石類型和微相類型的儲集特徵，採用多因素疊合法對犍為地區嘉陵江組有利儲集相帶進行了預測，指出了有利儲集相帶的分佈。
  4. Qianwei area is located in the southwest of sichuan basin, with the controlled area of more than 5000 square kilometers. the earlier exploration results in the study area and concerned information in the neighboring area show that it has rich hydrocarbon source

    犍為地區位於四川盆地西南部，工區控制面積5000餘平方公里，前期勘探成果和鄰區勘探資料已顯示該區有豐富油氣資源，區內下三疊統嘉陵江組為重點目的層。
  5. Under the guidance of new principles and methods of sedimentology and reservoir sedimentology, this thesis takes jialingjiang formation in qianwei area as the main object of study. the petrology characteristics and sedimentary facies of nine basic wells have been studied exhaustively, from which it is deducted the depositional framework, and main types and characteristics of sedimentary facies in jialingjiang formation. then four types of sedimentary facies are recognized and their facies models are established

    本論文以現代沉積學與儲層沉積學的新理論、新觀點、新方法為指導，以犍為地區嘉陵江組為重點研究對象，通過9口基幹井的單井巖石學特徵、沉積相的分析，闡述了犍為地區嘉陵江組的沉積格局以及主要的沉積相類型與特徵，識別出了四種不同類型的亞相，並分別建立了沉積相模式；在單井沉積相分析的基礎上，通過三條連井剖面沉積相的對比研究，闡明了犍為地區嘉陵江組沉積相的縱向與橫向發育規律。
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