tertiary hydrocarbon 中文意思是什麼

tertiary hydrocarbon 解釋
叔烴
  • tertiary : adj 1 第三的，第三位的，第三級的。2 【化學】特的，叔的，三代的。3 【醫學】第三期的。4 〈T 〉【地...
  • hydrocarbon : n. 碳氫化合物，烴。
  1. 4. combined with the analysis of the hydrocarbon - generation history, hydrocarbon maturity, fluid inclusions, authigenic illites isotopes chronology and trap forming history, it affirms that jurassic reservoirs formed in three phases : the first in the late jurassic, which was the primary pool - forming phase, the second in the telophase of jurassic to cretaceous, which was the adjusting - destroying phase, the third in tertiary, which was the secondary phase

    4 、採用烴源巖生烴史、油氣成熟度、流體包裹體、儲層自生伊利石同位素年代學和圈閉演化史綜合方法，確認焉耆盆地侏羅系油氣藏具有三期成藏的特點，第一期發生在侏羅紀晚期，是盆地的主要成藏期，第二期為侏羅紀末至白堊紀的油氣藏破壞、調整和再分配期，第三期發生在第三紀，是盆地的次要成藏期。
  2. Through research, the organic matter of source rocks in carboniferous - permian coal measure strata began first hydrocarbon - generating in mesozoic, and the first hydrocarbon - filling took place. but, because of yanshan movement later, the carboniferous - permian strata rose, as a result, the first hydrocarbon - generating and reservoir - forming paused ; in early tertiary period, because carboniferous - permian strata dipping forward east originally turned into dipping forward west, the prototype of faulted block began to form gradually ; by the end of sha - 3 period of early tertiary, the paleogeotherm of carboniferous - permian strata exceed the mesozoic ' s temperature again, and accordingly, abundant hydrocarbon was generated and expulsed secondly. the trap continued to develop ; from the end of late tertiary to quaternary, the second hydrocarbon - generating and expulsing got to its peak, and the second reservoir - forming was over

    研究表明，本區石炭?二疊紀烴源巖在中生代發生一次生烴和排烴，並有油氣充注，后因燕山運動導致地層抬升，一次生烴和成藏過程中止；在早第三紀，原來東傾的地層變為西傾，斷塊圈閉開始具雛形；至早第三紀沙二末期，石炭?二疊系的大部分地層古地溫再次超過中生代一次生烴的溫度，開始二次生烴和排烴，圈閉持續發育；晚第三紀末?第四紀，二次生烴、排烴達到高峰，二次成藏完成。
  3. The paper takes an example of condensed gas feild in qianmiqiao buried - hills. based on the research of formation and development of the buried - hills, three important subjects in the research are discussed with the application of advanced technical and methods ( namely, balanced cross sections, analysis of carbon isotope, mensuration of reservoir fluid inclusion ) : ( 1 ) the development of karstification and characters of reservoir in ordovician ; ( 2 ) lower tertiary ( es3 ) source in the depression nearby ; ( 3 ) the hydrocarbon generation history, migration phase and reservoir formation history

    論文以千米橋潛山凝析氣藏為例，在研究潛山形成演化基礎上，採用先進技術手段（平衡剖面技術、碳同位素分析、儲層流體包裹體測定） ，討論了該潛山油氣藏研究中三個重要問題： （ 1 ）古巖溶發育與奧陶系儲層特徵； （ 2 ）臨近凹陷下第三系油氣源： （ 3 ）油氣生成史與運移期次以及成藏歷史。
  4. And the hydrocarbon - generating is mainly from late cretaceous to tertiary, while traps formed mainly from late cretaceous to tertiary, prior to the hydrocarbon migration or simultaneously, with a fine coordination on the duration

    主要生烴階段發生在晚白堊-第三紀，圈閉的主要形成期在晚白堊紀-第三紀，圈閉形成時間基本早於或同時于油氣運移時間，具有較好的時間配套關系。
  5. In himalaya period, the basin was compressed. as tertiary deposits increased, jurassic source rocks started secondary hydrocarbon generation, thus resulting in the activation and reconstruction of the petroleum system

    燕山運動中晚期，侏羅系大規模沖隆及剝蝕，侏羅系源巖生烴作用終止，含油氣系統被破壞。
  6. The study result show that tarim basin has three major better hydrocarbon source rocks, which are the cambrian - ordovician, carboniferous - lower permian and triassic - tertiary source rocks, and high efficiency gas reservoirs and seal rocks, forming five sets of regional associations of gas reservoir and capping bed

    在盆地內廣泛發育有寒武系奧陶系、石炭系下二疊統和三疊系侏羅系等3套優質烴源巖，以及多套優質儲層和蓋層，形成了5套區域性儲蓋組合。
  7. Investigation into the hydrocarbon generation kinetics of tertiary source rocks from the west of qaidam basin

    柴達木盆地西部第三系烴源巖生烴動力學研究
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