condensed oils造句

• 4 . based on the research of geochemical characters of hydrocarbon source rock and comparison of oil and gas sources , it is indicated that the condensed oil and gas in buried hills mainly came from es3 effective hydrocarbon source rock of type iii kerogen - type ii2 kerogen in banqiao deprssion and qikou depression beside both sides of the tilting horst , and which is the main source of buried hill with early reservoir and late oil and gas source
  4根据烃源岩地球化学特征和油气源对比，指出潜山凝析油气主要来自翘倾地垒块两侧板桥和歧口凹陷的沙三段腐植-偏腐植型有效烃源岩，该凝析油气是“新生古储”型潜山的主要油气源。
• Futhermore , the formation of reservoir experienced four periods : the first , from esi to ed ; the second , from late ng to early nm ; the third , nm ; the fourth , from late nm to now . so we predict that exploration in qianmiqiao should be mainly directed to condensed oil and gas reservoir nearby banqiao depression and gas reservoir is more probably found near qikou depression . 8 . analogue of the conditions required for reservoir formation in huanghua buried hills shows that , high quality and thick es3 hydrocarbon source rock distributed richly in the middle area depression , and moderate quality sandstone distributed in south area , but the match bet
  8对黄骅坳陷区“新生古储”型潜山成藏条件的类比分析表明，中区凹陷中分布有厚度较大的优质沙三段烃源岩，南区分布有较好的孔二段烃源岩，但中区千米桥地区生储配置比南区好，因此，整体上中区千米桥潜山一带油气藏的勘探前景优于南区。
• The formation of oil and gas experienced three periods with different temperature peak zone : first , 120 - 125 , oil generation period ; second , 140 ~ 150 , condensed oil generation period ; third , 160 - 190 , condensed oil and dry gas generation period . likewise , the migration of oil and gas are divided into three stages : from early esi to late ng , then from early nm to mid nm , and last from late nm to now . we can see clearly that oil and gas began to migrate with large scale after nm
  其中，油气形成有三个时期，其温度主值区间为：第一期， 120 125 ，为生油时期，第二期， 140 150 ，为凝析油生成时期，第三期， 160 190 ，为凝析油和干气生成时期；油气运移期次为三期：即沙一早期?馆陶末期，明化镇早期?明化镇中期和明化镇晚期?现在，而且明化镇晚期以后油气才发生大规模运移。