凝析油 meaning in Chinese
condensate oil; condensate
Examples
- Research of condensate accumulation based on phase change of gas condensate
基于凝析气相变的凝析油聚集规律研究 - The geochemical characteristics and origin of gas and condensate oil in kokyar gas field , tarim basin
塔里木盆地柯克亚地区天然气和凝析油的地球化学特征与成因 - The estimation results show that the wax precipitation amount and related temperature given by the model are in good agreement with the experimental data for the condensate hydrocarbon mixtures
通过对凝析油蜡沉积的计算表明，用该模型计算蜡的沉积量和析蜡温度与实验结果非常吻合。 - Firstly , based on the basin prototype , the triassic and jurassic mudstone and coal , the main source rocks of the basin , did not develop better in baicheng sag than in the northern thrust belt including keyi structural belt ; secondly , because of the thrusting happened in late cenozoic , the triassic and jurassic source rocks reach to a high to over high maturity and thus generate gas or condensate oil mainly . thirdly , the thrust faults compelled the natural gas to migrate from the north to the south or from the deep to the shallow . as a result , the keyi structural belt and the eastern qiulitage structural belt enriched in natural gas because they were not only located on the migration routines of the natural gas , but also developed simultaneously when the gas migration happened
从盆地构造史研究的角度认为库车盆地的天然气主要来源于北部山前冲断带： 1受原型盆地构造格局的制约，三叠系侏罗系烃源岩发育的最有利位置不是在拜城凹陷，而是在克依构造带及其以北的北部山前冲断带2晚第三纪以来的逆冲推覆作用使得烃源岩提早进入高过成熟阶段，并以产气和凝析油为主3逆冲推覆作用所产生的北倾逆断层控制天然气自下而上自北而南运移，位于运移路线上的克依构造带和秋里塔格构造带的东段与烃源岩的排气期匹配较好，从而使这些地区最富集天然气。 - 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。