摘要
本文采用开放系统热解实验，对合肥盆地白垩系朱巷组、响导铺组及下第三系定远组的三个生油岩样品分别进行了加热速率为２０℃／ｍｉｎ、３０℃／ｍｉｎ、４０℃／ｍｉｎ和５０℃／ｍｉｎ的热解，测定了各样品的累积生烃率与温度的关系，从而确定出合肥盆地不同时代生油岩的动力学多数。
In this paper,three source rocksamples are sampld from the Cretaceous Zhuxiangand Xiangdaopu Frs.and the Tertiary Dingyuan Fr. of the Hefei basin,and the pyrolyticanalyses have been carried out with the heating rates of 20℃/min,30℃/min,40℃/min,and 50℃/min respectively in an open experimental system. Thi:causes the determinationof the relationship between the generating rates of accumulated hydrocarbons and the tem-peratures of various souece rock samples. Furthermore, it can ascertain the kinetic param-eters of various samples of different geological ages in the Hefei basin.
出处
《石油实验地质》
CAS
CSCD
北大核心
1994年第3期303-307,共5页
Petroleum Geology & Experiment
