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三江盆地白垩纪—第三纪地层剥蚀厚度恢复研究
Study on the erosion amount of Tertiary-Cretaceous in Sanjiang Basin
【摘要】 本文利用泥岩声波时差法和总声波时差法相结合,辅以镜质体反射率法,恢复了三江盆地白垩系—第三系地层剥蚀厚度。研究表明,三江盆地前进坳陷宝泉岭组剥蚀厚度具有东多西少,北多南少,富锦组剥蚀厚度则具有西多东少,南多北少的特点。滨参1井地区剥蚀作用使生烃处于停滞状态,对油气生成起破坏作用。
【Abstract】 In this paper,we calculate the erosion amount of Tertiary-Cretaceous in Sanjiang Basin by mudstone and total acoustic time difference method and vitrinite reflectance method.The result shows that the three methods fit well.It revealed that: in Sanjiang Basin Baoquanling Formation erosion amount increase from Northeast to Southwest,Fujin Formation erosion amount increase from Southwest to Northeast.In the area of BC1,the erosion played a destroying role in the generation of hydrocarbon.
【关键词】 声波时差;
镜质体反射率;
三江盆地;
剥蚀厚度;
【Key words】 acoustic time difference; vitrinite reflectance; Sanjiang Basin; erosion amount;
【Key words】 acoustic time difference; vitrinite reflectance; Sanjiang Basin; erosion amount;
- 【文献出处】 吉林地质 ,Jilin Geology , 编辑部邮箱 ,2007年01期
- 【分类号】P536
- 【被引频次】2
- 【下载频次】319