The data of chemical composition of sediments indicate that the tectonic background of the turbidites is passive continental margin environment.
碎屑物常量化学成分投点表明,其形成时构造背景属被动大陆边缘。
There is a barrier between reservoir and atmospheric water of basin margin forming reducing environment with low sulphate which is favorable to methane bacteria activity.
储层与盆地边缘大气水渗滤带隔绝,形成了低硫酸盐的还原环境,有利于甲烷菌活动。
The sediment environment was in the passive continental margin.
沉积环境为被动大陆边缘。
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