沉积中心 depocenter
- 台北凹陷在侏罗纪以后成为吐哈盆地的沉积中心。
Taibei Say was the depositional center of Turpan-Harmi Basin after Jurassic. - 受构造运动的影响,塔里木盆地志留系可容空间发生变化,沉积中心随之迁移,地层厚度发生变化。
Influenced by tectonic movements, the accommodation, the center of sedimentation and the formation thickness changed in the Silurian of Tarim Basin. - 潜江凹陷蚌湖向斜是下第三系潜江组的沉积中心,是江汉盆地油气最富集的生烃中心。
Banghu syncline in the Qianjiang sag is a depocenter of Paleogene Qianjiang Formation, and is the richest hydrocarbon generation center in Jianghan Basin.
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