Abstract Three anticline zones developed on the south margine of Junggar Basin. 準噶爾盆地南緣發(fā)育三排背斜帶。
The effect of Yanshan movement and Himalayan orogeny on hydrocarbon migration and accumulation in Junggar basin is analyzed. 分析了燕山運動(dòng)和喜馬拉雅運動(dòng)在準噶爾盆地油氣運移和聚集中的作用。
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