Conclusion From Late Permian to Early Jurassic the basin′s subsidence center was situated in Tiaohu Sag, until Middle Jurassic the basin′s subsidence center moved eastwardly to Malang Sag.
结论晚二叠-早侏罗世,盆地的沉降
于条湖凹陷,从侏罗世西山窑期开始盆地的沉降
东迁至马朗凹陷内。
东,从东方东的,从东方的Conclusion From Late Permian to Early Jurassic the basin′s subsidence center was situated in Tiaohu Sag, until Middle Jurassic the basin′s subsidence center moved eastwardly to Malang Sag.
结论晚二叠-早侏罗世,盆地的沉降于条湖凹陷,从侏罗世西山窑期开始盆地的沉降东迁至马朗凹陷内。
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