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  • 匿名
关注:1 2013-05-23 12:21

求翻译:在早二叠世鄂尔多斯盆地再度上升,海水基本全部退出盆地,逐渐发展成为内陆拗陷盆地,东西沉积差异也逐渐消失,以河湖相沉积为主。是什么意思?

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在早二叠世鄂尔多斯盆地再度上升,海水基本全部退出盆地,逐渐发展成为内陆拗陷盆地,东西沉积差异也逐渐消失,以河湖相沉积为主。
问题补充:

  • 匿名
2013-05-23 12:21:38
Rise again in the Early Permian Ordos Basin, the sea all the basic out of the basin, and gradually developed into the basin of the inland depression, things deposition differences gradually disappear, mainly lacustrine deposits.
  • 匿名
2013-05-23 12:23:18
As early as 2 stack in the Ordos basin, the sea rose again basic exit all basin, and gradually developed into a land-locked limit sediment trap basin, and what differences are gradually disappearing, rivers and lakes in the sediment.
  • 匿名
2013-05-23 12:24:58
Rises once again in the early permian world Erdos basin, the sea water basic all withdraws from the basin, develops into the interior depression basin gradually, the thing deposition difference also gradually vanishes, by river lacustrine facies deposition primarily.
  • 匿名
2013-05-23 12:26:38
Rising again in the early Permian in Ordos basin, basic all exit basins of water, gradually develop into an inland depression basins, sedimentary difference gradually disappeared, the sediment of rivers and lakes.
  • 匿名
2013-05-23 12:28:18
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