red graben basin 红色断陷盆地
half-graben basin 箕状断陷盆地
half-graben-basin 箕状断陷盆地
Taiyuan graben basin 太原断陷盆地
unsymmetrical graben basin 不对称地堑盆地
graben-shaped basin 地堑形盆地
graben-fill basin 地堑填充盆地
graben-type basin 地堑型盆地
graben-like basin 似地堑盆地
The Shulan basin is located in the middle sector of Yilan-Yitong rift, and is a semi-graben basin.
舒兰盆地位于依兰—伊通裂谷中段，为半地堑盆地，依兰—伊通裂谷为盆地的边缘断裂，控制了盆内白垩系及新近系含煤地层沉积。
A series of half graben like faulted basins were developed in Jurassic in the northern edge of Qaidam basin, which was mainly controlled by extensional tectonic framework.
柴达木盆地北缘地区在侏罗纪主要受伸展构造体制控制，发育一系列规模较小的箕状断陷盆地。
The Yitong Graben is a Tertiary petroliferous strike-slip fault basin developed on the Hercynian fold basement.
伊通地堑是一个主体在海西期褶皱基底上发育起来的第三纪含油气走滑断陷盆地。
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