新生代裂谷盆地主要沿依兰-伊通和敦化-密山断裂呈线状分布。
Cenozoic rift basin is characterized by linear distribution along Yilan-Yitong fault and Dunhua-Mishan fault.
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。
The Yitong Graben is a Tertiary petroliferous strike-slip fault basin developed on the Hercynian fold basement.
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。
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。
The Shulan basin is located in the middle sector of Yilan-Yitong rift, and is a semi-graben basin.
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