都日木断陷为二连盆地的中新生代单断型凹陷，其地表为腾格尔沙漠的一部分。
Durimu faulted depression is a Cenozoic simple fault type depression in Erlian basin. Its surface is a part of Tengger Desert.
喀什凹陷北部地表构造出露有多处油砂，分布层位主要是中新统安居安组和帕卡布拉克组，次为下白垩统克孜勒苏群。
Oilsand has been found in many ground structures in northern Kashi sag, which distributed mainly in Miocene Anjuan andPakabulake Formation, secondly in Lower Cretaceous Kzlesu Formation.
都日木断陷是二连盆地中一个中新生代单断型凹陷，其地表景观为腾格尔沙漠的一部分。
Durimu sag is a Mesozoic Cenozoic sag of Erlian Basin and its landscape is a part of Tengger Desert.
都日木断陷是二连盆地中一个中新生代单断型凹陷，其地表景观为腾格尔沙漠的一部分。
Durimu sag is a Mesozoic Cenozoic sag of Erlian Basin and its landscape is a part of Tengger Desert.
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