老君庙构造带是中国发现最早的老君庙油田所处的构造带，位于酒泉盆地南缘新生代前陆冲断带，叠置于早白垩世断陷盆地的南部隆起和石大凹陷之上。

Laojunmiao structural belt is located in Cenozoic foreland thrust belt of south margin, Jiuquan basin, which is superposed over the south uplift and Shida depression of Early Cretaceous faulted basin.

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老君庙构造带是中国发现最早的老君庙油田所处的构造带，位于酒泉盆地南缘新生代前陆冲断带，叠置于早白垩世断陷盆地的南部隆起和石大凹陷之上。

Laojunmiao structural belt is located in Cenozoic foreland thrust belt of south margin, Jiuquan basin, which is superposed over the south uplift and Shida depression of Early Cretaceous faulted basin.

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