浅部地下水主要由现代区内降水补给形成，而深部地下水则可能由地质历史时期降水补给形成。
The shallow groundwater is mainly recharged by modern and local precipitation, and the deep groundwater might be originated from infiltration recharge of ancient precipitation.
浅部地下水主要由现代区内降水补给形成，而深部地下水则可能由地质历史时期降水补给形成。
The shallow groundwater is mainly recharged by modern and local precipitation, and the deep groundwater might be originated from infiltration recharge of ancient precipitation.
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