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当挠褶型或单斜型自流含水层的一边发生尖灭或者为正断层所限制时,就形成了自流水盆地。假定盆地的边缘是由直线形补给边线和半圆形不渗透边线所组成,如图1所示,这是近似的表示了实际情况。
Self-flowing basins are formed when one side of a flexure-type or monocline-type artesian aquifer is pinned out or restricted by normal faults. Assuming that the basin’s edge is composed of a straight supply edge and a semi-circular impermeable edge, as shown in FIG. 1, this is approximate to represent the actual situation.