“第三系”造句

第三系渐新统临河组 ( E_3l ),始新统乌拉特组 ( E_2wl ).
Paleogene Oligocene Linhe formation ( E _ 3 J ) and Eocene Wulate formation ( E _ 2 wl ).

第三系含水层不能作为供水的主要目的层,但能提供高温热水,可作为供热热源.
But Eogene aquifer cannot be taken as the main objective formation.

黄骅盆地南部前第三系构造层中广泛发育有逆冲构造.
Thrust structure widely developed in pre Tertiary basement in south area of Huanghua basin.

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