In the Perminan,the compression strengthened further and the North Qinling-North Huaiyang structural belt uplifted,making the epeiric sea transit to a marginal lake basin.
二叠纪挤压作用进一步加强，北秦岭—北淮阳构造带全面隆升，致使其北侧由
海演化为缘近海湖泊盆地；
地的In the Perminan,the compression strengthened further and the North Qinling-North Huaiyang structural belt uplifted,making the epeiric sea transit to a marginal lake basin.
二叠纪挤压作用进一步加强，北秦岭—北淮阳构造带全面隆升，致使其北侧由海演化为缘近海湖泊盆地；
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