江苏地温分布主要受燕山运动以来，特别是挽近地质时期仍然活动的构造体系（主要是新华夏系和华夏式构造）的控制。
The thermal distribution in Jiangsu are controlled largely by tectonic systems since Yanshanian movement , especially Neocathaysian and Cathaysian structural systems .
新华夏式