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石油公司在印度尼西亚的20个陆地盆地钻探的929口井的地热资料,与这个地区的地质和构造有关．可以看出热传导随海侵沉积物和海退沉积物的凝结度以及埋藏深度而增加,但随混合物和不均匀晶粒体积的增大而减少．温度梯度主要是受盆地下部热源深度和温度所控制．在苏门答腊中部、南部、Salawati盆地和Bintuni盆地发现的高热流密度可能是由相对浅的岩浆侵入引起的．
The geothermal data of 929 wells drilled by oil companies in 20 land basins in Indonesia are related to the geology and tectonics of the area. It can be seen that the heat conduction increases with the degree of condensation and the burial depth of the transgressive sediments and the recalcitrant sediments but decreases with the increase of the volume of the mixture and the inhomogeneous grains. The temperature gradient is mainly controlled by the depth and temperature of the heat source in the lower part of the basin. The high heat flux density found in central Sumatra, the southern Salawati and Bintuni basins may be caused by the relatively shallow magma intrusion.