Using integrated geophysical data to study basement seperation and geotemperature anomaly field in Zhunger Basin.;

In the geothermal field of xinzheng mining area,there are characteristics of high thermal fluid and high geothermal gradient The geothermal anomaly is result of two actions stack which that locally thermal accumulation caused by special structure and upward flow of high temperature thermal water controlled by hydrogeological conditions,but no relation with deep crustal movemen

The satellite thermal infrared temperature anomaly area always repeats in the same position as the proved oil prospect area in the East China Sea Shelf Basin, and coincides well with both the CH4 content curve at the water-atmosphere interface and the seafloor geochemical anomaly.