The upper spontaneous potential produced by oil and gas accumulation is of a stable potential field,and its intensity is directly proportional to the content of the source and inversely proportional to the radius apart from the source. Theoretical research and practical results show that anomalies of spontaneous potential can indicate oil-bearing sandstone bodies and locate the areas of oil and gas accumulation. In oil areas which have fewer reservoir beds,the petroleum reservoir thickness can be predicted by determining the linear relationship between potential intensity and apparent equivalent thickness. In the Weixing (卫星) oilfield,which is devoid of sufficient reservoir beds,its apparent equivalent thickness can be predicted by the linear equation h= -0.19x+0.74. On the basis of geological research,we use the spontaneous potential method to predict the equivalent thickness,helping in the selection of the most appropriate drill sites to enhance the probability of successful well boring so as to serve the next round development of the oilfield. The upper spontaneous potential produced by oil and gas accumulation is of a stable potential field, and its intensity is directly proportional to the content of the source and inversely proportional to the radius apart from the source. potential can indicate oil-bearing sandstone bodies and locate the areas of oil and gas accumulation. in the oil area which have less reservoir beds, the petroleum reservoir thickness can be predicted by determining the linear relationship between potential intensity and apparent equivalent thickness. (Satellite) oilfield, which is devoid of sufficient reservoir beds, its apparent equivalent thickness can be predicted by the linear equation h = -0.19x + 0.74. On the basis of geological research, we use the spontaneous potential method to predict the equivalent thickness , helping in the selection of the most appropriate drill sites to enhance the probability of successful well boring so as to serve the next round development of the oilfield.