一、前言自70年代以来,地球化学勘查测汞方法普遍应用于矿产勘测领域,直到90年代,此方法在断裂构造研究中得以应用并具有显著的效果。随着现代科学技术的发展及对断裂构造研究的深入,人们对地球化学勘查测汞方法的原理、应用等产生了新的认识。实践证明,土壤中的汞气无论来源如何,它都是沿着断裂破碎带这个通道向上移动的。因此,汞气异常能够指示断裂构造的所在位置。本文拟通过土壤吸咐汞的地球化学测量技术来探讨河北 I. Introduction Since the 1970s, geochemical methods for measuring mercury have been widely used in the field of mineral exploration. Until the 1990s, this method was applied in fracture structure research and had significant effects. With the development of modern science and technology and the deepening of research on fault structure, people have come to a new understanding of the principles and applications of mercury detection methods in geochemical exploration. Practice has shown that, regardless of the source of mercury in the soil, it moves up the fault-breaking zone. Therefore, mercury gas anomalies can indicate the location of the fault structure. This paper intends to explore Hebei by geochemical measurement of mercury sorption in soils