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海底热流研究的首次尝试是 S.E.布拉德(Bullara)于1952年在大西洋进行的。二十多年来,特别是进入七十年代以后,海底热流的研究获得了长足的发展。到1975年为止,世界各国在海洋中总共测量了3718个热流数据,占全球5417个热流数据的三分之二以上。最近几年又有新的增长。众所周知,海底热流的平均值同大陆热流的平均值相等。但是,由于海底面积极其辽阔,地球内部通过海洋散失的热量远远超过从大陆散失的热量。此外,还应看到,由
The first attempt at submarine heat flow research was conducted by S.E. Bullara in the Atlantic in 1952. Over the past two decades, especially after entering the seventies, great progress has been made in the research of seafloor heat flow. By 1975, a total of 3,718 heat flow data were measured in oceans in the world, accounting for more than two thirds of the 5,417 heat flow data worldwide. In recent years there have been new growth. It is well-known that the average value of the seafloor heat flux is equal to the average value of the mainland heat flux. However, due to the vastness of the seafloor, the amount of heat lost through the oceans inside the Earth far exceeds that dissipated from the mainland. In addition, you should also see, from