一、地球内部热量地球内部包含有巨大的热量,这些热量简称地球内热,它是驱动板块构造、地幔对流和地球自激发电机的动力,是推动整个地球发生发展和演化的原动力。在45亿~47亿年前的地球形成早期,地热促成了核、幔、壳的分异,使地球从一个太空中未曾分异的“混沌体”演变成现今所看到的多圈层的地球;在现今,地热驱动着诸如构造运动、岩浆活动、火山作用等一 First, the Earth’s internal heat The Earth’s interior contains huge amounts of heat, these heat referred to as the Earth’s heat, which is driven plate tectonics, mantle convection and the Earth’s self-excited power generator is to promote the development and evolution of the entire planet the driving force behind. From 4.5 billion to 4.7 billion years ago, the Earth formed early, geothermal contributed to the nuclear, mantle, shell differentiation, the Earth from a space undivided “chaos body ” evolved into today’s multi-turn Layer of earth; in today, geothermal drives such as tectonic movement, magmatic activity, volcanism, etc.