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探索研究地球固体部分的科学称为地球科学(Geosience),主要包括地质学、地球物理学和地球化学。这门科学虽起步不晚,但却远远不如空间和海洋科学发展迅速,特别是空间科学。笔者认为其主要原因在于人们对地球固体内部的探测缺乏直接有效的方法和取样手段。为此,当代地球科学工作者都在设想和试探如何利用新的探测和采样手段来使地球科学出现新的突破。本文首先回顾探测地下科学技术的历史发展过程,然后就我国制定大陆科学深和超深钻井规划提出建议。
The science that explores the solid part of the Earth is called Geosience, and includes mainly geology, geophysics and geochemistry. Although this science started not too late, it is far behind the rapid development of space and marine science, especially in space science. The author believes that the main reason is that people do not have direct and effective methods and sampling methods for the detection of the earth's interior. For this reason, contemporary earth science workers are envisioning and testing how new detection and sampling methods can be used to make new breakthroughs in earth science. This article first reviews the historical development of underground science and technology and then makes recommendations on the formulation of deep and ultra-deep drilling programs for continental science in China.