《地球论》由现代地质学之父詹姆斯·赫顿于1788 年发表。赫顿提出的“均变说”认为，现代地质过程在整个地质时期内以同样方式发生过，并且基本上有相同的强度。根据“均变说&rdquo
- 目录
- 前辅文
- THEORY OF THE EARTH: PLATES
- PART I
- Prospect of the Subject to be treated of
- PART II
- An Investigation of the Natural Operations employed
- in consolidating the Strata of the Globe
- PART III
- Investigation of the Natural Operations employed in
- the Production of Land above the Surface of the Sea
- PART IV
- System of Decay and Renovation observed in the Earth
