概括
古代的石表明海洋地的沉降始于大约40亿年前. 这一早期的地质过程为地球提供了洞察力
科学领域:
- 地质学
- 地质时间学
- 板块构造
背景情况:
- 石是坚固的矿物质, 保存了早期地球条件的证据.
- 之前的研究主要集中在较晚的潜水启动期.
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