Wegener's book on continental drift was published in 1915.

Wegener关于陆漂移的著作出版于1915年。

There's some kind of continental drift going on.

现在感觉我们之间产生巨分歧。

People didn't understand continental drift because they didn't understand seafloor spreading.

人们不相信陆漂移是因为他们不了解海底扩。

In 1912 meteorologist Alfred Wegener came forward with the first truly detailed explanation of continental drift.

1912 年，气象家阿尔弗雷德·魏格纳提出了第个真正详细的陆漂移解释理论。

This was the mechanism that could drive continental drift, now understood as plate tectonics.

这是驱动陆漂移的机制，现在被称为板块构造。

Just like any detective story, the case of continental drift required keen observation, relentless questioning, and a little bit of serendipity.

就像任何侦探故事样，陆漂移案件需要敏锐的观察、不懈的质点点偶然性。

So why did it take people so long to believe in continental drift, when it's obvious that Africa and South America fit together like a puzzle?

为什么陆漂移经过那么长时间才被普遍认可，这不目了然吗，非洲南美洲可以像拼图样拼在起？

This is a 'continental drift book' only to the extent that Wegener was interested in that topic and later became famous for it.

这是本“陆漂移书”，只是韦格纳对该主题感兴趣并后来因此而闻名。

Over the next decades, other scientists brought forth more evidence for the theory of continental drift, such as the presence of identical plant fossils in North American and European coal deposits.

在接下来的几十年里，其他科家为陆漂移理论提出了更多的证据，比如在北美欧洲的煤矿中发现了相同的植物化石。

In 1953 he confessed: I have never succeeded in freeing myself from a nagging prejudice against continental drift; in my geological bones, so to speak, I feel the hypothesis is a fantastic one.

1953年，他承认：“对于陆漂移，我从来没有摆脱过种令人不安的反感；在作为地质家的骨子里，恕我直言，我觉得这个假设是个荒唐的假设。”

Yet plate tectonics is a descendant of Alfred Wegener's theory of continental drift, in quite the same way that modern evolutionary theory is a descendant of Darwin's theory of natural selection.

然而板块构造是阿尔弗雷德·韦格纳陆漂移理论的后裔，就像现代进化论是达尔文自然选择理论的后裔样。

The theory of continental drift was also instrumental in developing another theory — that of plate tectonics, which explains that the movement of large sections of Earth's crust, called tectonic plates, causes changes in Earth's surface.

陆漂移理论也有助于发展另种理论——板块构造理论，该理论解释了地壳块区域（即构造板块）的运动导致了地球表面的变化。

When I started writing about Wegener's life and work, one of the most intriguing things about him for me was that, although he came up with a theory on continental drift, he was not a geologist.

当我开始写韦格纳的生活工作时，对我来，关于他最有趣的事情之是，尽管他提出了陆漂移理论，但他并不是位地质家。