起源大陆-地球科学堆栈交换江南电子竞技平台江南体育网页版 最近30从www.hoelymoley.com 2023 - 07 - 10 - t13:15:51z //www.hoelymoley.com/feeds/question/24430 https://creativecommons.org/licenses/by-sa/4.0/rdf //www.hoelymoley.com/q/24430 4 起源大陆 Gillgamesh //www.hoelymoley.com/users/27819 2022 - 10 - 18 - t21:13:48z 2022 - 10 - 19 - t02:15:49z < p >从WorldBuilding SE来访。有人最近问了一个问题,我曾经掸掉旧理论,所以我开始挖掘。可悲的是我能找到更多的话题比我第一次这么想我来这里。< / p > < p >我记得在学校学习板块构造,书籍,电视,杂志文章等。所有提到的< em > < / em >起源大陆被悄然跳过。如果提到它只是指出一个谜。< / p > < p >快进几年和让我了解到另一个的理论,关于月球的形成。我读了< a href = " https://en.wikipedia.org/wiki/Giant-impact_hypothesis " rel = " nofollow noreferrer " >忒伊亚碰撞理论< / >,看到这个动画,另一个(忒伊亚)的行星影响Proto-Earth,形成月球:< / p > < p > < a href = " https://i.stack.imgur.com/LzEJH.gif " rel = " nofollow noreferrer " > < img src = " https://i.stack.imgur.com/LzEJH.gif " alt = "在这里输入图像描述" / > < / > < / p > < p >当我看到它我就知道这是大陆的起源。也许不是地壳板块,但内容,或者说的< a href = " https://en.wikipedia.org/wiki/Craton " rel = " nofollow noreferrer " >克拉通< / >,漂浮在地幔并形成我们所熟悉的大陆。< / p > < p >大家都知道冈瓦纳和泛大陆过去的超级大陆。更很少知道有多达10超级大陆。你和瓦尔巴拉是第一批,数十亿年前泛大陆。

Question: Have there been any publications or studies to prove my novice theory that the moon formation had something to do with the origin of the continents? I was able to find a couple references from Harvard papers, but honestly and obviously it would take a degree to decipher 90 percent of it. In which case I would be answering my own question. Even here the closest answer is that they formed in the early Hadean.

So is this an accepted theory I just haven't ran across, or has it been considered much before?

//www.hoelymoley.com/questions/24430/-/24431 # 24431 7 回答的除砂器的大洲 除砂器 //www.hoelymoley.com/users/27389 2022 - 10 - 18 - t23:43:58z 2022 - 10 - 18 - t23:43:58z < p >创建月球的影响发生早期太阳系的寿命。这种规模的身体都还大多是熔融的影响;据我所知,你的理论不是主流地质思想的一部分,尽管这不能阻止你提出这些想法!< / p > < p >当前被广泛接受的模式是在地质时间和大陆逐渐增加,其中很少是非常小的碎片回收到地幔。还有其他几个,更多的边缘理论支持静态大陆与海洋地壳的比率通过地质时间,为一个更大的部分大陆回收。后者营反对相当大量的放射性年龄证据和年龄之间的相关性和过程持续的构造活动大陆边缘。< / p > < p >要理解为什么大陆了,您需要理解“分化”的过程。在最近的地质环境中(大约3.7年前)后发生的什么事,分化解释了为什么火成岩(熔岩和岩浆)达到他们的各种化学成分:某些元素比其他人更热力学稳定的固相,而另一些人则更喜欢在液体(岩浆)更长时间。这意味着某些元素集中在早期固体(岩石),而其他人更丰富之后形成的岩石。所以那些发生在后者,钠、钾、铝、和(因为它的丰富)硅-往往形成密度更低矿物质,这些矿物质一起为低密度的岩石。< / p > < p >如果你分化的概念应用于跨国境传播岩浆海洋,就像地球上的地狱的——你沉重的元素集中在地球深处,这就是为什么地核和地幔富含元素(如铁、镍和铬等。 Over time, further differentiation operating on a much smaller scale will produce low-density rocks that are too light to be shoved back into the mantle, effectively permanently stranding them near the surface - and thus creating the beginnings of a continent. Repeating this process over billions of years worth of magmatism is what is generally accepted to have led to the gradual (and more or less permanent) growth of the continents.

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