如果人们想要到达地幔,为什么不直接利用火山口呢?-地江南体育网页版球科学堆栈交换江南电子竞技平台 最近30个来自www.hoelymoley.com 2023 - 03 - 25 - t17:33:40z //www.hoelymoley.com/feeds/question/23220 https://creativecommons.org/licenses/by-sa/4.0/rdf //www.hoelymoley.com/q/23220 6 如果人们想要到达地幔,为什么不直接利用火山口呢? 乔凡尼 //www.hoelymoley.com/users/24914 2021 - 11 - 28 - t14:26:52z 2021 - 11 - 28 - t22:58:50z 偶尔有抱负的人想要钻穿地壳到达地幔,但是当地幔实际上在火山口表面或非常接近地表时,他们为什么要这样做呢?科学家们难道不能只利用火山口来研究地幔,而不是在其他地方的地表上钻探数英里吗?< / p > //www.hoelymoley.com/questions/23220/-/23221#23221 1 如果人们的目标是到达地幔,为什么不直接使用火山口呢? hurreechunder //www.hoelymoley.com/users/21109 2021 - 11 - 28 - t19:08:27z 2021 - 11 - 28 - t19:08:27z 我不是地质学家,但我的理解如下:火山可能是长英质或镁铁质的。后者从地幔内部的热点获取“燃料”。这些火山位于地壳较薄的板块边界上。如果问题是“为什么我们不能将探测器发射到这样一个热点火山的地幔中”——我不确定为什么这比直接钻到海洋地壳中更容易,地幔在几公里以下。毕竟,油井钻得比这深得多(尽管它们往往位于大陆架附近,那里有中生代碎屑的增生楔) //www.hoelymoley.com/questions/23220/-/23222#23222 13 如果人们的目标是到达地幔,为什么不直接使用火山口呢? Gimelist //www.hoelymoley.com/users/725 2021 - 11 - 28 - t22:58:50z 2021 - 11 - 28 - t22:58:50z

他们为什么不直接用火山口?< / p >

Because volcano craters don't go to the mantle.

Here's a sketch of how the crust, mantle, and volcanoes look like:

enter image description here

Tan colour is crust, orange is mantle. Your question may come from the misconception that the mantle is molten, but it is actually not. It's solid, except for very localised cases where the mantle is molten (see diagram for examples). This magma then rises through weaknesses or cracks in the solid crust to reach the surface.

Drilling through volcanoes will only give you information on the shallow plumbing of the magmatic system through the crust, and not much on the mantle.

There are places where the mantle is very shallow, for example in oceanic spreading ridges, but those are active magmatic zones and drilling through liquid hot magma is not something that's feasible.

Finally, there are places where mantle rocks have actually been exposed on thee surface, such as ophiolites, but these are probably exposed because the mantle there is slightly unusual. It provides only limited information on the more common and deeply-buried type of mantle that's elsewhere.

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