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Updated: Apr 5, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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作为富含液体钻石的来源,来自流板的高度盐酸液体

Yaakov Weiss1, John McNeill2, D Graham Pearson3

  • 1Lamont-Doherty Earth Observatory, Columbia University, New York, New York 10964, USA.

Nature
|August 21, 2015
PubMed
概括

钻石揭示了盐水流体, 源于沉积的构造板, 是深层地幔融化的父母. 这些液体驱动了岩层的化学变化, 对于钻石的形成至关重要.

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Deep Sea Microbial Ecology01:18

Deep Sea Microbial Ecology

The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches...
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