.png){kind=icon}
.png){kind=icon}
Return
Dissociation of methane and formation of carbon clusters in a reducing pyrolitic magma ocean
.png){kind=icon}
PRE
AI
A
N
R
DOI：10.1016/j.epsl.2026.120222.png)
.png){kind=icon}
Original request for help.png){kind=icon}
Share.png){kind=icon}
Save
Abstract
En 中文
• Methane is not stable in pyrolite melts or in the vapor phase at temperatures greater than 3000 K. • While methane does not appear to dissociate at 2000 K, neither does it readily form. • Methane was likely not a significant component of the early Earth’s magma ocean or early atmosphere.
Journal
IF:
5.1
Papers:
774
Citations:
6.9W
Organization
Cited Papers