1887

Abstract

An entry of magmatic melt to the distinct area of Earth’s crust containing gas deposits can cause significant local warming of it. The temperature increase of a gas deposit located constantly at a determined depth, leads to the increase in pressure due to gas expansion and increasing saturation by water vapors. The degree of pressure increase in the modeled methane gas deposit is appreciated in this work for temperature range from 120 to 360 oC

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.20145516
2010-05-04
2021-01-27
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20145516
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error