Pressure core characterization tools for hydrate-bearing sediments

Natural gas hydrates form under high fluid pressure and low temperature, where biogenic or thermogenic gases are available. These requirements delimit the distribution of hydrate-bearing sediments to sub-permafrost, deep lakes

Bibliographic Details
Main Authors: J. Carlos Santamarina, Sheng Dai, Junbong Jang, Marco Terzariol
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2012
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.652.8694
http://pmrl.ce.gatech.edu/papers/Santamarina_2012a.pdf
Description
Summary:Natural gas hydrates form under high fluid pressure and low temperature, where biogenic or thermogenic gases are available. These requirements delimit the distribution of hydrate-bearing sediments to sub-permafrost, deep lakes