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Rapid intrusion of magma into wet rock: groundwater flow due to pore pressure increases.

Journal of Geophysical Research

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Abstract

Analytical and numerical solutions are developed to simulate the pressurization, expansion, and flow of groundwater contained within saturated, intact host rocks subject to sudden heating from the planar surface of an igneous intrusion. For most rocks, water diffuses more rapidly than heat, assuring that groundwater is not heated along a constant-volume pressure path and that thermal expansion and pressurization adjacent to the intrusion drives a flow that extends well beyond the heated region. -from Author

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Rapid intrusion of magma into wet rock: groundwater flow due to pore pressure increases.
Series title:
Journal of Geophysical Research
Volume
87
Issue:
B9
Year Published:
1982
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
First page:
7739
Last page:
7756
Number of Pages:
18