Investigating the role of dehydration reactions in subduction zone pore pressures using newly-developed permeability-porosity relationships

Author(s): Screaton, E.; Daigle, Hugh; James, S.; Meridth, L.; Jaeger, J. M.; Villaseñor, T. G.
Author Affiliation(s): Primary:
University of Florida, Gainesville, FL, United States
Other:
University of Texas at Gainesville, United States
Volume Title: AGU 2014 fall meeting
Source: American Geophysical Union Fall Meeting, Vol.2014; American Geophysical Union 2014 fall meeting, San Francisco, CA, Dec. 15-19, 2014. Publisher: American Geophysical Union, Washington, DC, United States
Note: In English
Summary: Dehydration reactions are linked to shallow subduction zone deformation through excess pore pressures and their effect on mechanical properties. Two reactions, the transformation of smectite to illite and of opal-A to opal-CT and then to quartz, can occur relatively early in the subduction process and may affect the propagation of the plate boundary fault, the updip limit of velocity-weakening frictional paper, and tsunamigenesis. Due to large variations between subduction zones in heat flow, sedimentation rates, and geometries, dehydration location may peak prior to subduction to as much as 100 km landward of the deformation front. The location of the dehydration reaction peak relative to when compaction occurs, causes significant differences in pore pressure generation. As a result, a key element to modeling excess pore pressures due to dehydration reactions is the assumed relationship between permeability and porosity. Data from Integrated Ocean Drilling Program (IODP) drilling of subduction zone reference sites were combined with previously collected results to develop relationships for porosity-permeability behavior for various sediment types. Comparison with measurements of deeper analog data show that porosity-permeability trends are maintained through burial and diagenesis to porosities <10%, suggesting that behavior observed in shallow samples is informative for predicting behavior at depth following subduction. We integrate these permeability-porosity relationships, compaction behavior, predictions of temperature distribution, kinetic expressions for smectite and opal-A dehydration, into fluid flow models to examine the role of dehydration reactions in pore pressure generation.
Year of Publication: 2014
Research Program: IODP Integrated Ocean Drilling Program
Key Words: 21 Hydrogeology and Hydrology; Dehydration; Integrated Ocean Drilling Program; Marine sediments; Permeability; Porosity; Sediments; Subduction zones
Record ID: 2016006554
Copyright Information: GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data supplied by, and/or abstract, Copyright, American Geophysical Union, Washington, DC, United States
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100 1 |a Screaton, E.  |u University of Florida, Gainesville, FL 
245 1 0 |a Investigating the role of dehydration reactions in subduction zone pore pressures using newly-developed permeability-porosity relationships 
300 |a Abstract H33B-0805 
500 |a In English 
500 |a Research program: IODP Integrated Ocean Drilling Program 
500 |a Affiliation: University of Florida; Gainesville, FL; USA; United States 
500 |a Affiliation: University of Texas at Gainesville; ; USA; United States 
500 |a Source note: American Geophysical Union Fall Meeting, Vol.2014; American Geophysical Union 2014 fall meeting, San Francisco, CA, Dec. 15-19, 2014. Publisher: American Geophysical Union, Washington, DC, United States 
500 |a Publication type: conference paper or compendium article 
510 3 |a GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data supplied by, and/or abstract, Copyright, American Geophysical Union, Washington, DC, United States 
520 |a Dehydration reactions are linked to shallow subduction zone deformation through excess pore pressures and their effect on mechanical properties. Two reactions, the transformation of smectite to illite and of opal-A to opal-CT and then to quartz, can occur relatively early in the subduction process and may affect the propagation of the plate boundary fault, the updip limit of velocity-weakening frictional paper, and tsunamigenesis. Due to large variations between subduction zones in heat flow, sedimentation rates, and geometries, dehydration location may peak prior to subduction to as much as 100 km landward of the deformation front. The location of the dehydration reaction peak relative to when compaction occurs, causes significant differences in pore pressure generation. As a result, a key element to modeling excess pore pressures due to dehydration reactions is the assumed relationship between permeability and porosity. Data from Integrated Ocean Drilling Program (IODP) drilling of subduction zone reference sites were combined with previously collected results to develop relationships for porosity-permeability behavior for various sediment types. Comparison with measurements of deeper analog data show that porosity-permeability trends are maintained through burial and diagenesis to porosities #LT10%, suggesting that behavior observed in shallow samples is informative for predicting behavior at depth following subduction. We integrate these permeability-porosity relationships, compaction behavior, predictions of temperature distribution, kinetic expressions for smectite and opal-A dehydration, into fluid flow models to examine the role of dehydration reactions in pore pressure generation. 
650 7 |a Dehydration  |2 georeft 
650 7 |a Integrated Ocean Drilling Program  |2 georeft 
650 7 |a Marine sediments  |2 georeft 
650 7 |a Permeability  |2 georeft 
650 7 |a Porosity  |2 georeft 
650 7 |a Sediments  |2 georeft 
650 7 |a Subduction zones  |2 georeft 
700 1 |a Daigle, Hugh, 
700 1 |a James, S., 
700 1 |a Meridth, L., 
700 1 |a Jaeger, J. M., 
700 1 |a Villaseñor, T. G., 
711 2 |a American Geophysical Union 2014 fall meeting  |d (2014 :  |c San Francisco, CA, United States)  
773 0 |t AGU 2014 fall meeting  |d Washington, DC : American Geophysical Union, Dec. 2014  |k American Geophysical Union Fall Meeting  |n American Geophysical Union Fall Meeting, Vol.2014; American Geophysical Union 2014 fall meeting, San Francisco, CA, Dec. 15-19, 2014. Publisher: American Geophysical Union, Washington, DC, United States Publication type: conference paper or compendium article  |g Vol. 2014