The role of fault-zone architectural elements and basal altered zones on pore pressure propagation and induced seismicity
Abstract
Here, we used hydrogeologic models to assess how fault-zone properties promote or inhibit the downward propagation of fluid overpressures from a basal reservoir injection well (150 m from fault zone, Q = 5000 m3/day) into the underlying crystalline basement rocks. We varied the permeability of the fault-zone architectural components and a crystalline basement weathered layer as part of a numerical sensitivity study. Realistic conduit-barrier style fault zones effectively transmit elevated pore pressures associated with four years of continuous injection to depths of ~2.5 km within the crystalline basement while compartmentalizing fluid flow within the injection reservoir. The presence of a laterally continuous, relatively low-permeability altered/weathered basement horizon (kaltered layer = 0.1 × kbasement) can limit the penetration depth of the pressure front to ~500 m. On the other hand, the presence of a discontinuous altered/weathered horizon that partially confines the injection reservoir without blocking the fault fluid conduit promotes downward propagation of pressures. Permeability enhancement via hydromechanical failure was found to increase the depth of early-time pressure front migration by a factor of 1.3 to 1.85. Dynamic permeability models may help explain seismicity at depths of >10 km such as is observed within the Permian Basin, NM.
- Authors:
-
- Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
- New Mexico Inst. of Mining and Technology, Socorro, NM (United States). Dept. of Earth and Environmental Science
- Utah State Univ., Logan, UT (United States). Dept. of Geology
- Publication Date:
- Research Org.:
- Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
- Sponsoring Org.:
- USDOE; USGS National Earthquake Hazards Reduction Program (NEHRP); W.M. Keck Foundation
- OSTI Identifier:
- 1467281
- Report Number(s):
- LA-UR-18-22111
Journal ID: ISSN 0017-467X
- Grant/Contract Number:
- AC52-06NA25396; 2015-0068; 989941
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Ground Water
- Additional Journal Information:
- Journal Volume: 57; Journal ID: ISSN 0017-467X
- Publisher:
- Wiley - NGWA
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; Induced seismicity; hydrologic modeling; fault-zone architecture; crystalline basement faults; basal reservoirs; triggered seismicity; damage zone
Citation Formats
Ortiz, John Philip, Person, Mark A, Mozley, Peter S, Evans, James P, and Bilek, Susan L. The role of fault-zone architectural elements and basal altered zones on pore pressure propagation and induced seismicity. United States: N. p., 2018.
Web. doi:10.1111/gwat.12818.
Ortiz, John Philip, Person, Mark A, Mozley, Peter S, Evans, James P, & Bilek, Susan L. The role of fault-zone architectural elements and basal altered zones on pore pressure propagation and induced seismicity. United States. https://doi.org/10.1111/gwat.12818
Ortiz, John Philip, Person, Mark A, Mozley, Peter S, Evans, James P, and Bilek, Susan L. Thu .
"The role of fault-zone architectural elements and basal altered zones on pore pressure propagation and induced seismicity". United States. https://doi.org/10.1111/gwat.12818. https://www.osti.gov/servlets/purl/1467281.
@article{osti_1467281,
title = {The role of fault-zone architectural elements and basal altered zones on pore pressure propagation and induced seismicity},
author = {Ortiz, John Philip and Person, Mark A and Mozley, Peter S and Evans, James P and Bilek, Susan L},
abstractNote = {Here, we used hydrogeologic models to assess how fault-zone properties promote or inhibit the downward propagation of fluid overpressures from a basal reservoir injection well (150 m from fault zone, Q = 5000 m3/day) into the underlying crystalline basement rocks. We varied the permeability of the fault-zone architectural components and a crystalline basement weathered layer as part of a numerical sensitivity study. Realistic conduit-barrier style fault zones effectively transmit elevated pore pressures associated with four years of continuous injection to depths of ~2.5 km within the crystalline basement while compartmentalizing fluid flow within the injection reservoir. The presence of a laterally continuous, relatively low-permeability altered/weathered basement horizon (kaltered layer = 0.1 × kbasement) can limit the penetration depth of the pressure front to ~500 m. On the other hand, the presence of a discontinuous altered/weathered horizon that partially confines the injection reservoir without blocking the fault fluid conduit promotes downward propagation of pressures. Permeability enhancement via hydromechanical failure was found to increase the depth of early-time pressure front migration by a factor of 1.3 to 1.85. Dynamic permeability models may help explain seismicity at depths of >10 km such as is observed within the Permian Basin, NM.},
doi = {10.1111/gwat.12818},
journal = {Ground Water},
number = ,
volume = 57,
place = {United States},
year = {Thu Aug 09 00:00:00 EDT 2018},
month = {Thu Aug 09 00:00:00 EDT 2018}
}
Web of Science
Works referenced in this record:
The relation between the lowering of the Piezometric surface and the rate and duration of discharge of a well using ground-water storage
journal, January 1935
- Theis, Charles V.
- Transactions, American Geophysical Union, Vol. 16, Issue 2
Probabilistic assessment of potential fault slip related to injection-induced earthquakes: Application to north-central Oklahoma, USA
journal, October 2016
- Walsh, F. Rall; Zoback, Mark D.
- Geology, Vol. 44, Issue 12
Permeability of the continental crust: Implications of geothermal data and metamorphic systems
journal, February 1999
- Manning, C. E.; Ingebritsen, S. E.
- Reviews of Geophysics, Vol. 37, Issue 1
Hydraulic properties of the crystalline basement
journal, November 2006
- Stober, Ingrid; Bucher, Kurt
- Hydrogeology Journal, Vol. 15, Issue 2
Permeability of continental crust influenced by internal and external forcing
journal, May 2008
- Rojstaczer, S. A.; Ingebritsen, S. E.; Hayba, D. O.
- Geofluids, Vol. 8, Issue 2
A review of recent developments concerning the structure, mechanics and fluid flow properties of fault zones
journal, November 2010
- Faulkner, D. R.; Jackson, C. A. L.; Lunn, R. J.
- Journal of Structural Geology, Vol. 32, Issue 11
Disposal of Hydrofracking Waste Fluid by Injection into Subsurface Aquifers Triggers Earthquake Swarm in Central Arkansas with Potential for Damaging Earthquake
journal, March 2012
- Horton, S.
- Seismological Research Letters, Vol. 83, Issue 2
Estimating the crust permeability from fluid-injection-induced seismic emission at the KTB site
journal, November 1997
- Shapiro, Sergei A.; Huenges, Ernst; Borm, Günter
- Geophysical Journal International, Vol. 131, Issue 2
Fault damage zones
journal, March 2004
- Kim, Young-Seog; Peacock, David C. P.; Sanderson, David J.
- Journal of Structural Geology, Vol. 26, Issue 3
Permeability of fault-related rocks, and implications for hydraulic structure of fault zones
journal, November 1997
- Evans, James P.; Forster, Craig B.; Goddard, James V.
- Journal of Structural Geology, Vol. 19, Issue 11
A reservoir analysis of the Denver earthquakes: A case of induced seismicity
journal, February 1981
- Hsieh, Paul A.; Bredehoeft, John D.
- Journal of Geophysical Research: Solid Earth, Vol. 86, Issue B2
Permeability of the continental crust: dynamic variations inferred from seismicity and metamorphism
journal, February 2010
- Ingebritsen, S. E.; Manning, C. E.
- Geofluids
Hydrogeologic Controls on Induced Seismicity in Crystalline Basement Rocks Due to Fluid Injection into Basal Reservoirs: Y. Zhang et al. Ground Water xx, no. xx: xx-xx
journal, June 2013
- Zhang, Yipeng; Person, Mark; Rupp, John
- Groundwater, Vol. 51, Issue 4
Is the permeability of crystalline rock in the shallow crust related to depth, lithology or tectonic setting?
journal, September 2014
- Ranjram, M.; Gleeson, T.; Luijendijk, E.
- Geofluids, Vol. 15, Issue 1-2
Internal structure and permeability of major strike-slip fault zones: the Median Tectonic Line in Mie Prefecture, Southwest Japan
journal, January 2003
- Wibberley, Christopher A. J.; Shimamoto, Toshihiko
- Journal of Structural Geology, Vol. 25, Issue 1
Chemical changes and fluid-rock interaction in faults of crystalline thrust sheets, northwestern Wyoming, U.S.A.
journal, April 1995
- Goddard, James V.; Evans, James P.
- Journal of Structural Geology, Vol. 17, Issue 4
Spatial and mechanical controls on normal fault populations
journal, February 1996
- Knott, Steven D.; Beach, Alastair; Brockbank, Paul J.
- Journal of Structural Geology, Vol. 18, Issue 2-3
Induced seismicity associated with fluid injection into a deep well in Youngstown, Ohio: INDUCED SEISMICITY IN YOUNGSTOWN, OHIO
journal, July 2013
- Kim, Won-Young
- Journal of Geophysical Research: Solid Earth, Vol. 118, Issue 7
Controls on damage zone asymmetry of a normal fault zone: outcrop analyses of a segment of the Moab fault, SE Utah
journal, October 2005
- Berg, Silje S.; Skar, Tore
- Journal of Structural Geology, Vol. 27, Issue 10
Fault zone architecture and permeability structure
journal, January 1996
- Caine, Jonathan Saul; Evans, James P.; Forster, Craig B.
- Geology, Vol. 24, Issue 11
Fault activation and induced seismicity in geological carbon storage – Lessons learned from recent modeling studies
journal, December 2016
- Rutqvist, Jonny; Rinaldi, Antonio P.; Cappa, Frederic
- Journal of Rock Mechanics and Geotechnical Engineering, Vol. 8, Issue 6
Sharp increase in central Oklahoma seismicity since 2008 induced by massive wastewater injection
journal, July 2014
- Keranen, K. M.; Weingarten, M.; Abers, G. A.
- Science, Vol. 345, Issue 6195
Potentially induced earthquakes in Oklahoma, USA: Links between wastewater injection and the 2011 Mw 5.7 earthquake sequence
journal, June 2013
- Keranen, Katie M.; Savage, Heather M.; Abers, Geoffrey A.
- Geology, Vol. 41, Issue 6
How faulting keeps the crust strong
journal, January 2000
- Townend, John; Zoback, Mark D.
- Geology, Vol. 28, Issue 5
Types of permeable fractures in granite
journal, January 2005
- Sausse, J.; Genter, A.
- Geological Society, London, Special Publications, Vol. 240, Issue 1
Geological implications of a permeability-depth curve for the continental crust
journal, January 1999
- Ingebritsen, S. E.; Manning, Craig E.
- Geology, Vol. 27, Issue 12
Hydromechanical properties and alteration of natural fracture surfaces in the Soultz granite (Bas-Rhin, France)
journal, April 2002
- Sausse, Judith
- Tectonophysics, Vol. 348, Issue 1-3
A Rare Moderate‐Sized ( M w 4.9) Earthquake in Kansas: Rupture Process of the Milan, Kansas, Earthquake of 12 November 2014 and Its Relationship to Fluid Injection
journal, September 2016
- Choy, George L.; Rubinstein, Justin L.; Yeck, William L.
- Seismological Research Letters, Vol. 87, Issue 6
Hydraulic conductivity of fractured upper crust: insights from hydraulic tests in boreholes and fluid-rock interaction in crystalline basement rocks
journal, September 2014
- Stober, I.; Bucher, K.
- Geofluids, Vol. 15, Issue 1-2
Works referencing / citing this record:
Earthquake Swarms Triggered by Groundwater Extraction Near the Dead Sea Fault
journal, July 2019
- Wetzler, Nadav; Shalev, Eyal; Göbel, Thomas
- Geophysical Research Letters, Vol. 46, Issue 14