Key points are not available for this paper at this time.
Research Article| October 01, 1989 Earthquakes triggered by fluid extraction P. Segall P. Segall 1U.S. Geological Survey, Menlo Park, California 940252Department of Geophysics, Stanford University, Stanford, California 94305-2215 Search for other works by this author on: GSW Google Scholar Author and Article Information P. Segall 1U.S. Geological Survey, Menlo Park, California 940252Department of Geophysics, Stanford University, Stanford, California 94305-2215 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1989) 17 (10): 942–946. https://doi.org/10.1130/0091-7613(1989)0172.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation P. Segall; Earthquakes triggered by fluid extraction. Geology 1989;; 17 (10): 942–946. doi: https://doi.org/10.1130/0091-7613(1989)0172.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Seismicity is correlated in space and time with production from some oil and gas fields where pore pressures have declined by several tens of megapascals. Reverse faulting has occurred both above and below petroleum reservoirs, and normal faulting has occurred on the flanks of at least one reservoir. The theory of poroelasticity requires that fluid extraction locally alter the state of stress. Calculations with simple geometries predict stress perturbations that are consistent with observed earthquake locations and focal mechanisms. Measurements of surface displacement and strain, pore pressure, stress, and poroelastic rock properties in such areas could be used to test theoretical predictions and improve our understanding of earthquake mechanics. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
P. Segall (Sun,) studied this question.