eprintid: 2027
rev_number: 10
eprint_status: archive
userid: 9
dir: disk0/00/00/20/27
datestamp: 2017-12-14 08:47:05
lastmod: 2017-12-14 08:47:05
status_changed: 2017-12-14 08:47:05
type: conference_item
metadata_visibility: show
creators_name: Boak, Jeremy
corp_creators: University of Oklahoma
title: Patterns of induced seismicity in central and northwest Oklahoma
subjects: MP2
subjects: RU6
subjects: SHC
subjects: SHU
divisions: IP14
full_text_status: none
pres_type: speech
keywords: pore pressure, induced seismicity, hydrology, Basement, earthquake
abstract: Oklahoma experienced an average of 1.6 earthquakes of Magnitude 3 or greater (M3.0+) from the 1980s through 2008. Since that time, seismicity has increased to 907 M3.0+ earthquakes in 2015. More than 95% of these earthquakes occur over only ~17% of the area of Oklahoma (Figure 1). This pattern is generally attributed to increased injection of saline formation water co-produced along with oil and gas into the underpressured and relatively permeable Arbuckle Group, which lies directly on top of Precambrian crystalline basement (for example, Walsh and Zoback, 2015). Pressure communication from the Arbuckle to faults in the basement is interpreted to have reduced effective normal stress on the faults. This stress reduction allows faults aligned favorable with respect to the stress field in Oklahoma (SHMax = N 85° E) to move. This paper discusses the evolution of this seismicity, the regulatory actions taken to reduce seismicity by reducing deep injection, and the importance of declining oil price in reducing injected volumes in advance of full implementation of these regulatory directives
date: 2016-10-19
event_title: SEG International Exposition and 86th Annual Meeting
event_type: conference
official_url: https://doi.org/10.1190/segam2016-13960154.1
access_IS-EPOS: limited
owner: Publisher
citation:   Boak, Jeremy  (2016) Patterns of induced seismicity in central and northwest Oklahoma.  In: SEG International Exposition and 86th Annual Meeting.