A new analysis of historical seismic data conducted by The University of Texas at Austin, SMU and other academies has found that earthquake activity in West Texas around Pecos has increased dramatically since 2009.
The study, published Nov. 4, 2019, in the Journal of Geophysical Research: Solid Earth, is important because it leverages old, unmined data to track seismic activity over nearly the past two decades – much further back than other studies— to show that activity has increased during the past decade in an area of the Permian Basin that is being heavily developed for oil and gas. Although researchers have generally thought that to be true, the statewide TexNet earthquake monitoring system has been gathering data since only 2017, making it impossible to definitely determine when the cluster of seismic activity around Pecos really began.
The researchers were able to extend the seismic record of the area by turning to the older TXAR system near Lajitas about 150 miles to the south. TXAR is an array of 10 seismographs installed in the 1990s by scientists at SMU (Southern Methodist University) to help track nuclear testing across the world, said lead author Cliff Frohlich, a senior research scientist emeritus at the University of Texas Institute for Geophysics (UTIG).
“Especially for these West Texas earthquakes, we would like to get some information about when they started,” Frohlich said. “I really saw this as a way to bridge the gap before TexNet.”
The TXAR system is some distance from Pecos, but Frohlich said the equipment is highly sensitive and that the area is remote and seismically very quiet, making the system perfect for picking up vibrations from explosions across the world or from earthquakes 150 miles away. Frohlich worked with Chris Hayward, director of SMU’s Geophysics Research Program, to create a method to derive the earthquake data from the international data TXAR collects and build an earthquake catalog for the Delaware Basin near Pecos from 2000 to 2017.
By analyzing data from 2000 to 2017, scientists were able to document more than 7,000 seismic events near Pecos that were determined by the team to be earthquakes. Data on these seismic events had to be manually reviewed to ensure they were in fact earthquakes and not a false detection. This was done by Frohlich and Julia Rosenblit, who was an SMU intern at the time.
Multiple events first started occurring in 2009, when 19 earthquakes of at least magnitude 1 were documented. The rate increased over time, with more than 1,600 earthquakes of magnitude 1 or greater in 2017. Most were so small that no one felt them.
The study shows a correlation between earthquake activity in the area and an increase in oil and gas activity but doesn’t make an effort to directly tie the two together as other studies have done.
“West Texas now has the highest seismicity rates in the state,” said Heather DeShon, study co-author and associate professor at SMU’s Roy M. Huffington Department of Earth Sciences. “What remained uncertain is when the earthquakes actually started. This study addresses that.”
This study is the latest in a comprehensive effort to determine what is causing an increase in seismic activity in Texas and how oil and gas operations can be managed to minimize that human-induced element. The state approved the TexNet system in 2015, which is operated in tandem with research efforts by the Center for Integrated Seismicity Research (CISR).
Co-author Peter Hennings, who leads CISR and is a Senior Research Scientist at the UT Bureau of Economic Geology said that fundamental research like this latest study is vital when trying to unravel such a complicated problem.
“The obvious next step is exactly what the University of Texas is doing – conducting these careful studies on the relationship between earthquakes and their human and natural causes to build an integrated understanding,” Hennings said.
SMU seismologists have also been the lead or co-authors of a series of studies on Texas earthquakes. For instance, UT Austin and SMU found that earthquakes triggered by human activity have been happening in Texas since 1925, and they have been widespread throughout the state ever since. In addition, SMU research showed that many of the Dallas-Fort Worth earthquakes were triggered by increases in pore pressure–the pressure of groundwater trapped within tiny spaces inside rocks in the subsurface.
The Bureau of Economic Geology and UTIG are units of the UT Jackson School of Geosciences. Scientists from SMU, Portland State University, the University of Oklahoma and the French institute IFREMER also worked on the study.