Helium leakage from Earth's mantle in Los Angeles Basin
New discoveries about Newport-Inglewood Fault Zone in Los Angeles Basin
- June 29, 2015
- University of California - Santa Barbara
- Geologists have found evidence of helium leakage from Earth's mantle along a 30-mile stretch of the Newport-Inglewood Fault Zone in the Los Angeles Basin. Using samples of casing gas from two dozen oil wells ranging from LA's Westside to Newport Beach in Orange County, researchers discovered that more than one-third of the sites -- some of the deepest ones -- show evidence of high levels of helium-3 (3He).
UC Santa Barbara geologist Jim Boles has found evidence of helium leakage from Earth's mantle along a 30-mile stretch of the Newport-Inglewood Fault Zone in the Los Angeles Basin. Using samples of casing gas from two dozen oil wells ranging from LA's Westside to Newport Beach in Orange County, Boles discovered that more than one-third of the sites -- some of the deepest ones -- show evidence of high levels of helium-3 (3He).
Considered primordial, 3He is a vestige of the Big Bang. Its only terrestrial source is the mantle. Leakage of 3He suggests that the Newport-Inglewood fault is deeper than scientists previously thought. Boles's findings appear in Geochemistry, Geophysics, Geosystems (G-Cubed), an electronic journal of the American Geophysical Union and the Geochemical Society.
"The results are unexpected for the area, because the LA Basin is different from where most mantle helium anomalies occur," said Boles, professor emeritus in UCSB's Department of Earth Science. "The Newport-Inglewood fault appears to sit on a 30-million-year-old subduction zone, so it is surprising that it maintains a significant pathway through the crust."
When Boles and his co-authors analyzed the 24 gas samples, they found that high levels of 3He inversely correlate with carbon dioxide (CO2), which Boles noted acts as a carrier gas for 3He. An analysis showed that the CO2 was also from the mantle, confirming leakage from deep inside Earth.
Blueschist found at the bottom of nearby deep wells indicates that the Newport-Inglewood fault is an ancient subduction zone -- where two tectonic plates collide -- even though its location is more than 40 miles west of the current plate boundary of the San Andreas Fault System. Found 20 miles down, blueschist is a metamorphic rock only revealed when regurgitated to the surface via geologic upheaval.
"About 30 million years ago, the Pacific plate was colliding with the North American plate, which created a subduction zone at the Newport-Inglewood fault," Boles explained. "Then somehow that intersection jumped clear over to the present San Andreas Fault, although how this occurred is really not known. This paper shows that the mantle is leaking more at the Newport-Inglewood fault zone than at the San Andreas Fault, which is a new discovery."
The study's findings contradict a scientific hypothesis that supports the existence of a major décollement -- a low-angle thrust fault -- below the surface of the LA Basin. "We show that the Newport-Inglewood fault is not only deep-seated but also directly or indirectly connected with the mantle," Boles said.
"If the décollement existed, it would have to cross the Newport-Inglewood fault zone, which isn't likely," he added. "Our findings indicate that the Newport-Inglewood fault is a lot more important than previously thought, but time will tell what the true importance of all this is."
Study co-authors include Grant Garven of Tufts University; Hilario Camacho of Occidental Oil and Gas Corp.; and John Lupton of the National Oceanic and Atmospheric Administration's Pacific Marine Environmental Laboratory.
This research was supported by the U.S. Department of Energy's Office of Science and Office of Basic Energy Sciences and by the NOAA Pacific Marine Environmental Laboratory.
- J. R. Boles, G. Garven, H. Camacho, J. E. Lupton. Mantle helium along the Newport-Inglewood fault zone, Los Angeles basin, California-A leaking paleo-subduction zone. Geochemistry, Geophysics, Geosystems, 2015; DOI: 10.1002/2015GC005951