According to experts, thanks to this substance, slow shifts occur on the fault line instead of sudden ruptures. This can reduce the risk of large and devastating earthquakes.
At first examination, the research team thought that the structure that reduces friction was graphite. However, as a result of laboratory analysis, the substance “graphene oxide”, which is much more slippery than graphite, was detected. Scientists stated that this substance acts like a natural lubricant between rock surfaces.
Researchers assess that graphene oxide may re-form as the fault moves. This means that the fault line may have developed a natural balance mechanism within itself.
Experts state that the discovery in question may play an important role in earthquake predictions and risk analyzes in the future.
