Thermal stability of the electron spin resonance signal of modern continental barite

Abstract

The electron spin resonance (ESR) method has been successfully applied to dating hydrothermal barite; however, there have been few studies of modern continental barite, such as that generated by fault movement or in sedimentary deposits. To better understand the geological processes involved in the formation of continental barite, its thermal characteristics and age firstly need to be defined. In this study, one fault barite sample and two sedimentary barite samples were obtained from continental sites in China for ESR signal thermal stability experiments. Microwave-power experiments indicate that 0.5 mW produces the maximum ESR signal intensity and the highest signal-to-noise ratio. Stepwise-heating results reveal that ESR signal intensities remain stable below 100 °C then show an increasing trend that peaks at ∼180 °C, following which they decrease rapidly between 180 and 320 °C and disappear at ∼380 °C. Isothermal heating results show that ESR signal intensities remain stable within a temperature range of 100–200 °C but show a decreasing trend for temperatures of 240–320 °C. These results indicate that the thermal decay of the ESR signal intensity for the three studied continental barites follows second-order decay kinetics. The thermal lifetimes calculated for the three samples are 6.3 × 108, 7.5 × 107, and 8.7 × 106 a, respectively. Thus, barite ESR dating can be used to date related geological events since early Pleistocene.