Exploring the potential of acquisition curves of the anhysteretic remanent magnetization as a tool to detect subtle magnetic alteration induced by heating

Recently, many new methods and improved protocols to determine the absolute paleointensity of lavas reliably have been proposed. Here we study eight recent flows from three different volcanic edifices (Mt. Etna, La Palma and Hawaii) with the so-called multispecimen parallel differential pTRM (MSP) method including the recently proposed domain-state correction (MSP-DSC) (Fabian and Leonhardt, 2010). Surprisingly, apart from approximately correct paleointensity values, we observe major underestimates of the paleofield. These deviations are possibly related to alteration that is not revealed by rock-magnetic analysis. We explore the potential of high-resolution acquisition curves of the anhysteretic remanent magnetization (ARM) to detect subtle alteration in the samples. It appears that assessing changes in the ARM acquisition properties before and after heating to the desired MSP temperature discriminates between underestimates and approximately correct estimations of the paleofield in the outcomes of the MSP-DSC protocol. By combining observations from the domain-state corrected MSP protocol and ARM acquisition experiments before and after heating, an extended MSP protocol is suggested which makes it possible to assess the best set temperature for the MSP-DSC protocol and to label MSP results as being approximately correct, or an underestimate of the paleofield.