text: Mass spectrometry is used to separate and measure distinct isotopes present in a sample. Archaeologists typically employ isotope ratio mass spectrometers or IRMSs, consisting of an inlet system, ion source, mass analyser and multiple ion detectors.
  The sample is usually introduced into the mass spectrometer as a gas, with oxygen and carbon being introduced as carbon dioxide.
  Strontium is too unstable to be easily handled in gas form, instead, it is evaporated and ionised in a vacuum. This use of a solid source is referred to as thermal ionisation mass spectrometry or TIMS. More recently, strontium isotopes have been at the centre of discussion and investigation into the use of laser ablation inductively coupled mass spectrometry (ICP-MS), which is also of interest due to its less invasive nature.
  Electron bombardment ionises the gas, allowing the molecules to be focused into a beam which is then split by mass into smaller beams - forming a "mass spectrum". The relative intensities of the different beams is then measured in the ion collector and relayed as isotope ratios.