Additional file 12 of New absolute paleomagnetic intensity data from Cenozoic basalts of Northeast China and exploring rock-magnetic parameters for efficient sample preselection on the Tsunakawa–Shaw paleointensity method

Additional file 12: Table S8. Comparison of API determinations between the TS and Coe–Thellier (vacuum) methods with variable acceptance criteria. The TS API value for each sample was obtained from the result of a single specimen belonging to the sample, except for sample 14,181-E, which yielded a sample-level API value by calculating the mean value from the two specimen-level results. Each sample-level Coe–Thellier API value with certain criteria was obtained by averaging all API values that were calculated to meet certain criteria for a single specimen-level result.