Skip to main content

Table 1 Mean ChRM directions for sites

From: Paleomagnetic study of basaltic rocks from Baengnyeong Island, Korea: efficiency of the Tsunakawa–Shaw paleointensity determination on non-SD-bearing materials and implication for the early Pliocene geomagnetic field intensity

B1 + B29/11347.338.34.9113.4
  1. n/N, the number of specimen-level ChRM determinations used in mean calculation/the number of specimens measured; Dm (Im), declination (inclination) of mean ChRM determination; α95, 95% confidence limit; and k, precision parameter