Science. 1993 Oct 15;262(5132):412-6. doi: 10.1126/science.262.5132.412.
Geomagnetic paleointensity determinations from radiocarbon-dated lava flows on the island of Hawaii provide an estimate of broad trends in paleointensity for Holocene time and offer a glimpse of intensity variations near the end of the last glacial period. When the data from Hawaii are compared with others worldwide, the intensity of the geomagnetic field seems to have been reduced from the Holocene average by about 35 percent between 45,000 and 10,000 years ago. A long-term reduction of this magnitude is compatible with reported increases in the production rate of cosmogenic nuclides during the same interval.
从夏威夷岛上的放射性碳定年熔岩流中得出的地磁强度测量值为全新世时期的地磁强度提供了一个大致趋势的估计,并提供了在上一个冰河期末期强度变化的一个 glimpse。当夏威夷的数据与全球其他数据进行比较时,45000 到 10000 年前,磁场强度似乎比全新世平均值降低了约 35%。在同一时期,这种幅度的长期减少与报告的宇宙成因核素生成率的增加是一致的。