摘要
Paleomagnetic study from Tongjing basalts, Shandong Province, China, provides a record of the transitional field behaviour for the Matuyama-Brunhes. Based on the record the transitional field configurations are studied. The reasons that make the virtual geomagnetic pole (VGP) at the low latitude are researched.
Paleomagnetic study from Tongjing basalts, Shandong Province, China, provides a record of the transitional field behaviour for the Matuyama-Brunhes. Based on the record the transitional field configurations are studied. The reasons that make the virtual geomagnetic pole (VGP) at the low latitude are researched.
