17:15 〜 18:45
[SGL19-P03] 瑞浪層群宿洞層（中新統）の古地磁気：パレオパラドキシアは日本海拡大を見たか？
キーワード：磁化率異方性、古地磁気、パレオパラドキシア、瑞浪層群、回転運動、日本海拡大
Magnetic measurements were performed on the sandstone block containing a paleoparadoxiid fossil specimen from the Shukunohora Formation of the Miocene Mizunami Group in central Japan. Stepwise demagnetization suggests the presence of both magnetite and greigite, with the latter being probably authigenic minerals formed during early diagenesis. The anisotropy of magnetic susceptibility (AMS) analysis shows a highly variable magnetic fabric with no preferred orientation, suggesting the absence of a consistent grain alignment in the sandstones. This likely reflects disturbances by storms or bioturbation. The sandstone block-mean remanent magnetization direction may be attributed to chemical remanent magnetization (CRM) carried by greigite and, therefore, may not represent the paleofield direction at the time of deposition. However, assuming CRM acquisition during early diagenesis shortly after deposition, the deposition was during a reverse polarity period around 16.5 Ma, potentially either Chron C5Cr (17.154-16.637 Ma), C5Cn.2r (16.532-16.434 Ma), or C5Cn.1r (16.351-16.261 Ma). The deviation of the block-mean remanent magnetization direction from an expected paleofield direction suggests an approx. 20-30° clockwise tectonic rotation for the crust beneath the study area relative to the Asian continent. This rotation coincides with the clockwise rotation of Southwest Japan during the major opening of the Japan Sea, suggesting the paleoparadoxiid specimen lived amidst this tectonic event.