해남지역에 분포하는 화산암과 화산쇄설성 퇴적암으로부터 고지자기 연구를 실시하고, 국내에서는 처음으로 특성잔류자화를 구하였다. 이들 화산암류는 K-Ar 전암분석에 의해, 일부 전기백악기를 제외하면, 주로 후기백악기의 연대를 나타내고 있다. 이들 암석의 특성잔류자화 방향을 나타내는 자성광물은 자철석으로 판명되었다. 연구지역의 후기백악기 암석들로부터 구한 평균자화방향을 Dm/Im=21.4$^{0}$ /57.1$^{0}$ ($\alpha_{95}=13.4^{\circ}$, k=350.0)으로서, 이로부터 구한 고지자기극의 위치는 $72.5^{\circ}N/199.9^{\circ}E$ (dp/dm=$14.2^{\circ}/19.5^{\circ}$)이다. 이 결과는 80~90 Ma의 유라시아 대륙으로부터 구한 고지자기극의 위치와 통계적으로 일치하며, 연구지역을 포함한 한반도가 후기백악기 이래로 안정되어 왔음을 시사한다. 연구지역의 전기 백악기의 암석들로부터 구한 평균자화방향은 동시기의 경상분지의 방향과 편의를 나타내며, 이것은 해남지역을 포함하는 소지괴가 전기백악기 말과 후기백악기 초 사이에 반시계방향의 수평회전운동을 경험했을 가능성을 제시하여 준다.
해남지역에 분포하는 화산암과 화산쇄설성 퇴적암으로부터 고지자기 연구를 실시하고, 국내에서는 처음으로 특성잔류자화를 구하였다. 이들 화산암류는 K-Ar 전암분석에 의해, 일부 전기백악기를 제외하면, 주로 후기백악기의 연대를 나타내고 있다. 이들 암석의 특성잔류자화 방향을 나타내는 자성광물은 자철석으로 판명되었다. 연구지역의 후기백악기 암석들로부터 구한 평균자화방향을 Dm/Im=21.4$^{0}$ /57.1$^{0}$ ($\alpha_{95}=13.4^{\circ}$, k=350.0)으로서, 이로부터 구한 고지자기극의 위치는 $72.5^{\circ}N/199.9^{\circ}E$ (dp/dm=$14.2^{\circ}/19.5^{\circ}$)이다. 이 결과는 80~90 Ma의 유라시아 대륙으로부터 구한 고지자기극의 위치와 통계적으로 일치하며, 연구지역을 포함한 한반도가 후기백악기 이래로 안정되어 왔음을 시사한다. 연구지역의 전기 백악기의 암석들로부터 구한 평균자화방향은 동시기의 경상분지의 방향과 편의를 나타내며, 이것은 해남지역을 포함하는 소지괴가 전기백악기 말과 후기백악기 초 사이에 반시계방향의 수평회전운동을 경험했을 가능성을 제시하여 준다.
A mean characteristic remanent magnetization was obtained for the first time in Korea from volcanic and pyroclastic sedimentary rocks distributed in Haenam Area, located in southwestern part of the Korean Peninsula. The age of the prevailing rocks in this area belongs mostly to Late Cretaceous, with...
A mean characteristic remanent magnetization was obtained for the first time in Korea from volcanic and pyroclastic sedimentary rocks distributed in Haenam Area, located in southwestern part of the Korean Peninsula. The age of the prevailing rocks in this area belongs mostly to Late Cretaceous, with a few exceptions of Early Cretaceous, mainly based on K/Ar whole rock age dating. Characteristic remanent magnetizations of these have both normal and reverse polarities with antipodal direction, which were interpreted to be the primary remanent magnetizations obtained by the ambient Earth's magnetic field at the time of formation of the concerned rocks. The source magnetic minerals of the remanent magnetization has been identified as magnetite. The mean direction of characteristic remanent magnetization obtained from the Late Cretaceous rocks in this study is Dm/Im=21.4 supper(o)/57.1 supper(o) (${\alpha}_{95}=13.4^{\circ}$, k=350.0). The paleomagnetic pole position calculated from this result for the Late Cretaceous, is $72.5^{\circ}N/199.9^{\circ}E$ (dp/dm= $14.2^{\circ}/19.5^{\circ}E$), which matches well with those of 80 Ma ($76.2^{\circ}N/198.9^{\circ}E$) and 90 Ma ($76.2^{\circ}N/200.1^{\circ}E$) of the Eurasian Continent's APWP (Apparent Polar Wander Path). This result strongly indicates that the studied area, belonging to the Eurasian Continent, have suffered very little geotectonic movement after the Late Cretaceous. The deflection of declination of remanence from Early Cretaceous rocks in the study area may indicate that the micro-block was counterclockwisely rotated with vertical axis between the late of Early Cretaceous and the early of Late Cretaceous.
A mean characteristic remanent magnetization was obtained for the first time in Korea from volcanic and pyroclastic sedimentary rocks distributed in Haenam Area, located in southwestern part of the Korean Peninsula. The age of the prevailing rocks in this area belongs mostly to Late Cretaceous, with a few exceptions of Early Cretaceous, mainly based on K/Ar whole rock age dating. Characteristic remanent magnetizations of these have both normal and reverse polarities with antipodal direction, which were interpreted to be the primary remanent magnetizations obtained by the ambient Earth's magnetic field at the time of formation of the concerned rocks. The source magnetic minerals of the remanent magnetization has been identified as magnetite. The mean direction of characteristic remanent magnetization obtained from the Late Cretaceous rocks in this study is Dm/Im=21.4 supper(o)/57.1 supper(o) (${\alpha}_{95}=13.4^{\circ}$, k=350.0). The paleomagnetic pole position calculated from this result for the Late Cretaceous, is $72.5^{\circ}N/199.9^{\circ}E$ (dp/dm= $14.2^{\circ}/19.5^{\circ}E$), which matches well with those of 80 Ma ($76.2^{\circ}N/198.9^{\circ}E$) and 90 Ma ($76.2^{\circ}N/200.1^{\circ}E$) of the Eurasian Continent's APWP (Apparent Polar Wander Path). This result strongly indicates that the studied area, belonging to the Eurasian Continent, have suffered very little geotectonic movement after the Late Cretaceous. The deflection of declination of remanence from Early Cretaceous rocks in the study area may indicate that the micro-block was counterclockwisely rotated with vertical axis between the late of Early Cretaceous and the early of Late Cretaceous.
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