希腊查尔基迪基沉积物岩心的古地磁和岩石磁学性质

E. Aidona , D. Kondopoulou , A. Georgakopoulos
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引用次数: 5

摘要

对Chalkidiki半岛4个深层钻孔(1-3.1km)的始新世和渐新世岩芯样本进行了详细的古地磁调查。低场磁化率和自然剩余磁化强度(NRM)都表明材料的磁化强度相当弱。134个样品已经经历了逐步的热消磁或交变场消磁。两种程序都表明,NRM是由磁铁矿携带的。等温剩余磁化(IRM)采集曲线表明磁铁矿占主导地位。最后,为了更准确地表征样品的磁性矿物学,对12个薄片进行了研究。本次调查揭示了磁铁矿和黄铁矿的存在。一般来说,在这些岩石中观察到的特征剩磁的倾角远低于预期的倾角,但与从陆地上的地层中获得的倾角一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Palaeomagnetic and rock magnetic properties of sediment cores from Chalkidiki, Greece
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