机译:有机富集脉状湖泊沉积物沉积后剩余磁化锁定深度的估算
Department of Earth Sciences - Geophysics, Uppsala University, Villavaegen 16, SE-752 36 Uppsala, Sweden,Department of Geology - Quaternary Sciences, Lund University, Soelvegatan 12, SE-223 62 Lund, Sweden;
Department of Geology - Quaternary Sciences, Lund University, Soelvegatan 12, SE-223 62 Lund, Sweden;
Department of Geology - Quaternary Sciences, Lund University, Soelvegatan 12, SE-223 62 Lund, Sweden;
Department of Geology - Quaternary Sciences, Lund University, Soelvegatan 12, SE-223 62 Lund, Sweden;
Geology and Geophysics, School of Environmental Sciences, University of Liverpool, Liverpool, United Kingdom;
Department of Geology - Quaternary Sciences, Lund University, Soelvegatan 12, SE-223 62 Lund, Sweden;
Department of Geology - Quaternary Sciences, Lund University, Soelvegatan 12, SE-223 62 Lund, Sweden;
GFZ German Research Centre for Geosciences, Section 5.2 Climate dynamics and Landscape Evolution, Telegrafenberg, D-14473 Potsdam, Germany;
Paleomagnetic secular variation; Post-depositional remanent magnetization; Lock-in depth; Varves;
机译:通过古磁场模型评估的精确定年脉沉积物中的沉积后剩余磁化锁定深度
机译:由〜(10)Be和古磁记录通过Matuyama-Brunhes边界推导出的沉积物的沉积后剩余磁化锁定
机译:为什么地磁偏移并不总是记录在沉积物中?沉积后剩余磁化锁定模型的约束
机译:磁偶极子互相互相关方法,用于估计磁化方向下的磁化磁化强度
机译:研究基质性质对沉积物中沉积后剩余磁化强度(pDRM)的影响。
机译:IODP站点U1467(Maldives平台)早期上新世沉积物的特征剩磁和磁特性数据集
机译:有机富湖变质湖泊沉积物中沉积后剩余磁化锁定深度的估算