Geomagnetic events and relative palaeointensity variations during the past 300 ka as recorded in Kolbeinsey Ridge sediments, Iceland Sea: indication for a strongly variable geomagnetic field

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Geomagnetic events and relative palaeointensity variations during the past 300 ka as recorded in Kolbeinsey Ridge sediments, Iceland Sea: indication for a strongly variable geomagnetic field

机译：冰岛海的Kolbeinsey Ridge沉积物中记录的过去300 ka内的地磁事件和相对古强度变化：指示强烈变化的地磁场

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《International Journal of Earth Sciences》 |1999年第1期|116-131|共16页
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正文语种 eng
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Magnetostratigraphy; Geomagnetic field reversals; Palaeointensity variations; Brunhes Chron; Rock magnetism;

机译：磁地层学;地磁场反转;古强度变化;布鲁内斯年代学;岩石磁性;
入库时间 2022-08-18 03:40:11

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1. Relative paleointensity of the geomagnetic field during Brunhes Chron recorded in North Pacific deep-sea sediment cores: orbital influence? [J] . Toshitsugu Yamazaki Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System . 1999,第1a2期

机译：在北太平洋深海沉积物核中记录的Brunhes Chron期间地磁场的相对古强度：轨道影响？
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3. A high resolution authigenic ~(10)Be/~9Be record of geomagnetic moment variations over the last 300 ka from sedimentary cores of the Portuguese margin [J] . Julien Carcaillet, Didier L. Bourles, Nicolas Thouveny, Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System . 2004,第3a4期

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4. Study of Forbush Decrease Event and Associated Geomagnetic Field Variation During Space Radiation Storm [C] . Sujeet K.Mishra, Subhash C.Kaushik International Cosmic Ray Conference . 2003

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5. High-resolution magnetic records in pelagic sediments: The Oligocene geomagnetic field, the Brunhes/Matuyama geomagnetic reversal, and rock magnetic changes at the Eocene/Oligocene boundary. [D] . Hartl, Paul David. 1996

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7. FTE (Flux Transfer Event) Like Variations in the Geomagnetic Field at Ground Based Conjugate Stations in the Cusp Regions [R] . Trivedi, N. B., Lanzerotti, L. J., Wolf, A., 1987

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Geomagnetic events and relative palaeointensity variations during the past 300 ka as recorded in Kolbeinsey Ridge sediments, Iceland Sea: indication for a strongly variable geomagnetic field

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