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DOI: 10.1002/2015GL066306
论文题名:
The effect of hydrostatic pressure up to 1.61 GPa on the Morin transition of hematite-bearing rocks: Implications for planetary crustal magnetization
作者: Bezaeva N.S.; Demory F.; Rochette P.; Sadykov R.A.; Gattacceca J.; Gabriel T.; Quesnel Y.
刊名: Geophysical Research Letters
ISSN: 0094-8352
EISSN: 1944-8083
出版年: 2015
卷: 42, 期:23
起始页码: 10188
结束页码: 10196
语种: 英语
英文关键词: hematite-bearing rock ; hydrostatic pressure ; Martian magnetic anomalies ; Morin transition
Scopus关键词: Hematite ; Hydraulics ; Hydrostatic pressure ; Magnetization ; Quantum interference devices ; SQUIDs ; Banded iron formations ; Crustal magnetization ; High pressure cells ; Isothermal remanent magnetization ; Magnetic anomalies ; Morin transitions ; Pressure applications ; Superconducting quantum interference ; Pressure effects ; crustal structure ; hematite ; hydrostatic pressure ; magnetic anomaly ; magnetic field ; magnetization ; magnetometer ; Mars ; remanent magnetization
英文摘要: We present new experimental data on the dependence of the Morin transition temperature (TM) on hydrostatic pressure up to 1.61 GPa, obtained on a well-characterized multidomain hematite-bearing sample from a banded iron formation. We used a nonmagnetic high-pressure cell for pressure application and a Superconducting Quantum Interference Device magnetometer to measure the isothermal remanent magnetization (IRM) under pressure on warming from 243 K to room temperature (T0). IRM imparted at T0 under pressure in 270 mT magnetic field (IRM270mT) is not recovered after a cooling-warming cycle. Memory effect under pressure was quantified as IRM recovery decrease of 10%/GPa. TM, determined on warming, reaches T0 under hydrostatic pressure 1.38-1.61 GPa. The pressure dependence of TM up to 1.61 GPa is positive and essentially linear with a slope dTM/dP = (25 ± 2) K/GPa. This estimate is more precise than previous ones and allows quantifying the effect of a pressure wave on the upper crust magnetization, with special emphasis on Mars. © 2015. American Geophysical Union. All Rights Reserved.
URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84953635024&doi=10.1002%2f2015GL066306&partnerID=40&md5=59781a0aea10e0353a1610f5dac1151d
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/7968
Appears in Collections:科学计划与规划
气候变化与战略

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作者单位: Earth Physics Department, Faculty of Physics, M.V. Lomonosov Moscow State University, Moscow, Russian Federation

Recommended Citation:
Bezaeva N.S.,Demory F.,Rochette P.,et al. The effect of hydrostatic pressure up to 1.61 GPa on the Morin transition of hematite-bearing rocks: Implications for planetary crustal magnetization[J]. Geophysical Research Letters,2015-01-01,42(23).
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