Magnetic and Paleomagnetic Characterization of the Ivrea-Verbano Lower Crust Body (NW Italy): Assessing the Magnetization of Variscan-Age Lower Crust

IF 3.9 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Gaia Siravo, Fabio Speranza, Liliana Minelli, Michele Zucali, Eugenio Fazio, Chiara Caricchi, Lilla Spagnuolo
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Abstract

The source of high-intensity magnetic anomalies from (mostly Precambrian) lower crust of continent interiors has long been debated, as it requires speculative rocks yielding 2–6 A/m magnetization. We report on the magnetic and paleomagnetic investigation of the Ivrea-Verbano Zone (IVZ), Western Alps, where metamorphic and intrusive lower crust rocks of Late Variscan-Permian ages are exposed. We sampled 39 oriented sites along the Cannobina, Ossola, Strona, and Sesia valleys/sections. Low (0.27–2.1·10−3 SI) magnetic susceptibility (k) values were measured in metapelite-metabasite metamorphic rocks from the Ossola and Strona valleys. There only two metabasite (one amphibolite and one granulite) out of 25 metamorphic sites containing pseudo-single domain (PSD) magnetite yield 0.48–1.1·10−1 SI k values that remain constant until 550°C heating. K of gabbros-granodiorites from Sesia valley mimic low values from metamorphic rocks, whereas at Cannobina valley one gabbro and one mafic granulite display values comparable to the two strongly magnetic sites from Ossola/Strona valleys. Peridotite lenses at Balmuccia and Finero similarly yielded low (0.24–5.5·10−3 SI) k values, consistently with their low (<20%) serpentinization. Remanence contribution is negligible, as (a) Q < 1 values imply remanent magnetization subordinate to induced magnetization, (b) paleomagnetic directions from most magnetic sites are scattered, and (c) remanence is unstable at lower crust temperatures. We conclude that IVZ lower crust rocks could not yield magnetic anomalies generated by Precambrian lower crust from continent interiors, and similar conclusions might stand for other Variscan-age lower crust sections. Scattered high-intensity metabasites could be candidates, if their PSD magnetite-rich mineralogy dominated Precambrian lower crust.

Abstract Image

意大利西北部Ivrea-Verbano下地壳的磁性和古地磁特征:评估瓦里斯坎时代下地壳的磁化强度
来自大陆内部(主要是前寒武纪)下地壳的高强度磁异常的来源长期以来一直存在争议,因为它需要具有2-6 A/m磁化强度的投机岩石。本文报道了西阿尔卑斯山Ivrea-Verbano带(IVZ)的地磁和古地磁调查,该区出露晚瓦里斯坎—二叠纪变质和侵入下地壳岩石。我们沿着Cannobina, Ossola, Strona和Sesia山谷/部分采样了39个定向站点。在Ossola和Strona山谷的变质岩中测得低磁化率(k)(0.27 ~ 2.1·10−3 SI)。在25个含有伪单畴(PSD)磁铁矿的变质点中,只有2个变质岩(1个角闪岩和1个麻粒岩)的产率0.48-1.1·10−1 SI k值保持恒定,直到550°C加热。来自赛西亚山谷的辉长岩-花岗闪长岩的K值与来自变质岩的低值相似,而在Cannobina山谷,一个辉长岩和一个基性麻粒岩的K值与来自Ossola/Strona山谷的两个强磁点相当。Balmuccia和Finero的橄榄岩透镜同样产生了低(0.24-5.5·10−3 SI)的k值,与它们低(<20%)的蛇纹岩化一致。剩余物的贡献可以忽略不计,如(a) Q <;1的值意味着剩余磁化服从于感应磁化,(b)大多数磁位的古磁方向是分散的,(c)在地壳温度较低时剩磁不稳定。我们的结论是,IVZ下地壳岩石不可能产生前寒武纪下地壳从大陆内部产生的磁异常,类似的结论可能适用于其他瓦里斯坎时代下地壳剖面。如果其富含PSD磁铁矿的矿物学在前寒武纪下地壳中占主导地位,则分散的高强度变质岩可能是候选物。
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来源期刊
Journal of Geophysical Research: Solid Earth
Journal of Geophysical Research: Solid Earth Earth and Planetary Sciences-Geophysics
CiteScore
7.50
自引率
15.40%
发文量
559
期刊介绍: The Journal of Geophysical Research: Solid Earth serves as the premier publication for the breadth of solid Earth geophysics including (in alphabetical order): electromagnetic methods; exploration geophysics; geodesy and gravity; geodynamics, rheology, and plate kinematics; geomagnetism and paleomagnetism; hydrogeophysics; Instruments, techniques, and models; solid Earth interactions with the cryosphere, atmosphere, oceans, and climate; marine geology and geophysics; natural and anthropogenic hazards; near surface geophysics; petrology, geochemistry, and mineralogy; planet Earth physics and chemistry; rock mechanics and deformation; seismology; tectonophysics; and volcanology. JGR: Solid Earth has long distinguished itself as the venue for publication of Research Articles backed solidly by data and as well as presenting theoretical and numerical developments with broad applications. Research Articles published in JGR: Solid Earth have had long-term impacts in their fields. JGR: Solid Earth provides a venue for special issues and special themes based on conferences, workshops, and community initiatives. JGR: Solid Earth also publishes Commentaries on research and emerging trends in the field; these are commissioned by the editors, and suggestion are welcome.
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