气候变化领域集成服务门户(CCPortal): The São Francisco cratonic root beneath the Neoproterozoic Brasilia belt (Brazil): Petrophysical data from kimberlite xenoliths

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DOI	10.1016/j.tecto.2021.229011
	The São Francisco cratonic root beneath the Neoproterozoic Brasilia belt (Brazil): Petrophysical data from kimberlite xenoliths
	Fernandes P.R.; Tommasi A.; Vauchez A.; Neves S.P.; Nannini F.
发表日期	2021
ISSN	00401951
卷号	816
英文摘要	Petrostructural analysis of 31 mantle xenoliths from three kimberlitic pipes intruding the Neoproterozoic Brasilia belt close to the southwestern margin of the São Francisco craton (SFC) reveals microstructures and compositions similar to those observed in cratonic roots worldwide. (1) The spinel-peridotites sampling the upper section of the lithospheric mantle have dominantly refractory modal and mineral compositions, whereas garnet-peridotites sampling the deep lithospheric mantle have more fertile compositions, consistent with those observed in cratonic roots worldwide. (2) The spinel-peridotites present a variation in microstructure from coarse-granular to coarse-porphyroclastic, but similar olivine crystallographic preferred orientations (CPO). (3) The garnet-peridotites have fine-porphyroclastic microstructures. (4) Many coarse-porphyroclastic spinel-peridotites display Fe-enrichment in olivine and pyroxenes, often associated with Ti-enrichment in pyroxenes or spinel and occurrence of modal phlogopite. (5) Equilibrium temperatures and pressures of garnet-peridotites are consistent with a cratonic geotherm, but equilibrium conditions of spinel-peridotites require a warmer geotherm. We interpret these observations as indicating that the xenoliths sample the SFC mantle root, which extends beneath the Brasilia belt, but was modified by reactive transport of the magmas forming the Alto Parnaiba Igneous Province (APIP) between 120 and 90 Ma. The APIP magmatism resulted in heterogeneous modal metasomatism, Fe enrichment, development of coarse-porphyroclastic microstructures in spinel peridotites and fine-porphyroclastic microstructures in garnet-peridotites, and moderate heating of the cratonic mantle root. These changes may produce a decrease in seismic velocities explaining the local weak negative anomaly observed in the lithospheric mantle beneath the APIP, which contrasts with the positive velocity anomalies characterizing the SFC mantle root in P-wave tomography models. However, reactive magma transport did not erase the olivine CPO. Comparison of the average seismic properties of the xenoliths with seismological data implies dominantly subhorizontal fossil flow directions and a non-negligible contribution of the cratonic root to teleseismic S-waves splitting. © 2021 Elsevier B.V.
关键词	Annealing Craton Deformation Mantle Melt-rock reaction Metasomatism Olivine Seismic anisotropy Seismic velocities
英文关键词	Belts; Garnets; Mica; Olivine; Seismic waves; Seismology; Shear waves; Volcanic rocks; Crystallographic preferred orientations; Equilibrium conditions; Equilibrium temperatures; Lithospheric mantle; Mineral composition; Petrophysical datum; Petrostructural analysis; Seismological data; Microstructure
语种	英语
来源期刊	Tectonophysics
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/207972
作者单位	Serviço Geológico do Brasil (CPRM), Brazil; Géosciences Montpellier, CNRS & Université de Montpellier, France; Instituto de Geociências, Universidade Federal de Pernambuco (UFPE), Brazil; Universidade Federal de Uberlândia (UFU), Brazil
推荐引用方式 GB/T 7714	Fernandes P.R.,Tommasi A.,Vauchez A.,et al. The São Francisco cratonic root beneath the Neoproterozoic Brasilia belt (Brazil): Petrophysical data from kimberlite xenoliths[J],2021,816.
APA	Fernandes P.R.,Tommasi A.,Vauchez A.,Neves S.P.,&Nannini F..(2021).The São Francisco cratonic root beneath the Neoproterozoic Brasilia belt (Brazil): Petrophysical data from kimberlite xenoliths.Tectonophysics,816.
MLA	Fernandes P.R.,et al."The São Francisco cratonic root beneath the Neoproterozoic Brasilia belt (Brazil): Petrophysical data from kimberlite xenoliths".Tectonophysics 816(2021).