Electrical resistivity imaging of continental United States from three-dimensional inversion of EarthScope USArray magnetotelluric data

被引:19
|
作者
Yang, Bo [1 ,2 ]
Egbert, Gary D. [2 ]
Zhang, Huiqian [2 ,3 ]
Meqbel, Naser [4 ,5 ]
Hu, Xiangyun [1 ]
机构
[1] China Univ Geosci, Inst Geophys & Geomat, Hubei Subsurface Multiscale Imaging Key Lab, Wuhan, Peoples R China
[2] Oregon State Univ, Coll Earth Ocean & Atmospher Sci, Corvallis, OR 97331 USA
[3] Peking Univ, Sch Earth & Space Sci, Beijing, Peoples R China
[4] Natl Observ, Rio De Janeiro, Brazil
[5] 3D Consulting Geo GmbH, Berlin, Germany
基金
美国国家科学基金会; 中国国家自然科学基金;
关键词
USArray; magnetotellurics; continental US; upper mantle; water content; H2O STORAGE CAPACITY; ELECTROMAGNETIC INDUCTION; TRANSITION-ZONE; WATER-CONTENT; CONDUCTIVITY; OLIVINE; MODEL; ASTHENOSPHERE; CONSEQUENCES; GPA;
D O I
10.1016/j.epsl.2021.117244
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Long-period magnetotelluric (MT) sites, covering much of the continental United States (US) have been collected through the EarthScope USArray MT Transportable Array (TA) project. Previous regional studies using subsets of these data suggest large-scale variations in deep (sub-lithospheric) resistivity, often of significant amplitude. Here, we present a range of three-dimensional (3D) continental-scale electrical resistivity models from 3D inversion of the MT TA data, with a focus on testing robustness and resolution of this deep structure. The main features of our initial model, obtained with no constraints, are quite similar to those from previous studies, with significant (+/- 1 order of magnitude) lateral variations in deep resistivity. We show that data fit, as measured by global normalized root-mean-square misfit, is not increased by replacing structures below 200 km depth with layer averages. A more careful examination of residuals leads to further refinements, with a slight improvement in data fit. These include a moderately conductive mantle transition zone (13 Omega.m), and subtle (+/- 1/4 order of magnitude) lateral variations in resistivity below 200 km. In contrast to the initial results, these variations can be explained by reasonable variations in mantle temperature and hydration. Overall, our results suggest that the asthenospheric mantle at 200-275 km is nearly dry on average and at greater depths contains 150-300 ppm water. Lateral variations may be explained by this range of water content, or by temperature variations of 80-120 degrees C. Patterns of resistivity variations below 200 km are consistent with known continental structure, and suggest deep roots (similar to 250 km) beneath cratons, and perhaps also beneath the mid-continent rift. Reduced resistivity, likely requiring greater hydration (or higher temperatures), occurs beneath the North-central part of the continental US, the oldest part of the continent, and beneath the Yellowstone hotspot. (C) 2021 Elsevier B.V. All rights reserved.
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页数:13
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