4.7 Article

Tectonic regionalization without a priori information: A cluster analysis of upper mantle tomography

期刊

EARTH AND PLANETARY SCIENCE LETTERS
卷 308, 期 1-2, 页码 151-160

出版社

ELSEVIER
DOI: 10.1016/j.epsl.2011.05.050

关键词

global tomography; continental lithosphere; hotspots; cluster analysis; waveform modeling

资金

  1. NSF [EAR-0738284]

向作者/读者索取更多资源

Global mantle tomography can be improved through better use of data and application of more accurate wave propagation methods. However, few techniques have been developed for objective validation and exploration of the resulting tomographic models. We show that cluster analysis can be used to validate and explore the salient features across such models. We present a cluster analysis of a global upper mantle radially anisotropic model SEMum developed using full waveform tomography and the Spectral Element Method. Applied to SEMum down to 350 km depth, the cluster analysis reveals that absolute shear wave velocity (Vs) depth profiles naturally group into families that correspond with known surface tectonics. This allows us to construct a global tectonic regionalization based solely on tomography, without the help of any a priori information. We find that the profiles of stable platforms and shields consistently exhibit a mid-lithospheric low velocity zone (LVZ) between 80 and 130 km depth, while the asthenosphere is found at depths greater than 250 km in both regions. This global intra-continental-lithosphere low velocity zone agrees with recent receiver function studies and regional tomographic studies. Furthermore, we identify an anomalous oceanic region characterized by slow shear wave speeds at depths below 150 km. Hotspots are found preferentially in the vicinity of this anomalous region. In the Pacific Ocean, where plate velocities are largest, these regions have elongated shapes that align with absolute plate motion, suggesting a relationship between the location of hotspots and small-scale convection in the oceanic upper mantle. (C) 2011 Elsevier B.V. All rights reserved.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

Article Multidisciplinary Sciences

Upper mantle structure of Mars from InSight seismic data

Amir Khan, Savas Ceylan, Martin van Driel, Domenico Giardini, Philippe Lognonne, Henri Samuel, Nicholas C. Schmerr, Simon C. Staehler, Andrea C. Duran, Quancheng Huang, Doyeon Kim, Adrien Broquet, Constantinos Charalambous, John F. Clinton, Paul M. Davis, Melanie Drilleau, Foivos Karakostas, Vedran Lekic, Scott M. McLennan, Ross R. Maguire, Chloe Michaut, Mark P. Panning, William T. Pike, Baptiste Pinot, Matthieu Plasman, John-Robert Scholz, Rudolf Widmer-Schnidrig, Tilman Spohn, Suzanne E. Smrekar, William B. Banerdt

Summary: By analyzing seismic data from Mars, researchers have constrained the planet's internal structure and thermochemical state, revealing that Mars has a thicker thermal lithosphere than Earth and a much higher enrichment of heat-producing elements in the crust than previously thought.

SCIENCE (2021)

Article Multidisciplinary Sciences

Seismic detection of the martian core

Simon C. Stahler, Amir Khan, W. Bruce Banerdt, Philippe Lognonne, Domenico Giardini, Savas Ceylan, Melanie Drilleau, A. Cecilia Duran, Raphael F. Garcia, Quancheng Huang, Doyeon Kim, Vedran Lekic, Henri Samuel, Martin Schimmel, Nicholas Schmerr, David Sollberger, Eleonore Stutzmann, Zongbo Xu, Daniele Antonangeli, Constantinos Charalambous, Paul M. Davis, Jessica C. E. Irving, Taichi Kawamura, Martin Knapmeyer, Ross Maguire, Angela G. Marusiak, Mark P. Panning, Clement Perrin, Ana-Catalina Plesa, Attilio Rivoldini, Cedric Schmelzbach, Geraldine Zenhausern, Eric Beucler, John Clinton, Nikolaj Dahmen, Martin van Driel, Tamara Gudkova, Anna Horleston, W. Thomas Pike, Matthieu Plasman, Suzanne E. Smrekar

Summary: The study found that Mars has a core radius of around 1830 +/- 40 kilometers, with a density of 5.7 to 6.3 grams per cubic centimeter. The martian mantle is mineralogically similar to Earth's upper mantle and transition zone, but lacks a bridgmanite-dominated lower mantle, suggesting a different geological structure. This also affects the seismic observations of potentially active regions on Mars.

SCIENCE (2021)

Article Geochemistry & Geophysics

Global reference seismological data sets: multimode surface wave dispersion

P. Moulik, V Lekic, B. Romanowicz, Z. Ma, A. Schaeffer, T. Ho, E. Beucler, E. Debayle, A. Deuss, S. Durand, G. Ekstrom, S. Lebedev, G. Masters, K. Priestley, J. Ritsema, K. Sigloch, J. Trampert, A. M. Dziewonski

Summary: Global variations in the propagation of surface waves provide unique constraints on the source properties and structure of the Earth's mantle. This study aims to construct a reference data set of multimode dispersion measurements by reconciling large and diverse catalogues of surface wave dispersion. The study finds that the measurements of fundamental-mode dispersion are internally consistent, but the agreement deteriorates for overtones.

GEOPHYSICAL JOURNAL INTERNATIONAL (2022)

Article Multidisciplinary Sciences

On the relative temperatures of Earth's volcanic hotspots and mid-ocean ridges

Xiyuan Bao, Carolina R. Lithgow-Bertelloni, Matthew G. Jackson, Barbara Romanowicz

Summary: Research suggests that volcanic hotspots vary greatly in temperature, with some being extremely hot, some cold, and others not hot enough to actively upwell. Cold hotspots may originate from the upper mantle depth or be cooled by small-scale convection.

SCIENCE (2022)

Review Geochemistry & Geophysics

Achievements and Prospects of Global Broadband Seismographic Networks After 30 Years of Continuous Geophysical Observations

A. T. Ringler, R. E. Anthony, R. C. Aster, C. J. Ammon, S. Arrowsmith, H. Benz, C. Ebeling, A. Frassetto, W-Y Kim, P. Koelemeijer, H. C. P. Lau, J. P. Montagner, P. G. Richards, D. P. Schaff, M. Vallee, W. Yeck, V Lekic

Summary: Global seismographic networks (GSNs) have played a crucial role in advancing our understanding of Earth's structure and processes. Through international collaborations and technological advancements, GSNs have provided real-time and high-quality data for seismic studies, earthquake characterization, and environmental monitoring. The integration of GSN data with other geophysical data has further enhanced our ability to study and interpret seismic activities on a global scale.

REVIEWS OF GEOPHYSICS (2022)

Article Geochemistry & Geophysics

Dense mantle flows periodically spaced below ocean basins

Isabelle Panet, Marianne Greff-Lefftz, Barbara Romanowicz

Summary: Understanding mantle flow is crucial for understanding the connection between deep Earth dynamics and global tectonics. This study analyzes derivatives of seafloor topography and gravity potential over the Pacific and Northern Indian ocean basins, revealing periodic undulations and identifying alignments with sub-lithospheric upper mantle mass excess and slow seismic velocity fingers. This suggests an intermediate scale of mantle convection below ocean basins, driven by lateral variations in composition. Further research is needed to investigate the nature of these mass excess sources and their relationship with slow seismic velocities.

EARTH AND PLANETARY SCIENCE LETTERS (2022)

Article Multidisciplinary Sciences

Seismic detection of a deep mantle discontinuity within Mars by InSight

Quancheng Huang, Nicholas C. Schmerr, Scott D. King, Doyeon Kima, Attilio Rivoldini, Ana-Catalina Plesa, Henri Samuel, Ross R. Maguire, Foivos Karakostas, Vedran Lekic, Constantinos Charalambous, Max Collinet, Robert Myhill, Daniele Antonangeli, Melanie Drilleau, Misha Bystricky, Caroline Bollinger, Chloe Michaut, Tamara Gudkova, Jessica C. E. Irving, Anna Horleston, Benjamin Fernando, Kuangdai Leng, Tarje Nissen-Meyer, Frederic Bejina, Ebru Bozdag, Caroline Beghein, Lauren Waszek, Nicki C. Siersch, John-Robert Scholz, Paul M. Davis, Philippe Lognonne, Baptiste Pinot, Rudolf Widmer-Schnidrig, Mark P. Panning, Suzanne E. Smrekar, Tilman Spohn, William T. Pike, Domenico Giardini, W. Bruce Banerdt

Summary: Constraining the thermal and compositional state of the mantle is crucial for deciphering the formation and evolution of Mars. By analyzing seismic data collected by NASA's InSight Mission to Mars, researchers have detected a midmantle discontinuity, revealing information about the temperature and composition of Mars' mantle. This study suggests that the Martian mantle is colder and more iron-enriched compared to Earth's mantle.

PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA (2022)

Article Multidisciplinary Sciences

Surface waves and crustal structure on Mars

D. Kim, W. B. Banerdt, S. Ceylan, D. Giardini, V Lekic, P. Lognonne, C. Beghein, E. Beucler, S. Carrasco, C. Charalambous, J. Clinton, M. Drilleau, C. Duran, M. Golombek, R. Joshi, A. Khan, B. Knapmeyer-Endrun, J. Li, R. Maguire, W. T. Pike, H. Samuel, M. Schimmel, N. C. Schmerr, S. C. Stahler, E. Stutzmann, M. Wieczorek, Z. Xu, A. Batov, E. Bozdag, N. Dahmen, P. Davis, T. Gudkova, A. Horleston, Q. Huang, T. Kawamura, S. D. King, S. M. McLennan, F. Nimmo, M. Plasman, A. C. Plesa, I. E. Stepanova, E. Weidner, G. Zenhausern, I. J. Daubar, B. Fernando, R. F. Garcia, L. Posiolova, M. P. Panning

SCIENCE (2022)

Article Astronomy & Astrophysics

Crustal Structure Constraints From the Detection of the SsPp Phase on Mars

Jiaqi Li, Caroline Beghein, Paul Davis, Mark. A. Wieczorek, Scott M. M. McLennan, Doyeon Kim, Ved Lekic, Matthew Golombek, Martin Schimmel, Eleonore Stutzmann, Philippe Lognonne, William Bruce Banerdt

Summary: The shallowest layer beneath the Mars InSight Lander site has low seismic wave velocity due to high porosity and other lithological factors. The SsPp phase was detected on Mars for the first time, confirming the existence of an 8 km interface and a large wave speed contrast across it. The average P-wave speed in the top crustal layer was found to be between 2.5 and 3.2 km/s, providing a more precise estimate than previous studies.

EARTH AND SPACE SCIENCE (2023)

Article Geosciences, Multidisciplinary

Crustal Anisotropy in the Martian Lowlands From Surface Waves

C. Beghein, J. Li, E. Weidner, R. Maguire, J. Wookey, V Lekic, P. Lognonne, W. Banerdt

Summary: Scientists have observed two different types of wave signals in seismic events on Mars, which cannot be explained by a single model, indicating the presence of seismic anisotropy. They discuss various possible origins of these signals, including crystal orientation, crack alignment, impacts, and volcanic eruptions.

GEOPHYSICAL RESEARCH LETTERS (2022)

Article Geosciences, Multidisciplinary

Structure Along the Martian Dichotomy Constrained by Rayleigh and Love Waves and Their Overtones

D. Kim, S. C. Stahler, S. Ceylan, V. Lekic, R. Maguire, G. Zenhausern, J. Clinton, D. Giardini, A. Khan, M. P. Panning, P. Davis, M. Wieczorek, N. Schmerr, P. Lognonne, W. B. Banerdt

Summary: Using seismic recordings, we analyzed event S1222a to determine the shear velocity and radial anisotropic structure of the Martian crust. Our findings indicate a uniform vertically polarized shear velocity between 5 and 30 km depth, with a radial anisotropy of up to 12%. At a depth of approximately 63 +/- 10 km, a significant velocity increase suggests the presence of the crust-mantle boundary.

GEOPHYSICAL RESEARCH LETTERS (2023)

Article Multidisciplinary Sciences

Imaging deep-mantle plumbing beneath La Reunion and Comores hot spots: Vertical plume conduits and horizontal ponding zones

Mathurin Dongmo Wamba, Jean-Paul Montagner, Barbara Romanowicz

Summary: The debate about whether the two large low-shear velocity provinces (LLSVPs) at the base of Earth's mantle are wide compact structures extending thousands of kilometers upward or bundles of distinct mantle plumes is highlighted by full waveform shear wave tomography of the deep mantle beneath the Indian Ocean. It reveals the presence of several separate broad low-velocity conduits anchored at the core-mantle boundary in the eastern part of the African LLSVP, most clearly beneath La Reunion and Comores hot spots. The deep plumbing system beneath these hot spots may resemble dyke and sills in crustal volcanic systems, but at a whole-mantle scale.

SCIENCE ADVANCES (2023)

Article Geosciences, Multidisciplinary

Global Crustal Thickness Revealed by Surface Waves Orbiting Mars

D. Kim, C. Duran, D. Giardini, A. -C. Plesa, S. C. Stahler, C. Boehm, V. Lekic, S. M. McLennan, S. Ceylan, J. F. Clinton, P. Davis, A. Khan, B. Knapmeyer-Endrun, M. P. Panning, M. Wieczorek, P. Lognonne, W. B. Banerdt

Summary: We observed Rayleigh waves that orbit around Mars up to three times after the S1222a marsquake. By averaging these signals, we found the largest amplitude signals with central periods of 30 and 85 s, propagating at different group velocities of 2.9 and 3.8 km/s, respectively. The thickness of the Martian crust is 42-56 km on average, thicker than the crusts of Earth and Moon, suggesting that it plays a significant role in the thermal evolution and local melt zones within Mars.

GEOPHYSICAL RESEARCH LETTERS (2023)

Article Multidisciplinary Sciences

First observations of core-transiting seismic phases on Mars

Jessica C. E. Irving, Vedran Lekic, Cecilia Duran, Melanie Drilleau, Doyeon Kim, Attilio Rivoldini, Amir Khan, Henri Samuel, Daniele Antonangeli, William Bruce Banerdt, Caroline Beghein, Ebru Bozdag, Savas Ceylan, Constantinos Charalambous, John Clinton, Paul Davis, Raphael Garcia, Domenico Giardini, Anna Catherine Horleston, Quancheng Huang, Kenneth J. Hurst, Taichi Kawamura, Scott D. King, Martin Knapmeyer, Jiaqi Li, Philippe Lognonne, Ross Maguire, Mark P. Panning, Ana-Catalina Plesa, Martin Schimmel, Nicholas C. Schmerr, Simon C. Staehler, Eleonore Stutzmann, Zongbo Xu

Summary: We have observed seismic waves propagating through the core of Mars for the first time and used these observations to construct the first seismically constrained models for Mars' core properties. By measuring the travel times of the core-transiting seismic phase SKS and performing probabilistic inversions, we have obtained information about the bulk modulus, density, and composition of Mars' core. Our models suggest a smaller and denser core compared to previous estimates, with a P-wave velocity of 4.9 to 5.0 km/s at the core-mantle boundary.

PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA (2023)

Article Astronomy & Astrophysics

An Object-Oriented Bayesian Gravity Inversion Scheme for Inferring Density Anomalies in Planetary Interiors

Kristel Izquierdo, Vedran Lekic, Laurent G. J. Montesi

Summary: Gravity inversions have made significant contributions to our understanding of planetary body interiors and their formation processes. A novel global gravity inversion algorithm called THeBOOGIe is introduced in this study, which is capable of inferring density anomalies within the crust and mantle of planetary bodies at a global scale. By incorporating Bayesian approach and prior geological/ geophysical information, THeBOOGIe overcomes the non-uniqueness challenge in gravity inversions and accurately detects deep mantle density anomalies. Moreover, it provides complementary information to seismic models by constraining non-spherically symmetric density anomalies.

EARTH AND SPACE SCIENCE (2023)

Article Geochemistry & Geophysics

Eoarchean ultramafic rocks represent crustal cumulates: A case study of the Narssaq ultramafic body, southern West Greenland

Lingyu Zhang, Kristoffer Szilas

Summary: This study presents new petrological and geochemical data for the Narssaq Ultramafic Body (NUB) in the Itsaq Gneiss Complex of SW Greenland. The results indicate that the ultramafic rocks of NUB are not mantle residues, but instead represent crustal cumulates derived from high-Mg magmas.

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Article Geochemistry & Geophysics

Iron isotope evidence in continental intraplate basalts for mantle lithosphere imprint on heterogenous asthenospheric melts

Rong Xu, Sarah Lambart, Oliver Nebel, Ming Li, Zhongjie Bai, Junbo Zhang, Ganglan Zhang, Jianfeng Gao, Hong Zhong, Yongsheng Liu

Summary: This study investigated the iron isotope compositions of Cenozoic basalts in Southeast China, finding significant variations related to different types of basalts and their respective sources.

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Article Geochemistry & Geophysics

Shallow sources of upper mantle seismic anisotropy in East Africa

C. J. Ebinger, Miriam C. Reiss, Ian Bastow, Mary M. Karanja

Summary: The East African rift system is formed above mantle upwellings and the formation of rifts is related to lithospheric thinning and magmatic activity. The amount of splitting varies spatially and the fast axes are predominantly parallel to the orientation of the rifts. Thick lithospheric modules have less splitting and different orientations, which may indicate mantle plume flow. Splitting rotates and increases in strength as it enters the rift zones, suggesting that the anisotropy is mainly present at shallow depths.

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Correction Geochemistry & Geophysics

Serpentinite fluids and slab-melting in the Aleutian arc: Evidence from molybdenum isotopes and boron systematics (vol 603, 117970, 2023)

Ekaterina Rojas-Kolomiets, Owen Jensen, Michael Bizimis, Gene Yogodzinski, Lukas Ackerman

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Article Geochemistry & Geophysics

Concordance of V-in-olivine and Fe-XANES oxybarometry methods in mid-ocean ridge basalts

Robert W. Nicklas, Igor S. Puchtel, Ethan F. Baxter

Summary: Oxygen fugacity is a fundamental parameter for understanding redox processes in igneous systems. This study compares the Fe-XANES oxybarometry method with the V-in-olivine method for evaluating fO(2) in MORB lavas. The results show that the V-in-olivine method is not applicable to samples with low MgO content, and that the majority of Archean komatiite sources have lower fO(2) than modern MORB.

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Article Geochemistry & Geophysics

Calcium isotopes track volatile components in the mantle sources of alkaline rocks and associated carbonatites

Chunfei Chen, Stephen F. Foley, Sebastian Tappe, Huange Ren, Lanping Feng, Yongsheng Liu

Summary: The volatile components CO2 and H2O play a major role in mantle melting and heterogeneity. In this study, Ca isotopes were used to trace the lithological heterogeneity in alkaline magmatic rocks. The results revealed the presence of K-richterite and carbonate components as the source of alkaline magmas with low delta 44/40Ca values. These findings highlight the importance of Ca isotopes as a robust tracer of lithological variation caused by volatiles in the Earth's upper mantle.

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Article Geochemistry & Geophysics

Cosmogenic (un-)steadiness revealed by paired-nuclide catchment-wide denudation rates in the formerly half-glaciated Vosges Mountains (NE France)

Timothee Jautzy, Gilles Rixhon, Regis Braucher, Romain Delunel, Pierre G. Valla, Laurent Schmitt, Aster Team

Summary: Although the current approach to estimate catchment-wide denudation rates using only 10Be concentrations has made significant progress in geomorphology, this study argues for the inclusion of 26Al measurements and testing of steady-state assumptions in slow eroding, formerly glaciated landscapes. The study conducted measurements of both 10Be and 26Al in stream sediments from the Vosges Massif in France and found that elevation, slope, channel steepness, and precipitation were the primary factors controlling denudation rates. The study also revealed a significant relationship between the extent of past glaciation and the cosmogenic (un-)steadiness in the stream sediments.

EARTH AND PLANETARY SCIENCE LETTERS (2024)

Article Geochemistry & Geophysics

Linking rates of slab sinking to long-term lower mantle flow and mixing

Erik van der Wiel, Douwe J. J. van Hinsbergen, Cedric Thieulot, Wim Spakman

Summary: Numerical models of Earth's mantle dynamics can predict the vigour and mixing of mantle flow, and the average slab sinking rates are an unexplored parameter that can provide intrinsic information on these characteristics. Through numerical experiments, it has been found that slab sinking rates are strongly correlated with mantle convection and mixing, and may explain geochemical observations from hotspot volcanoes.

EARTH AND PLANETARY SCIENCE LETTERS (2024)