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| Open AccessMantle exhumation at magma-poor rifted margins controlled by frictional shear zones
The development of offset normal faults in the conjugate Flemish Cap and Galicia magma-poor rifted margins is explored. The authors propose alternating opposite dipping detachments to be the underlying cause.
- Thomas Theunissen
- & Ritske S. Huismans
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Article
| Open AccessGrowth of Neogene Andes linked to changes in plate convergence using high-resolution kinematic models
A high-resolution model of the motion between Nazca and South American plates is presented. The work shows rapid changes that help explaining tectono-magmatic events via a balance between kinematic energy and gravitational potential energy stored in the roots of the Andes.
- Felipe Quiero
- , Andrés Tassara
- & Osvaldo Rabbia
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| Open AccessConstraining composition and temperature variations in the mantle transition zone
A new study by @JinZhang_MP models the global distribution of wadsleyite proportion, temperature and water content in the upper mantle transition zone.
- Wen-Yi Zhou
- , Ming Hao
- & Brandon Schmandt
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| Open AccessSlab control on the mega-sized North Pacific ultra-low velocity zone
Ultra-low velocity zones (ULVZs) are localized small-scale patches with extreme physical properties at the core-mantle boundary. Here, the authors discover a mega-sized ULVZ (1,500 × 900 km) at the northern edge of the Pacific Large Low Velocity Province.
- Jiewen Li
- , Daoyuan Sun
- & Dan J. Bower
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Article
| Open AccessCatastrophic slab loss in southwestern Pangea preserved in the mantle and igneous record
The origin of the Permian-Triassic Choiyoi silicic large igneous province (SLIP) is assessed by linking the igneous record, plate-kinematic reconstructions, and the deep mantle. This study suggests an origin related to a massive slab loss in Pangea.
- Guido M. Gianni
- & César R. Navarrete
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| Open AccessEpisodic back-arc spreading centre jumps controlled by transform fault to overriding plate strength ratio
Back-arc spreading centre jumps have been suggested to be controlled by a number of different drivers. Here, the authors, using 3D numerical models, show that transform faults can trigger back-arc spreading centre jumps, without the need of any ad hoc factors.
- Nicholas Schliffke
- , Jeroen van Hunen
- & Frédéric Gueydan
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| Open AccessSouthward expanding plate coupling due to variation in sediment subduction as a cause of Andean growth
Climate and tectonics control the distribution of trench sediments which in turn exerts a strong influence on tectonics by controlling the coupling strength of plate interface. This process could have caused the southward growth of the Andes.
- Jiashun Hu
- , Lijun Liu
- & Michael Gurnis
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| Open AccessThermochemical anomalies in the upper mantle control Gakkel Ridge accretion
The ultimate driver of ultraslow spreading ridges is unknown. Here the authors use spreading rates derived directly from isotopic ages of seafloor samples to link magmatic and amagmatic segments with thermochemical variations in the upper mantle.
- John M. O’Connor
- , Wilfried Jokat
- & Anthony A. P. Koppers
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Article
| Open AccessLong-lived Paleoproterozoic eclogitic lower crust
The nature of the lower crust and the crust-mantle transition is fundamental to Earth Sciences. Here, the authors provide evidence for long-lasting presence of lower crustal eclogite below the seismic Moho, challenging conventional models.
- Sebastian Buntin
- , Irina M. Artemieva
- & Stefan Buske
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| Open AccessAlpine-style nappes thrust over ancient North China continental margin demonstrate large Archean horizontal plate motions
How far back in time plate tectonics operated on Earth is debated because of a paucity of geological evidence for horizontal plate motions. Here the authors show that plates moved laterally by >3500 kilometres 2.7–2.5 billion years ago, demonstrating plate tectonics in the Archean Eon, when life developed on Earth.
- Yating Zhong
- , Timothy Kusky
- & Hao Deng
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Article
| Open AccessSeismological expression of the iron spin crossover in ferropericlase in the Earth’s lower mantle
This study identifies the predicted seismic expression of the high-to-low iron spin crossover in the deep Earth mineral ferropericlase. A depth-dependent signal is detected in the fastest and slowest regions, related to lateral temperature variations, of several global seismic tomography models.
- Grace E. Shephard
- , Christine Houser
- & Renata M. Wentzcovitch
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| Open AccessEpisodic construction of the early Andean Cordillera unravelled by zircon petrochronology
Episodic magmatism of the early Andes is the result of a complex interplay between mantle, crust, slab and sediment contributions that can be traced using zircon chemistry. An external (tectonic) model is argued for the episodic plutonism in this extensional continental arc.
- José Joaquín Jara
- , Fernando Barra
- & Diego Morata
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| Open AccessA subduction influence on ocean ridge basalts outside the Pacific subduction shield
We discover a pervasive subduction influence in the Arctic, Atlantic and Indian mantle, which is nearly absent in the Pacific mantle. Such a hemispheric-scale upper mantle heterogeneity reflects the control of a “subduction shield” that has surrounded the Pacific Ocean for 180 Myr.
- A. Y. Yang
- , C. H. Langmuir
- & Z. Chen
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| Open AccessRheological inheritance controls the formation of segmented rifted margins in cratonic lithosphere
The evolution of rifts and rifted margins is controlled by the rheology of the lithosphere. Thus, pre-existing lateral rheological variations can dominate the rifting process and lead to margin segmentation, with along-strike changes in crustal structure and nature and timing of continental breakup.
- M. Gouiza
- & J. Naliboff
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| Open AccessBadland landscape response to individual geomorphic events
The relative role of individual forcing events in long-term landscape evolution is challenging to measure in the field. Badlands offer special opportunities to quantify common, natural landscape dynamics on observational time scales.
- Ci-Jian Yang
- , Jens M. Turowski
- & Kuo-Jen Chang
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| Open AccessDifferentiating induced versus spontaneous subduction initiation using thermomechanical models and metamorphic soles
The mechanism of subduction initiation is a key to modern plate tectonics. Here, using numerical modeling and geological observations, the authors find that the majority of active and paleo subduction zones with metamorphic soles likely formed during induced subduction initiation that involved a young overriding plate.
- Xin Zhou
- & Ikuko Wada
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Article
| Open AccessMassive carbon storage in convergent margins initiated by subduction of limestone
Experiments and buoyancy calculations reveal that subduction of limestone results in massive carbon storage in arc lithosphere, forming an important carbon reservoir in convergent margins. Remobilization of this carbon reservoir during arc magma ascent may dominate carbon emissions at volcanic arcs.
- Chunfei Chen
- , Michael W. Förster
- & Yongsheng Liu
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| Open AccessSubduction history of the Caribbean from upper-mantle seismic imaging and plate reconstruction
Seismic imaging of subducted plates offers a way to improve plate tectonic reconstructions. Here, Braszus et al. use new ocean-bottom seismometer data from the Lesser Antilles to locate subducted spreading centres and faults thus providing a new understanding of the evolution of the Caribbean plate.
- Benedikt Braszus
- , Saskia Goes
- & Marjorie Wilson
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| Open AccessLinking deeply-sourced volatile emissions to plateau growth dynamics in southeastern Tibetan Plateau
Deeply-sourced volatiles are releasing from orogenic plateau regions, providing windows to plateau growth dynamics occurring at variable depths. Here the authors show that mantle-derived volatiles reveal the involvement of mantle dynamics in southeastward growth of the Tibetan Plateau.
- Maoliang Zhang
- , Zhengfu Guo
- & Ying Li
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| Open AccessThermal state and evolving geodynamic regimes of the Meso- to Neoarchean North China Craton
Constraining the thermal state of the lithosphere is crucial to understanding geodynamic regime in early Earth. Here the authors reconstruct ~2.9–2.5 Ga thermal structure of continental lithosphere of the North China Craton using TTG and propose a systematic Archean geodynamic evolution process.
- Guozheng Sun
- , Shuwen Liu
- & Fangyang Hu
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| Open AccessMelt volume at Atlantic volcanic rifted margins controlled by depth-dependent extension and mantle temperature
Magmatic productivity at passive margins is controlled by mantle temperature and rifting style. The authors reveal that melt volume at rifted margins is linearly correlated with margin width and that volcanic margins may result from depth dependent extension without high temperature mantle plumes.
- Gang Lu
- & Ritske S. Huismans
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| Open AccessA Late Cretaceous true polar wander oscillation
The authors present a high-resolution palaeomagnetic record for a Late Cretaceous limestone in Italy. They claim that their record robustly shows a ~12° true polar wander oscillation between 86 and 78 Ma, with the greatest excursion at 84–82 Ma.
- Ross N. Mitchell
- , Christopher J. Thissen
- & Joseph L. Kirschvink
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| Open AccessSegregated oceanic crust trapped at the bottom mantle transition zone revealed from ambient noise interferometry
By combining ambient noise interferometry with mineral physics modeling, this work sheds new light on mantle transition zone physics. Their findings provide new evidence of segregated oceanic crust subducted and trapped within the mantle transition zone, implying complex mantle circulation modes.
- Jikun Feng
- , Huajian Yao
- & Zhu Mao
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| Open Access13 million years of seafloor spreading throughout the Red Sea Basin
Here, based on earthquake data, vertical gravity gradient data and high-resolution bathymetry, the authors show that the Red Sea is not in transition from rifting to spreading as previously proposed. They instead suggest it to be a mature ocean basin in which continuous seafloor spreading began quasi-instantaneously along its entire length around 13 Ma ago.
- Nico Augustin
- , Froukje M. van der Zwan
- & Bryndís Brandsdóttir
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| Open AccessGlobal influence of mantle temperature and plate thickness on intraplate volcanism
Here, the authors compile a global geochemical database of Neogene-Quaternary intraplate volcanism. By comparing the distribution and composition of these rocks with tomographic models they show that intraplate volcanism can be used to constrain upper-mantle structure at the time of eruption.
- P. W. Ball
- , N. J. White
- & S. N. Stephenson
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Article
| Open AccessFormation of large low shear velocity provinces through the decomposition of oxidized mantle
Dense Fe3+-rich bridgmanite can explain the seismic features of Large Low Shear Velocity Provinces, as it can form large-scale thermochemical piles in the deep mantle that remain stable throughout Earth’s history.
- Wenzhong Wang
- , Jiachao Liu
- & Zhongqing Wu
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| Open AccessThe Hindu Kush slab break-off as revealed by deep structure and crustal deformation
Here, the authors document active slab break-off and the crustal response during continental collision under the Hindu Kush, a rarely observed process since it happens over geologically short time spans.
- Sofia-Katerina Kufner
- , Najibullah Kakar
- & Bernd Schurr
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| Open AccessCaribbean plate tilted and actively dragged eastwards by low-viscosity asthenospheric flow
Here, the authors follow a new approach using analytic solutions for Poiseuille-Couette channel flow to compute asthenospheric viscosities under the Caribbean. Active asthenospheric flow observed under the Caribbean contradicts the traditional view that the asthenosphere is only a passive lubricating layer for Earth’s tectonic plates.
- Yi-Wei Chen
- , Lorenzo Colli
- & Hejun Zhu
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| Open AccessExtrusion of subducted crust explains the emplacement of far-travelled ophiolites
The interplay between continental subduction exhumation dynamics and the obduction of ophiolite sheets remains enigmatic. Here, the authors show that the extrusion of the subducted continental upper crust triggers the necking and breaking of the oceanic upper plate and leads to far-travelled ophiolite sheet emplacement.
- Kristóf Porkoláb
- , Thibault Duretz
- & Ernst Willingshofer
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| Open AccessA new global ice sheet reconstruction for the past 80 000 years
The configuration of past ice sheets, and therefore sea level, is highly uncertain. Here, the authors provide a global reconstruction of ice sheets for the past 80,000 years that allows to test proxy based sea level reconstructions and helps to reconcile disagreements with sea level changes inferred from models.
- Evan J. Gowan
- , Xu Zhang
- & Gerrit Lohmann
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Article
| Open AccessNo mafic layer in 80 km thick Tibetan crust
Crustal doubling in Tibet and the Himalayas by underthrusting of the Indian plate is thought to require the presence of a mafic layer above the Moho. Here, the authors present seismic data which shows that the middle Lhasa Terrane has very low velocity (Vp < 6.7 km/s) throughout the 80 km thick crust, which they suggest is predominantly felsic in composition.
- Gaochun Wang
- , Hans Thybo
- & Irina M. Artemieva
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Article
| Open AccessConstraining tectonic uplift and advection from the main drainage divide of a mountain belt
One of the most conspicuous features of a mountain belt is the main drainage divide. Here, the authors constrain the tectonic uplift and advection of a mountain belt from the location and migration direction of its main drainage divide.
- Chuanqi He
- , Ci-Jian Yang
- & Xiao-Ping Yuan
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Article
| Open AccessCentennial response of Greenland’s three largest outlet glaciers
The Greenland Ice Sheet is the largest land ice contributor to sea level rise and understanding the long-term glacier response to external forcing is key to improved projections. Here the authors show Greenland’s three largest outlet glaciers will likely exceed current worst-case scenario
- Shfaqat A. Khan
- , Anders A. Bjørk
- & Toni Schenk
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Article
| Open AccessAftershocks are fluid-driven and decay rates controlled by permeability dynamics
In this study, the authors propose that a fluid rich environment is necessary to generate long-lasting aftershock sequences. Based on this premise, the study presents a theory for modeling fluid-driven earthquake sequences
- Stephen A. Miller
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| Open AccessStagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers
Knowledge of shear-wave anisotropy is important to understanding the structure and dynamics of the subduction zone mantle wedge. Here, the authors find unambiguous evidence that forearc anisotropy resides in the upper-plate crust, while weak anisotropy in the most seaward part of the mantle wedge indicates decoupling from the slab
- Naoki Uchida
- , Junichi Nakajima
- & Youichi Asano
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| Open AccessFault valving and pore pressure evolution in simulations of earthquake sequences and aseismic slip
Coupling between fault zone fluid flow, permeability evolution, and elastic stress transfer produces fault valving and fluid-driven aseismic slip and pore pressure pulses. This model might explain late interseismic fault unlocking, slow slip, and rapid pressure transmission in induced seismicity.
- Weiqiang Zhu
- , Kali L. Allison
- & Yuyun Yang
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| Open AccessMantle flow distribution beneath the California margin
Although the surface deformation of tectonic plate boundaries is well determined by geological and geodetic measurements, the pattern of flow below the lithosphere remains poorly constrained. Here, the author finds that major earthquakes in California have occurred above the regions of current plastic strain accumulation in the mantle.
- Sylvain Barbot
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| Open AccessSubduction hides high-pressure sources of energy that may feed the deep subsurface biosphere
Geological sources of H2 and abiotic CH4 have had a critical role in the evolution of life and sustainability of the deep subsurface biosphere, yet the origins of these sources remain largely unconstrained. Here the authors show that deep serpentinization (40–80 km) during subduction generates significant amounts of H2 and abiotic CH4, potentially providing energy to the overlying subsurface biosphere.
- A. Vitale Brovarone
- , D. A. Sverjensky
- & I. Daniel
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Perspective
| Open AccessA transdisciplinary and community-driven database to unravel subduction zone initiation
Despite numerous advances in our understanding of subduction since the theory of plate tectonics was established, the mechanisms of subduction zone initiation remain highly controversial. Here, the authors present a transdisciplinary and expandable community database of subduction zone initiation events in the last 100 Ma, which establishes a clear direction for future research.
- Fabio Crameri
- , Valentina Magni
- & Marcel Thielmann
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Article
| Open AccessMolecular hydrogen in minerals as a clue to interpret ∂D variations in the mantle
Trace amounts of water dissolved in minerals play an important role in global tectonics through changing the density, viscosity and melting behaviour of the Earth’s mantle. Here, the authors identify the presence of molecular hydrogen in nominally anhydrous ecolgite minerals from the Kaapvaal and Siberian cratons, indicating that the storage capacity of H in the mantle may have been underestimated.
- B. N. Moine
- , N. Bolfan-Casanova
- & J. Y. Cottin
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Article
| Open AccessBreaking Earth’s shell into a global plate network
How Earth’s lithosphere first divided into tectonic plates remains uncertain. Here, the authors use 3D spherical shell models to demonstrate that anticipated warming of the early lithosphere should lead to thermal expansion and the initiation of a global network of rifts, dividing the lithosphere into tectonic plates.
- C. A. Tang
- , A. A. G. Webb
- & T. T. Chen
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Article
| Open AccessLow thermal conductivity of iron-silicon alloys at Earth’s core conditions with implications for the geodynamo
Thermal conductivity of Earth’s core affects Earth’s thermal structure, evolution and dynamics. Based on thermal conductivity measurements of iron–silicon alloys at high pressure and temperature conditions, the authors here propose Earth’s inner core could be older than previously expected.
- Wen-Pin Hsieh
- , Alexander F. Goncharov
- & Jung-Fu Lin
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Article
| Open AccessIn situ evidence of thermally induced rock breakdown widespread on Bennu’s surface
In their study, the authors discuss the potential of thermal weathering on airless bodies. As a case study, they use boulder and fracture morphologies on asteroid Bennu.
- J. L. Molaro
- , K. J. Walsh
- & D. S. Lauretta
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Article
| Open AccessVictoria continental microplate dynamics controlled by the lithospheric strength distribution of the East African Rift
One of the largest continental microplates on Earth is situated in the center of the East African Rift System, and oddly, the Victoria microplate rotates counterclockwise with respect to the neighboring African tectonic plate. Here, the authors' modelling results suggest that Victoria microplate rotation is caused by edge-driven lithospheric processes related to the specific geometry of rheologically weak and strong regions.
- Anne Glerum
- , Sascha Brune
- & Manfred R. Strecker
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Article
| Open AccessUnexpected large eruptions from buoyant magma bodies within viscoelastic crust
Large-volume volcanic eruptions can occur despite only limited precursory activity. Here the authors show that modelling the combined effects of buoyant magma, viscoelastic earth behaviour, and sustained magma channels can explain such behaviour of volcanoes and gives an estimate of pressure evolution in magma bodies.
- Freysteinn Sigmundsson
- , Virginie Pinel
- & Tadashi Yamasaki
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Article
| Open AccessIntradecadal variations in length of day and their correspondence with geomagnetic jerks
Earth rotation variation reflects the physics, dynamics and the magnetic field changes of Earth’s interior. The authors find a significant ~8.6 year periodic increasing oscillation in length of day and its good link to geomagnetic jerks related to Earth’s core oscillations, which may be used to predict the future jerk timings.
- Pengshuo Duan
- & Chengli Huang
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Article
| Open AccessEvidence for a serpentinized plate interface favouring continental subduction
The dynamics of continental subduction is largely controlled by the rheological properties of rocks involved along the subduction channel. Here, the authors reveal a prominent, yet previously undetected, low-velocity body beneath the Western Alps, along the plate interface between the European slab and the overlying Adriatic mantle, which they interpret as a serpentinite layer.
- Liang Zhao
- , Marco G. Malusà
- & Stefano Solarino
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| Open AccessOceanic crust recycling controlled by weakening at slab edges
Retreating subduction zones are enabled by the development of faults at the edges of the slab, but the physical mechanisms controlling fault propagation remain debated. Here, the authors find that oceanic crust recycling is controlled by weakening of fractures forming at the edges of slabs.
- Jessica Munch
- , Taras Gerya
- & Kosuke Ueda
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| Open AccessMultiscale variations of the crustal stress field throughout North America
The authors here present a stress map of the North American crust that gives a new view of dynamics of the continent. The results can be applied to probabilistic seismic hazard analysis and resource development as well as to provide constraints for theoretical models of crustal dynamics.
- Jens-Erik Lundstern
- & Mark D. Zoback