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| Open AccessUncovering the eruptive patterns of the 2019 double paroxysm eruption crisis of Stromboli volcano
Integrated field and laboratory investigations, and numerical simulations of the 2019 paroxysmal explosions at Stromboli volcano revealed that they were anticipated by a week-to-month-long destabilization in the normal volcanic activity, a pattern common to all paroxysms.
- Daniele Andronico
- , Elisabetta Del Bello
- & Federico Valentini
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Article
| Open AccessMariana-type ophiolites constrain the establishment of modern plate tectonic regime during Gondwana assembly
This paper placed the identified Mariana type ophiolite within a global tectonic re-organization at ca. 530-520 Ma. Similar ophiolites, together with other geological and chemical proxies, newly constrained the timing of establishment of modern plate tectonics, along with its links to surficial changes that characterize the contemporary Earth.
- Jinlong Yao
- , Peter A. Cawood
- & Peng Wang
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Article
| Open AccessOrbital forcing of ice sheets during snowball Earth
Reconciling the Snowball Earth hypothesis with sedimentological cyclicity has been a persistent challenge. A new cyclostratigraphic climate record for a Cryogenian banded iron formation in Australia provides evidence for orbital forcing of ice sheet advance and retreat cycles during Snowball Earth.
- Ross N. Mitchell
- , Thomas M. Gernon
- & Xiaofang He
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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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Article
| Open AccessFingerprinting the Cretaceous-Paleogene boundary impact with Zn isotopes
Elevated Zn isotope compositions occur in K-Pg sedimentary layers of three different depositional environments across North America and the Caribbean. The data indicate a volatilization event, and act as a robust mechanistic indicator of the meteorite impact at the end of the Cretaceous.
- Ryan Mathur
- , Brandon Mahan
- & Francisca E. Oboh-Ikuenobe
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Article
| Open AccessShallow slow earthquakes to decipher future catastrophic earthquakes in the Guerrero seismic gap
New offshore observations in the Guerrero seismic gap discovered shallow slow earthquakes, which suggest that a portion of the plate interface undergoes stable slip. This may explain the long return period of large earthquakes and why have previous large earthquakes not propagated into the gap.
- R. Plata-Martinez
- , S. Ide
- & Y. Ito
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Article
| Open AccessHydraulic transmissivity inferred from ice-sheet relaxation following Greenland supraglacial lake drainages
Hydraulic transmissivity under the 1km-thick Greenland Ice Sheet was inferred by ice-sheet uplift relaxation after rapid lake drainage events. A two-order-of-magnitude increase in hydraulic transmissivity was found throughout the melt season.
- Ching-Yao Lai
- , Laura A. Stevens
- & Howard A. Stone
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| Open AccessSunda arc mantle source δ18O value revealed by intracrystal isotope analysis
Subduction zone volcanoes are underlain by extensive magma plumbing systems, which can obscure original mantle source signals. Here, the authors show that intra-crystal oxygen isotope analysis of clinopyroxenes from the Sunda arc (Indonesia) reveal the δ18 O value of the sub-arc mantle.
- Frances M. Deegan
- , Martin J. Whitehouse
- & Osvaldo González-Maurel
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Article
| Open AccessOcean-bottom and surface seismometers reveal continuous glacial tremor and slip
Anomalously slow earthquakes play a critical role in the earthquake cycle and fault sliding. Here, the authors detect continuous seismic radiation from a glacier sliding over its bed and show persistent coastal shaking to represent an addition to the family of slow earthquakes.
- Evgeny A. Podolskiy
- , Yoshio Murai
- & Shin Sugiyama
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Article
| 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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Article
| Open AccessIndia-Asia collision as a driver of atmospheric CO2 in the Cenozoic
“Earth degassing is a critical carbon source, but its contribution to Cenozoic atmospheric CO2 variations is not well known. Here, the authors analyse CO2 fluxes on the Tibetan Plateau and suggest that the India-Asia collision was the primary driver of changes in atmospheric CO2 over the past 65 Ma.”
- Zhengfu Guo
- , Marjorie Wilson
- & Jiaqi Liu
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Article
| Open AccessQuantitative comparison of geological data and model simulations constrains early Cambrian geography and climate
There is a lot of uncertainty about what Earth’s climate and geography were like in the early Cambrian, when animal life diversified throughout the oceans. Here we show that numeric comparisons of model simulations and climatically influenced rocks can help constrain geography and climate during this time.
- Thomas W. Wong Hearing
- , Alexandre Pohl
- & Thijs R. A. Vandenbroucke
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Article
| Open AccessThe perpetual fragility of creeping hillslopes
The downhill motion of soils on hillslopes is not well understood. Here, the authors present laboratory experiments and show that hillslopes are made perpetually fragile by environmental perturbations that prevent them from stabilizing.
- Nakul S. Deshpande
- , David J. Furbish
- & Douglas J. Jerolmack
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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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Article
| 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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Article
| Open AccessCrustal rejuvenation stabilised Earth’s first cratons
Why Earth’s crust only started becoming widely preserved in the Eoarchaean, 500 Ma after planetary accretion, is poorly understood. Here, the authors document a shift to juvenile magmatic sources in the early Eoarchaean, linking crustal preservation to the formation of stabilising melt-depleted mantle.
- Jacob A. Mulder
- , Oliver Nebel
- & Timothy J. Ivanic
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Article
| Open AccessRapid endogenic rock recycling in magmatic arcs
A case study of migmatites indicates that the juvenile arc crust underwent a rapid self-recycling process from arc magmatism to erosion and weathering at the surface, then to burial and remelting. Intra-arc thrust fault systems might efficiently promote endogenous recycling.
- Jun-Yong Li
- , Ming Tang
- & Lin-Sen Li
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| Open AccessDislocation interactions in olivine control postseismic creep of the upper mantle
Models of the viscosity evolution of mantle rocks are central to analyses of postseismic deformation but constraints on underlying physical processes are lacking. Here, the authors present measurements of microscale stress heterogeneity in olivine suggesting that long-range dislocation interactions contribute to viscosity evolution.
- David Wallis
- , Lars N. Hansen
- & Ricardo A. Lebensohn
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| Open AccessNon-lithifying microbial ecosystem dissolves peritidal lime sand
Present et al. examine the processes controlling lithification of microbial mats in a Caribbean peritidal carbonate environment. The authors present sedimentological and geochemical evidence of a surprising bias against preserving the most robust, widespread microbial ecosystems in the sedimentary record.
- Theodore M. Present
- , Maya L. Gomes
- & John P. Grotzinger
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| Open AccessSubmarine landslide megablocks show half of Anak Krakatau island failed on December 22nd, 2018
The authors here present a detailed reconstruction of the landslide mass following the 2018 eruption of Anak Krakatau. Bathymetry data reports the volume of the collapsed submarine flank to be much larger than previously reported.
- J. E. Hunt
- , D. R. Tappin
- & U. Udrekh
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| Open AccessOn the use of plume models to estimate the flux in volcanic gas plumes
Monitoring the flux of gas from volcanoes is a fundamental component of volcano monitoring programs and is used as a basis for eruption forecasting. Here, the authors present a new method using video images of volcanic gas plumes to measure the speed of convective structures and to estimate volcanic fluxes.
- Julia Woitischek
- , Nicola Mingotti
- & Andrew W. Woods
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Article
| Open AccessExperimental evidence for hydrogen incorporation into Earth’s core
Based on diamond-anvil cell experiments and cutting-edge secondary ion mass spectrometry analyses, the authors here show that hydrogen may be an important constituent in the Earth’s core and also in the metallic cores of any terrestrial planet or moon having a mass in excess of 10% of the Earth.
- Shoh Tagawa
- , Naoya Sakamoto
- & Hisayoshi Yurimoto
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| Open AccessHelium in diamonds unravels over a billion years of craton metasomatism
Diamonds encapsulate the deep Earth fluids that form them, providing windows to deep mantle processes. This study constrains their ages, based on uranium-thorium-to-helium radioactive decay in the fluids and helium diffusivity in diamond, and relates diamond formation to geological events in Southern Africa.
- Yaakov Weiss
- , Yael Kiro
- & Steven L. Goldstein
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Article
| Open AccessUnconventional singularities and energy balance in frictional rupture
Ordinary cracks in bulk materials feature square root singular deformation fields near their edge. Here, the authors show that rupture fronts propagating along frictional interfaces, while resembling ordinary cracks in some respects, feature edge sigularity that differs from the conventional square root one.
- Efim A. Brener
- & Eran Bouchbinder
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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 AccessCalcium isotope evidence for early Archaean carbonates and subduction of oceanic crust
Phase equilibrium modelling combined with Ca isotope measurements in ancient granitoids demonstrates that subduction of oceanic crust occurred repeatedly throughout the Archaean and that carbonate sediments were present in early Eoarchaean oceans (>3.8 billion years).
- Michael A. Antonelli
- , Jillian Kendrick
- & Frédéric Moynier
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Article
| Open AccessCosmogenic in situ 14C-10Be reveals abrupt Late Holocene soil loss in the Andean Altiplano
The assessment of soil sustainability in prehistoric times requires comparing millennium-scale erosion rates with geological background rates. Here, the authors apply in situ cosmogenic 14C, 10Be, and 26Al to reveal rapid soil erosion on the Andean Altiplano in response to Late Holocene climate change and the onset of agropastoralism.
- Kristina Hippe
- , John D. Jansen
- & David Lundbek Egholm
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| Open AccessFluid pressurisation and earthquake propagation in the Hikurangi subduction zone
Laboratory experiments reproducing earthquake slip in non cohesive fault rocks under fluid pressurised conditions are challenging. Thanks to these experiments, the authors show that earthquake slip occurring in tsunamigenic subduction zone faults is controlled by dilatancy and pressurisation processes.
- S. Aretusini
- , F. Meneghini
- & G. Di Toro
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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 AccessRapid heat discharge during deep-sea eruptions generates megaplumes and disperses tephra
A novel model for submarine tephra dispersal by hydrothermal megaplumes is proposed. The energy flux inferred from our model aligns with megaplume observations, and suggests that the catastrophic release of hot crustal fluids, as opposed to lava heating, is responsible for megaplume generation.
- Samuel S. Pegler
- & David J. Ferguson
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| Open AccessHow deep ocean-land coupling controls the generation of secondary microseism Love waves
The authors here study the origin of seismic Love waves induced by ocean waves. The study finds Love waves to originate along steep bathymetry and underlying geological interfaces, particularly sedimentary basins, yielding spatio-temporal information about ocean-land coupling in deep water.
- Florian Le Pape
- , David Craig
- & Christopher J. Bean
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Article
| Open AccessEarly forecasting of tsunami inundation from tsunami and geodetic observation data with convolutional neural networks
Rapid and accurate hazard prediction is important for prompt evacuation and casualty reduction during natural disasters. Here, the authors present an AI-enabled tsunami forecasting approach, which provided rapid and accurate early warnings.
- Fumiyasu Makinoshima
- , Yusuke Oishi
- & Fumihiko Imamura
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Article
| Open AccessOxidized sulfur-rich arc magmas formed porphyry Cu deposits by 1.88 Ga
Tectonomagmatic conditions in the Precambrian were hypothesized to be unfavorable for porphyry Cu deposit formation. Here, the authors show that metallogenic processes typify Phanerozoic porphyry Cu deposits operated by ~1.88 Ga, reflecting modification of mantle lithosphere by oxidized slab-derived fluids at that time.
- Xuyang Meng
- , Jackie M. Kleinsasser
- & Richard A. Stern
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| Open AccessShort-term interaction between silent and devastating earthquakes in Mexico
This study shows how seismic and aseismic events are related in Mexico between 2017 and 2019. Based on a series of observations and models, the study suggests that the Mw 8.2 intraslab earthquake of 8 September 2017 severely altered the mechanical properties of the plate interface, facilitating the interaction between the events and disrupting the slow slip cycles at a regional scale.
- V. M. Cruz-Atienza
- , J. Tago
- & E. Kazachkina
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| Open AccessFire-induced rock spalling as a mechanism of weathering responsible for flared slope and inselberg development
Fire is an important mechanism of physical weathering responsible for the formation of overhanging flared slopes around the margins of steep-sided inselbergs. Fire-spalling erodes landscapes laterally rather than vertically and produces significant volumes of new sediment.
- Solomon Buckman
- , Rowena H. Morris
- & Robert P. Bourman
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| Open AccessIncreased respiratory morbidity associated with exposure to a mature volcanic plume from a large Icelandic fissure eruption
Large fissure eruptions can cause air pollution events when the volcanic plume returns to the same area after the initial advisory has been lifted. Here, the authors show that these events had a significant impact on health care usage in Iceland, and the impact was exacerbated when advisories were not issued successfully.
- Hanne Krage Carlsen
- , Evgenia Ilyinskaya
- & Thorolfur Gudnason
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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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| Open AccessMulti-phase seismic source imprint of tropical cyclones
The authors locate the maximum seismic energy imprint and lateral extent of the seismic sources generated by Typhoon Ioke. Based on this data set, they present a new tool to shed light on the generation mechanism of secondary microseisms body waves.
- Lise Retailleau
- & Lucia Gualtieri
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| Open AccessNickel isotopes link Siberian Traps aerosol particles to the end-Permian mass extinction
The end-Permian mass extinction was the most severe extinction event in the past 540 million years, and the Siberian Traps large igneous province is widely hypothesized to have been the primary trigger for the environmental catastrophe. In this study, Ni isotopes provide the link between Siberian Traps magmatism and early environmental degradation, ultimately leading to the end-Permian extinction.
- Menghan Li
- , Stephen E. Grasby
- & Yanan Shen
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Article
| Open AccessA reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting
Meltwater Pulse 1A was the most rapid global sea-level rise event during the last deglaciation, but the source of the freshwater causing this rise is debated. Here, the authors use a data-driven inversion approach to show that the North American and Eurasian Ice Sheets were the dominant contributors.
- Yucheng Lin
- , Fiona D. Hibbert
- & Sarah L. Bradley
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| Open AccessFault zone heterogeneities explain depth-dependent pattern and evolution of slow earthquakes in Cascadia
Here, the authors combine the geological and seismological constraints of the Cascadia Subduction Zone and develop a 3D rate and state friction model. By considering depth-dependent variations of differential pore pressure following a simple linear profile, the model reproduces the full spectrum of the observed ETS complexity.
- Yingdi Luo
- & Zhen Liu
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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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Article
| Open AccessBasalt derived from highly refractory mantle sources during early Izu-Bonin-Mariana arc development
Magmatism associated with early growth of subduction zones is unlike that of mature island arc systems. Here, the authors find basalts with distinct mineralogical and geochemical characteristics were erupted during this early stage, and derived from extremely refractory, hot mantle sources.
- He Li
- , Richard J. Arculus
- & Weidong Sun
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Article
| Open AccessChemical feedbacks during magma degassing control chlorine partitioning and metal extraction in volcanic arcs
Chlorine behaviour during complex, polybaric arc magma degassing is poorly understood. Here, the authors show that chemical feedbacks during coeval magma differentiation and degassing account for the Cl record at both volcanoes and ore deposits, and quantify the role of Cl in efficient copper extraction during degassing.
- B. Tattitch
- , C. Chelle-Michou
- & R. R. Loucks
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| Open AccessReversal of carbonate-silicate cation exchange in cold slabs in Earth’s lower mantle
CaCO3 is more stable than MgCO3 under conditions of Earth’s lowermost mantle, with implications for deep mantle chemistry.
- Mingda Lv
- , Susannah M. Dorfman
- & Vitali B. Prakapenka
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Article
| Open AccessImagining and constraining ferrovolcanic eruptions and landscapes through large-scale experiments
Ferrovolcanism is a hypothetical form of planetary volcanism in which the erupted lava is metallic in composition. Here we show that ferrovolcanic lava is denser and less viscous than silicate lava, resulting in fast-moving, thin, braided flows.
- A. Soldati
- , J. A. Farrell
- & J. A. Karson
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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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Article
| Open AccessGround deformation reveals the scale-invariant conduit dynamics driving explosive basaltic eruptions
Here, the authors use 20 years of ground deformation data from Stromboli and correlate this data with eruptive records. They find that duration and amplitude of the inflation trend scales with eruption magnitude, indicating that explosive dynamics obeys the same (scale-invariant) conduit process.
- M. Ripepe
- , G. Lacanna
- & D. Delle Donne
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| Open AccessAnatomy of subcritical submarine flows with a lutocline and an intermediate destruction layer
This study investigates the underlying physical mechanisms of turbidity currents travelling thousands of miles in confined submarine settings, rather than diffusing after short distance. Using high resolution simulations with up to a billion grid points helps to understand the evolving layered structure of a current.
- Jorge S. Salinas
- , S. Balachandar
- & M. I. Cantero