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Preferential localized thinning of lithospheric mantle in the melt-poor Malawi Rift
The mantle lithosphere has thinned more than the crust beneath the Malawi Rift despite being melt-poor, according to seismic wave imaging; this suggests early melting of fusible mantle material.
- Emily Hopper
- , James B. Gaherty
- & Gabriel Mbogoni
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Global distribution of sediment-hosted metals controlled by craton edge stability
Major sediment-hosted base metal deposits are located within 200 km of the border between thick and thin lithosphere, according to statistical comparisons between global lithospheric thickness and known deposit locations.
- Mark J. Hoggard
- , Karol Czarnota
- & Sia Ghelichkhan
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Distinct formation history for deep-mantle domains reflected in geochemical differences
Earth’s deep-mantle domains are geochemically distinct. The African domain is enriched in subducted material, which suggests a different history from the Pacific domain and a dynamic relationship between plate tectonics and deep-mantle structures.
- Luc S. Doucet
- , Zheng-Xiang Li
- & Ross N. Mitchell
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Steady erosion rates in the Himalayas through late Cenozoic climatic changes
Long-term Himalayan erosion rates remained stable through the global climatic changes of the past six million years, according to the cosmogenic nuclide composition of terrestrial sediments recovered from the Bay of Bengal.
- Sebastien J. P. Lenard
- , Jérôme Lavé
- & Karim Keddadouche
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Rapid crystallization of precious-metal-mineralized layers in mafic magmatic systems
Mineralization of platinum-group elements in mafic intrusions occurs due to repeated self-intrusion of magma, according to strontium isotope heterogeneities preserved in the Rum layered intrusion, Scotland.
- Luke N. Hepworth
- , J. Stephen Daly
- & Brian O’Driscoll
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Palaeoproterozoic oxygenated oceans following the Lomagundi–Jatuli Event
The oceans probably remained well-oxygenated for millions of years after the Palaeoproterozoic Lomagundi–Jatuli Event, according to high concentrations and isotope signatures of redox-sensitive metals in the 2-billion-year-old Zaonega Formation, Russia.
- Kaarel Mänd
- , Stefan V. Lalonde
- & Kurt O. Konhauser
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Limited Archaean continental emergence reflected in an early Archaean 18O-enriched ocean
The water cycle was in two different steady states, before and after continental emergence, as recorded in the decreasing oxygen isotope values of seawater since the Archaean, according to an inverse geochemical model of the oceanic crustal record.
- Benjamin W. Johnson
- & Boswell A. Wing
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Editorial |
Mining’s climate accountability
Mineral extraction will play an important role in climate change mitigation and green technologies. But ensuring that the net effect of mining is beneficial requires careful monitoring of greenhouse gas emissions and environmental impacts.
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Perspective |
Transparency on greenhouse gas emissions from mining to enable climate change mitigation
Direct and indirect greenhouse gas emissions from mining for green technologies need to be accurately and transparently accounted for, as highlighted by a case study of Chilean copper mining.
- Mehdi Azadi
- , Stephen A. Northey
- & Mansour Edraki
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Earth’s earliest granitoids are crystal-rich magma reservoirs tapped by silicic eruptions
The chemical diversity of Earth’s early continental building blocks can be explained by differentiation of a single melt, without complex geodynamic settings, according to petrological and geochemical analysis of samples from South Africa.
- Oscar Laurent
- , Jana Björnsen
- & Olivier Bachmann
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News & Views |
What goes down must come up
Differential cycling of carbonate and organic carbon in the mantle may link the Great Oxidation Event and the subsequent increase in carbon isotope values, according to a model that links the Earth’s surface and interior.
- Jeremy K. Caves Rugenstein
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Great Oxidation and Lomagundi events linked by deep cycling and enhanced degassing of carbon
Carbon cycling in the mantle may be a common mechanism that links the Great Oxidation Event and the subsequent Lomagundi increase in carbon isotope values, according to a box model that accounts for carbon and oxygen fluxes and reservoirs.
- James Eguchi
- , Johnny Seales
- & Rajdeep Dasgupta
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Duplex in the Main Himalayan Thrust illuminated by aftershocks of the 2015 Mw 7.8 Gorkha earthquake
The Main Himalayan Thrust comprises two fault planes connected by imbricated faults, a structure that impedes convergence, according to an analysis of the distribution and orientation of aftershocks of the 2015 Gorkha earthquake in Nepal.
- M. M. Mendoza
- , A. Ghosh
- & A. Velasco
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Release of oxidizing fluids in subduction zones recorded by iron isotope zonation in garnet
Lawsonite dehydration and release of oxidizing fluids could play an important role in sub-arc mantle oxidation in subduction zones, suggest measurements of changing oxygen fugacity in zoned garnets from Sifnos, Greece.
- Anna R. Gerrits
- , Edward C. Inglis
- & Kevin W. Burton
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News & Views |
Chemical origin of tectonic tremor
Tectonic tremor may ultimately be caused by in situ fluid overpressure generated by chemical reactions between a subducting slab and the mantle, according to field and microstructural observations of a shear zone.
- Kohtaro Ujiie
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News & Views |
The deep roots of Earth’s surface
The structure of the lithosphere is key to reconciling the dynamic topography predicted by mantle convection models with residual topography derived from observations, suggest analyses of both models and data.
- Nicolas Flament
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The susceptibility of Oklahoma’s basement to seismic reactivation
Seismicity induced by wastewater injections is widespread in Oklahoma, probably because its basement is susceptible to the reactivation of basement-rooted faults, according to three-dimensional seismic analyses, rock-mechanics experiments and field surveys.
- F. Kolawole
- , C. S. Johnston
- & B. M. Carpenter
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Early evolution of a young back-arc basin in the Havre Trough
The Havre Tough back-arc basin, New Zealand, formed rapidly and in two phases: initial, limited seafloor spreading was followed by a transition to arc magmatism, as shown by geophysical data and modelling.
- Fabio Caratori Tontini
- , Dan Bassett
- & Richard Wysoczanski
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Earth’s multi-scale topographic response to global mantle flow
The structure of the lithosphere and its impact on mantle flow significantly influence the impact of Earth’s interior dynamics on surface topography, suggest statistical analyses of Earth’s topography.
- D. R. Davies
- , A. P. Valentine
- & C. R. Wilson
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News & Views |
A silicon memory of subduction
Subduction processes may have operated very early in Earth’s history according to the heavy silicon isotope compositions of Archaean igneous rocks. The silicon that precipitated out of the Archaean oceans as chert was subducted and melted to yield seawater-like heavy isotope signatures in early granitic rocks.
- Franck Poitrasson
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An oceanic subduction origin for Archaean granitoids revealed by silicon isotopes
Archaean granitic rocks formed by melting of silica-enriched subducted basaltic crust through interaction with seawater, according to heavy silicon isotopes measured in Archaean samples.
- Zhengbin Deng
- , Marc Chaussidon
- & Frédéric Moynier
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Early continental crust generated by reworking of basalts variably silicified by seawater
Granitic continental crust in the Archaean formed from a basaltic source that was enriched in silica due to interaction with the early oceans before melting, according to silicon isotope analyses on rocks from the Kaapvaal craton.
- Luc André
- , Kathrin Abraham
- & Stephen Foley
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Palaeoarchaean deep mantle heterogeneity recorded by enriched plume remnants
Deep mantle heterogeneity and large-scale deep mantle convection has been operating since the Palaeoarchaean, according to enriched plume signatures found in a 3.45-billion-year-old ultramafic–mafic suite from the North China Craton.
- Chao Wang
- , Shuguang Song
- & Jinlong Dong
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News & Views |
Ancient rust
Confidence that banded iron formations record oxic conditions during deposition is established, as a model demonstrates that they are formed of primary iron oxides rather than secondarily altered silicate minerals.
- Eva E. Stüeken
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Hydrogeological constraints on the formation of Palaeoproterozoic banded iron formations
Banded iron formations could not have formed by postdepositional oxidation, according to four million hydrogeological box model iterations that failed to reproduce secondary oxidation on reasonable timescales.
- Leslie J. Robbins
- , Sean P. Funk
- & Kurt O. Konhauser
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Ammonium availability in the Late Archaean nitrogen cycle
Biologically available nitrogen in the form of ammonium was abundant in the Late Archaean ocean, according to nitrogen isotope and proxy analyses on 2.7 billion year old shales from Zimbabwe.
- J. Yang
- , C. K. Junium
- & A. L. Zerkle
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An isotopically depleted lower mantle component is intrinsic to the Hawaiian mantle plume
A mantle component that is isotopically depleted is intrinsic to the Hawaiian mantle plume, and is probably sourced from the lower mantle, according to radiogenic isotope analyses on shield-stage tholeitic basalts from Mauna Kea.
- C. DeFelice
- , S. Mallick
- & S. Huang
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Climate control on banded iron formations linked to orbital eccentricity
Long-period Milankovitch eccentricity oscillations controlled compositional variations in the 2.48-billion-year-old Kuruman Banded Iron Formation, according to cyclostratigraphic analysis and high-precision dating.
- Margriet L. Lantink
- , Joshua H. F. L. Davies
- & Frederik J. Hilgen
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Methanogenesis sustained by sulfide weathering during the Great Oxidation Event
Oxidative weathering supplied a crucial flux of nutrients to the late Archaean oceans that sustained methanogenesis and kept the Archaean atmosphere in a methane sweet-spot, according to analyses of nickel isotopes from glacial deposits.
- Shui-Jiong Wang
- , Roberta L. Rudnick
- & Laura E. Wasylenki
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Fully oxygenated water columns over continental shelves before the Great Oxidation Event
Before the Great Oxidation Event there was regional-scale, full water-column oxygenation above the continental shelf, according to molybdenum and thallium isotope records that indicate massive manganese oxide burial.
- Chadlin M. Ostrander
- , Sune G. Nielsen
- & Ariel D. Anbar
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Bilobate comet morphology and internal structure controlled by shear deformation
The shape and internal structure of bilobate comet 67P is controlled by shear deformation inducing mechanically driven erosion along shear fracture networks, according to a 3D analysis of images from the Rosetta mission.
- C. Matonti
- , N. Attree
- & J.-B. Vincent
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A 60-Myr record of continental back-arc differentiation through cyclic melting
Melting of sedimentary rocks in the continental back-arc is cyclical with peaks of magmatism every 10 to 15 million years, according to zircon ages from Paleozoic western Gondwana margin samples.
- Lauren C. Wolfram
- , Roberto F. Weinberg
- & Raul Becchio
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News & Views |
Climate swings in extinction
Extreme temperature swings and deteriorating environments are perhaps what killed most life in the end-Permian extinction, suggest climate model simulations. Siberian Traps volcanism probably triggered the events.
- Ying Cui
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Systemic swings in end-Permian climate from Siberian Traps carbon and sulfur outgassing
Carbon and sulfur release from the Siberian Traps igneous province caused climate swings during the end-Permian mass extinction, according to coupled global climate simulations.
- Benjamin A. Black
- , Ryan R. Neely
- & Charles Bardeen
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Basal continental mantle lithosphere displaced by flat-slab subduction
Continental mantle lithosphere is scraped from the base of the overriding plate by the underlying oceanic slab during flat subduction, according to numerical thermal–mechanical models.
- Gary J. Axen
- , Jolante W. van Wijk
- & Claire A. Currie
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Forced subduction initiation recorded in the sole and crust of the Semail Ophiolite of Oman
The subduction system recorded by the Semail Ophiolite of Oman was initiated by far-field events, according to a comparison of the ages of the upper and lower plate material.
- Carl Guilmette
- , Matthijs A. Smit
- & Dany Savard
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Rapid transition from continental breakup to igneous oceanic crust in the South China Sea
The onset of seafloor spreading in the northern South China Sea was marked by the rapid onset of magmatism and mantle upwelling, suggests an analysis of International Ocean Discovery Program core material.
- H. C. Larsen
- , G. Mohn
- & L. Zhong
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An impact melt origin for Earth’s oldest known evolved rocks
Earth’s oldest known felsic rocks formed by partial melting at low pressures and high temperatures caused by impact melting of mafic Hadean crust, according to phase equilibria and trace element modelling.
- Tim E. Johnson
- , Nicholas J. Gardiner
- & Hugh Smithies
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Extremely early recurrence of intraplate fault rupture following the Tohoku-Oki earthquake
A pair of closely spaced intraplate earthquakes in Japan can be explained by postseismic deformation associated with the 2011 Tohoku-Oki earthquake.
- Yo Fukushima
- , Shinji Toda
- & Kenji Tachibana
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Editorial |
Waste not, want not
Earth’s resources may not be running out, but the planet’s capacity to cope with the resulting waste products is limited. Resource geology can no longer be the preserve of the economic, mining or petroleum geologist; sustainably providing for the world’s population requires a broader skillset.
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Microbial life and biogeochemical cycling on land 3,220 million years ago
Microbial life colonized the land surface by 3.2 billion years ago, forming complex communities distinct from those in nearby marine environments, according to analyses of fossilized microbial mats in the Moodies Group, South Africa.
- Martin Homann
- , Pierre Sansjofre
- & Stefan V. Lalonde
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Riverine evidence for isotopic mass balance in the Earth’s early sulfur cycle
The isotopic composition of sulfur minerals formed during the Archaean can be reconstructed from dissolved sulfur in rivers draining cratons. Analyses from Canada suggest that the Archaean sulfur cycle was in isotopic mass balance.
- Mark A. Torres
- , Guillaume Paris
- & Woodward W. Fischer
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Cambrian Sauk transgression in the Grand Canyon region redefined by detrital zircons
Extensive flooding of the North American continent during the Cambrian occurred more recently and more rapidly than previously thought, according to analyses of detrital zircons sampled from the Grand Canyon region.
- Karl Karlstrom
- , James Hagadorn
- & Laura Crossey
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News & Views |
Valuable snapshots of deep time
A regional oxygenation event 1.6 billion years ago coincided with the appearance of large fossils, but whether the availability of oxygen was the primary driver of the diversification of multicellular organisms remains to be seen.
- Emma U. Hammarlund
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Oxygenation of the Mesoproterozoic ocean and the evolution of complex eukaryotes
The oxygenation of deeper continental shelf waters during the Mesoproterozoic coincided with the appearance of multicellular eukaryotes, according to geochemical and sedimentological analyses of the Yanliao Basin, China.
- Kan Zhang
- , Xiangkun Zhu
- & Simon W. Poulton
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Earth's oldest stable crust in the Pilbara Craton formed by cyclic gravitational overturns
The oldest stable crust on Earth may have formed during pulsed growth cycles, according to geochemical analyses of rocks preserved in the Pilbara Craton, Western Australia.
- Daniel Wiemer
- , Christoph E. Schrank
- & Charlotte M. Allen
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News & Views |
Metal footprint linked to economy
The annual quantity of metal being used by humans has been on the rise. A new analysis of 43 major economies reveals the extent to which year-to-year fluctuations in metal footprints have been in lockstep with countries’ economic growth and changes in investment spending.
- Paul J. Burke
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Modification of the Western Gondwana craton by plume–lithosphere interaction
South American and African cratons may have been substantially modified by mantle plumes, according to analyses of seismic images and tectonic records. The results imply that cratons may not be as stable as once thought.
- Jiashun Hu
- , Lijun Liu
- & Craig Lundstrom