Transition zone
View article: GDGTs and n-alkanes of Weihe Basin sediments at Pliocene-Pleistocene transition
GDGTs and n-alkanes of Weihe Basin sediments at Pliocene-Pleistocene transition Open
View article: GDGTs and n-alkanes of Weihe Basin sediments at Pliocene-Pleistocene transition
GDGTs and n-alkanes of Weihe Basin sediments at Pliocene-Pleistocene transition Open
View article: Global Assessment of the Cloud-Aerosol Transition Zone Using CALIPSO
Global Assessment of the Cloud-Aerosol Transition Zone Using CALIPSO Open
The interactions between clouds and aerosols represent one of the largest uncertainties in assessing the Earth’s radiation budget, highlighting the importance of research on the transition zone (TZ) within the cloud-aerosol continuum. This…
View article: Tectonic Memory in the Mantle: Linking Subduction Zone Evolution to Supercontinent Cycles
Tectonic Memory in the Mantle: Linking Subduction Zone Evolution to Supercontinent Cycles Open
The Earth's mantle preserves a "tectonic memory" of past subduction events, influencing subsequent mantle dynamics and supercontinent cycles. This paper explores the mechanisms by which subducted oceanic lithosphere retains its physical an…
View article: Tectonic Memory in the Mantle: Linking Subduction Zone Evolution to Supercontinent Cycles
Tectonic Memory in the Mantle: Linking Subduction Zone Evolution to Supercontinent Cycles Open
The Earth's mantle preserves a "tectonic memory" of past subduction events, influencing subsequent mantle dynamics and supercontinent cycles. This paper explores the mechanisms by which subducted oceanic lithosphere retains its physical an…
View article: Unlocking Slab Dynamics: A Global Synthesis of Subduction Geometry, Mantle Flow, and Back-Arc Deformation
Unlocking Slab Dynamics: A Global Synthesis of Subduction Geometry, Mantle Flow, and Back-Arc Deformation Open
This study presents a global synthesis of subduction zone dynamics, focusing on the intricate relationships between slab geometry, mantle flow patterns, and back-arc deformation. By integrating seismic tomography, geodynamic modeling, and …
View article: Unlocking Slab Dynamics: A Global Synthesis of Subduction Geometry, Mantle Flow, and Back-Arc Deformation
Unlocking Slab Dynamics: A Global Synthesis of Subduction Geometry, Mantle Flow, and Back-Arc Deformation Open
This study presents a global synthesis of subduction zone dynamics, focusing on the intricate relationships between slab geometry, mantle flow patterns, and back-arc deformation. By integrating seismic tomography, geodynamic modeling, and …
View article: First-row transition elements (FRTE) in spinel and garnet peridotite xenoliths from Mongolia and Siberia
First-row transition elements (FRTE) in spinel and garnet peridotite xenoliths from Mongolia and Siberia Open
View article: Invisible water in subducted crust: Lawsonite velocity anomalies under mantle conditions
Invisible water in subducted crust: Lawsonite velocity anomalies under mantle conditions Open
Subduction zones transport significant amounts of water into Earth’s mantle, primarily through hydrous minerals such as lawsonite. However, the seismic detectability of lawsonite-bearing oceanic crust at mantle depths remains uncertain. To…
View article: Large-scale flow toward low-velocity anomalies reconciles seismic and geodynamic constraints in the deepest mantle beneath Alaska
Large-scale flow toward low-velocity anomalies reconciles seismic and geodynamic constraints in the deepest mantle beneath Alaska Open
Deep mantle downwellings are typically located away from the two Large Low-Velocity Provinces (LLVPs) in Earth's mantle. Geodynamic models based on global seismic tomography generally predict that convective flow at the core-mantle boundar…
View article: First-row transition elements (FRTE) in spinel and garnet peridotite xenoliths from Mongolia and Siberia
First-row transition elements (FRTE) in spinel and garnet peridotite xenoliths from Mongolia and Siberia Open
View article: The Buoyancy of Cratonic Lithospheric Mantle
The Buoyancy of Cratonic Lithospheric Mantle Open
Cratons are generally thought to be characterized by stable, long-lived mantle roots. However, recent studies have suggested that the lithospheric mantle may be prone to removal, implying that it may be denser than the asthenosphere. To ad…
View article: Animations for the paper "Lateral Deformation of Large-scale Coronal Mass Ejections during the Transition from Non-radial to Radial Propagation" (Accepted in ApJ)
Animations for the paper "Lateral Deformation of Large-scale Coronal Mass Ejections during the Transition from Non-radial to Radial Propagation" (Accepted in ApJ) Open
This dataset contains the supplementary animations associated with the manuscript "Lateral Deformation of Large-scale Coronal Mass Ejections during the Transition from Non-radial to Radial Propagation," accepted for publication in The Astr…
View article: Animations for the paper "Lateral Deformation of Large-scale Coronal Mass Ejections during the Transition from Non-radial to Radial Propagation" (Accepted in ApJ)
Animations for the paper "Lateral Deformation of Large-scale Coronal Mass Ejections during the Transition from Non-radial to Radial Propagation" (Accepted in ApJ) Open
This dataset contains the supplementary animations associated with the manuscript "Lateral Deformation of Large-scale Coronal Mass Ejections during the Transition from Non-radial to Radial Propagation," accepted for publication in The Astr…
View article: Data of "Secondary organic aerosol formation during continental to oceanic transition in South China coast: effects of photostationary state, aqueous-phase processes, and heatwaves"
Data of "Secondary organic aerosol formation during continental to oceanic transition in South China coast: effects of photostationary state, aqueous-phase processes, and heatwaves" Open
Aerosol composition, gaseous pollutants, and meteorological parameters measured at the University of Macau site during spring and summer 2024.
View article: Data of "Secondary organic aerosol formation during continental to oceanic transition in South China coast: effects of photostationary state, aqueous-phase processes, and heatwaves"
Data of "Secondary organic aerosol formation during continental to oceanic transition in South China coast: effects of photostationary state, aqueous-phase processes, and heatwaves" Open
Aerosol composition, gaseous pollutants, and meteorological parameters measured at the University of Macau site during spring and summer 2024.
View article: Characterization of soil preferential flow in the paddy field-ridge transition zone of terrace, Southwest China
Characterization of soil preferential flow in the paddy field-ridge transition zone of terrace, Southwest China Open
View article: Plate Tectonic Metamorphosis: Subduction-to-Ridge Transitions and the Wilsonian Remapping of Earth's Surface
Plate Tectonic Metamorphosis: Subduction-to-Ridge Transitions and the Wilsonian Remapping of Earth's Surface Open
Plate tectonics is the fundamental framework for understanding Earth's dynamic surface processes, dictating the creation, consumption, and redistribution of lithosphere. While divergent (mid-ocean ridges) and convergent (subduction zones) …
View article: Plate Tectonic Metamorphosis: Subduction-to-Ridge Transitions and the Wilsonian Remapping of Earth's Surface
Plate Tectonic Metamorphosis: Subduction-to-Ridge Transitions and the Wilsonian Remapping of Earth's Surface Open
Plate tectonics is the fundamental framework for understanding Earth's dynamic surface processes, dictating the creation, consumption, and redistribution of lithosphere. While divergent (mid-ocean ridges) and convergent (subduction zones) …
View article: From Strong Plates to Weak Boundaries: Strain Localization in the Lithospheric Mantle with Low- to High-Temperature Dislocation Creep
From Strong Plates to Weak Boundaries: Strain Localization in the Lithospheric Mantle with Low- to High-Temperature Dislocation Creep Open
Plate-like behavior may be reproduced in numerical experiments of mantle convection if rheology combines a temperature-dependent viscosity capped with a low yield stress. Other processes limiting the mantle ductile strength have been propo…
View article: Large non-mass-dependent iron isotope fractionation in an oxic-anoxic transition zone of lake sediments
Large non-mass-dependent iron isotope fractionation in an oxic-anoxic transition zone of lake sediments Open
View article: A Phase Map for Vertical Upflow of Slightly Cohesive Geldart A Powders Focused on High Solids Mass Flux
A Phase Map for Vertical Upflow of Slightly Cohesive Geldart A Powders Focused on High Solids Mass Flux Open
Flow regimes of vertical upflow for slightly cohesive Geldart A powders at high solids mass flux (Gs≳ 500 kg/m2s) are not fully resolved. In particular, Dense Suspension Upflow (DSU) as a distinct flow regime and its transition boundaries …
View article: Global Finite-Frequency Tomography of the 220-km Discontinuity
Global Finite-Frequency Tomography of the 220-km Discontinuity Open
Summary The asthenosphere is a weak layer in the upper mantle that supports the movement of the overriding tectonic plates and facilitates mantle convection. In this study, we compile a global dataset of SS precursors reflected at the base…
View article: Dual-layered mantle lithosphere beneath southeastern Canadian Cordillera
Dual-layered mantle lithosphere beneath southeastern Canadian Cordillera Open
The craton edge beneath southwestern Canada has been characterized as a 'lithospheric step' involving the transition from the warm Cordillera to an ancient, mechanically strong North American craton. Using converted shear waves that are se…
View article: Crystal-mush remobilization timescales and magma storage depth in the Snæfellsnes Volcanic Zone (W-Iceland): insights from olivine Fe-Mg diffusion chronometry and fluid inclusion barometry
Crystal-mush remobilization timescales and magma storage depth in the Snæfellsnes Volcanic Zone (W-Iceland): insights from olivine Fe-Mg diffusion chronometry and fluid inclusion barometry Open
Constraining the conditions and timescales of magma storage, mixing, and transfer—and understanding how deep-seated unrest progresses towards eruption—is key to deciphering early stages of magma system reactivation. While these processes a…
View article: Effect of Distributed Roughness Elements on Crossflow Transition in a Yawed Cone in a Mach 6 Wind Tunnel
Effect of Distributed Roughness Elements on Crossflow Transition in a Yawed Cone in a Mach 6 Wind Tunnel Open
Research on hypersonic crossflow transition holds significant engineering and scientific importance. This paper investigates the impact of distributed roughness elements (DREs) on crossflow transition for a cone set at a 6° angle of attack…
View article: Self-limiting precipitation recycling during event-scale wet episodes in north-western China’s semi-arid transition zone
Self-limiting precipitation recycling during event-scale wet episodes in north-western China’s semi-arid transition zone Open
Recent decades have seen a marked climatic wetting across north-western China’s semi-arid transition zone, yet the extent to which this intensification arises from local land–atmosphere feedback or from external moisture inflow remains unc…
View article: Rapid Continental Reorganization Through Hydraulic Collapse: A Solution to the Heat Problem in Catastrophic Plate Tectonics
Rapid Continental Reorganization Through Hydraulic Collapse: A Solution to the Heat Problem in Catastrophic Plate Tectonics Open
Zenodo Entry Description - Version 2 Date: 2025-11-22DOI Concept: 10.5281/zenodo.17663309Status: Version 2 description for Appendix C release This paper proposes a hydraulic collapse mechanism for rapid, global-scale tectonic reorganizatio…
View article: Rapid Continental Reorganization Through Hydraulic Collapse: A Solution to the Heat Problem in Catastrophic Plate Tectonics
Rapid Continental Reorganization Through Hydraulic Collapse: A Solution to the Heat Problem in Catastrophic Plate Tectonics Open
Zenodo Entry Description - Version 2 Date: 2025-11-22DOI Concept: 10.5281/zenodo.17663309Status: Version 2 description for Appendix C release This paper proposes a hydraulic collapse mechanism for rapid, global-scale tectonic reorganizatio…
View article: Assessment of Climatic Trends and Change Points in the Western Agro-climatic Zone of Madhya Pradesh, India
Assessment of Climatic Trends and Change Points in the Western Agro-climatic Zone of Madhya Pradesh, India Open
This study examines the temporal variability, trend, and change point behaviour of key climatic parameters including annual rainfall, monsoon rainfall, number of rainy days, and one day maximum rainfall in the Western Agro-climatic Zone of…