| The geophysics, geology and mechanics of slow fault slip |
48 |
| Evolution of the Toarcian (Early Jurassic) carbon-cycle and global climatic controls on local sedimentary processes (Cardigan Bay Basin, UK) |
29 |
| Origin of the non-carbonaceous-carbonaceous meteorite dichotomy |
27 |
| Age of Izu-Bonin-Mariana arc basement |
27 |
| Two distinct origins for Archean greenstone belts |
25 |
| Geodynamics of kimberlites on a cooling Earth: Clues to plate tectonic evolution and deep volatile cycles |
25 |
| Constraining the evolution of Neogene ocean carbonate chemistry using the boron isotope pH proxy |
23 |
| Mercury anomalies across the end Permian mass extinction in South China from shallow and deep water depositional environments |
23 |
| Dual control of fault intersections on stop-start rupture in the 2016 Central Italy seismic sequence |
22 |
| Forearc ages reveal extensive short-lived and rapid seafloor spreading following subduction initiation |
22 |
| Secular change in TTG compositions: Implications for the evolution of Archaean geodynamics |
22 |
| Terrestrial sources as the primary delivery mechanism of mercury to the oceans across the Toarcian Oceanic Anoxic Event (Early Jurassic) |
22 |
| Uranium isotope evidence for an expansion of anoxia in terminal Ediacaran oceans |
22 |
| An Andean-type retro-arc foreland system beneath northwest South China revealed by SINOPROBE profiling |
21 |
| Mercury in marine Ordovician/Silurian boundary sections of South China is sulfide-hosted and non-volcanic in origin |
21 |
| Petrogenesis and tectonics of the Acasta Gneiss Complex derived from integrated petrology and Nd-142 and W-182 extinct nuclide-geochemistry |
20 |
| Crustal structure and deformation beneath eastern and northeastern Tibet revealed by P-wave receiver functions |
20 |
| Modulation of magmatic processes by CO2 flushing |
20 |
| Using the magmatic record to constrain the growth of continental crust-The Eoarchean zircon Hf record of Greenland |
20 |
| Daily bathymetric surveys document how stratigraphy is built and its extreme incompleteness in submarine channels |
20 |
| Transition from a warm and dry to a cold and wet climate in NE China across the Holocene |
20 |
| Global seawater redox trends during the Late Devonian mass extinction detected using U isotopes of marine limestones |
18 |
| Multiple episodes of fast exhumation since Cretaceous in southeast Tibet, revealed by low-temperature thermochronology |
18 |
| Structures within the oceanic crust of the central South China Sea basin and their implications for oceanic accretionary processes |
18 |
| Sulfur isotopes in rivers: Insights into global weathering budgets, pyrite oxidation, and the modern sulfur cycle |
18 |
| Biolabile ferrous iron bearing nanoparticles in glacial sediments |
18 |
| Controls on the barium isotope compositions of marine sediments |
17 |
| On the development of the calc-alkaline and tholeiitic magma series: A deep crustal cumulate perspective |
17 |
| Influences of large-scale convection and moisture source on monthly precipitation isotope ratios observed in Thailand, Southeast Asia |
17 |
| A re-assessment of the oxidation state of iron in MORB glasses |
17 |
| Global mercury cycle during the end-Permian mass extinction and subsequent Early Triassic recovery |
17 |
| Relationships between CO thermodynamic limits on silicate weathering, and the strength of the silicate weathering feedback |
17 |
| Beyond Byerlee friction, weak faults and implications for slip behavior |
16 |
| Tracking variable sedimentation rates and astronomical forcing in Phanerozoic paleoclimate proxy series with evolutionary correlation coefficients and hypothesis testing |
16 |
| Geochemical nature of sub-ridge mantle and opening dynamics of the South China |
16 |
| Did climate changes trigger the Late Devonian Kellwasser Crisis? Evidence from a high-resolution conodont delta O-18(PO4) record from South China |
16 |
| The 2016 Kaikoura earthquake: Simultaneous rupture of the subduction interface and overlying faults |
16 |
| Insight into zircon REE oxy-barometers: A lattice strain model perspective |
16 |
| Criteria and tools for determining drainage divide stability |
16 |
| Larger earthquakes recur more periodically: New insights in the megathrust earthquake cycle from lacustrine turbidite records in south-central Chile |
15 |
| Sedimentary evidence for enhanced hydrological cycling in response to rapid carbon release during the early Toarcian oceanic anoxic event |
15 |
| Evolution of b-value during the seismic cycle: Insights from laboratory experiments on simulated faults |
15 |
| A Tianshan Mountains loess-paleosol sequence indicates anti-phase climatic variations in arid central Asia and in East Asia |
15 |
| The effect of oxygen fugacity on the rheological evolution of crystallizing basaltic melts |
15 |
| On spreading modes and magma supply at slow and ultraslow mid-ocean ridges |
14 |
| An early diagenetic deglacial origin for basal Ediacaran cap dolostones |
14 |
| Cyclostratigraphic constraints on the duration of the Datangpo Formation and the onset age of the Nantuo (Marinoan) glaciation in South China |
14 |
| Rapid crustal growth and efficient crustal recycling in the early Earth: Implications for Hadean and Archean geodynamics |
14 |
| Early Miocene birth of modern Pearl River recorded low-relief, high-elevation surface formation of SE Tibetan Plateau |
14 |
| Continent stabilisation by lateral accretion of subduction zone-processed depleted mantle residues; insights from Zealandia |
14 |
