scholarly article | Q13442814 |
P2093 | author name string | Pietro Sternai | |
P2860 | cites work | Gneiss domes and crustal flow | Q102196028 |
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Plate tectonic controls on atmospheric CO2 levels since the Triassic | Q28660540 | ||
Glacial cycles drive variations in the production of oceanic crust | Q41233404 | ||
Depth-dependent extension, two-stage breakup and cratonic underplating at rifted margins. | Q41982412 | ||
Magma-assisted rifting in Ethiopia. | Q43530339 | ||
Is "Hotspot" Volcanism a Consequence of Plate Tectonics? | Q43587831 | ||
Magmatism at rift zones: The generation of volcanic continental margins and flood basalts | Q55878089 | ||
Deglaciation and glacial erosion: A joint control on magma productivity by continental unloading | Q56092785 | ||
The effect of deglaciation on mantle melting beneath Iceland | Q56384486 | ||
Feedback between deglaciation, volcanism, and atmospheric CO2 | Q56533749 | ||
Dynamic processes controlling evolution of rifted basins | Q56851082 | ||
TOPO-EUROPE: The geoscience of coupled deep Earth-surface processes | Q56851086 | ||
Large igneous provinces: Crustal structure, dimensions, and external consequences | Q57229359 | ||
CRUST 5.1: A global crustal model at 5° × 5° | Q57308373 | ||
Environmental signal propagation in sedimentary systems across timescales | Q57851580 | ||
Water follows carbon: CO2 incites deep silicate melting and dehydration beneath mid-ocean ridges | Q57857285 | ||
Mantle solidus: Experimental constraints and the effects of peridotite composition | Q57857385 | ||
Potential links between continental rifting, CO2 degassing and climate change through time | Q57858369 | ||
Magma Dynamics with the Enthalpy Method: Benchmark Solutions and Magmatic Focusing at Mid-ocean Ridges | Q57861705 | ||
Excess temperatures at ocean islands: Implications for mantle layering and convection | Q58211186 | ||
Ocean Basin Evolution and Global-Scale Plate Reorganization Events Since Pangea Breakup | Q58839735 | ||
Magmatism at rifted continental margins | Q59061034 | ||
Late Cenozoic uplift of mountain ranges and global climate change: chicken or egg? | Q59066908 | ||
Rifting, lithosphere breakup and volcanism: Comparison of magma-poor and volcanic rifted margins | Q60294248 | ||
Evolution of magma-poor continental margins from rifting to seafloor spreading | Q60297686 | ||
Controls of inherited lithospheric heterogeneity on rift linkage: Numerical and analog models of interaction between the Kenyan and Ethiopian rifts across the Turkana depression | Q60301213 | ||
Rifted margin architecture and crustal rheology: Reviewing Iberia-Newfoundland, Central South Atlantic, and South China Sea | Q60301214 | ||
Analogue modelling of continental extension: a review focused on the relations between the patterns of deformation and the presence of magma | Q61041967 | ||
Transition from continental break-up to punctiform seafloor spreading: How fast, symmetric and magmatic | Q61041971 | ||
Magma-induced strain localization in centrifuge models of transfer zones | Q61041972 | ||
Thermal structure of the North American uppermost mantle inferred from seismic tomography | Q63947161 | ||
Emplacement of metamorphic core complexes and associated geothermal systems controlled by slab dynamics | Q68873144 | ||
The role of viscous heating in Barrovian metamorphism of collisional orogens: thermomechanical models and application to the Lepontine Dome in the Central Alps | Q70085267 | ||
Milankovitch frequencies in tephra records at volcanic arcs: The relation of kyr-scale cyclic variations in volcanism to global climate changes | Q70684049 | ||
A model for the origin of large silicic magma chambers: precursors of caldera-forming eruptions | Q96484454 | ||
Thermal perturbation, mineral assemblages, and rheology variations induced by dyke emplacement in the crust | Q101011024 | ||
P433 | issue | 1 | |
P304 | page(s) | 7711 | |
P577 | publication date | 2020-05-07 | |
P1433 | published in | Scientific Reports | Q2261792 |
P1476 | title | Surface processes forcing on extensional rock melting | |
P478 | volume | 10 |
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