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DFENS: Diffusion Chronometry Using Finite Elements and Nested Sampling

open access: yesGeochemistry, Geophysics, Geosystems, 2021
In order to reconcile petrological and geophysical observations of magmatic processes in the temporal domain, the uncertainties in diffusion timescales need to be rigorously assessed.
Euan J. F. Mutch   +4 more
doaj   +12 more sources

Diffusion chronometry and the timescales of magmatic processes [PDF]

open access: yesNature Reviews Earth & Environment, 2020
Volcanic eruptions can represent major societal hazards. Placing tighter bounds on the timescales of magmatic processes that precede eruptions is, therefore, important for volcano monitoring and forecasting. Diffusion chronometry, where volcanic crystals that contain chemical gradients are treated as time capsules, allows the timescale of various ...
Thomas Shea   +2 more
exaly   +8 more sources

Leveraging radioisotope geochronology and diffusion chronometry to trace the thermal evolution of magmatic systems [PDF]

open access: yesNational Science Review
Time scales determined by radioisotope geochronology and diffusion chronometry for the same magmatic systems have shown variable degrees of discrepancy. We show in this paper that this could be due to the different temperature ranges that the two types of chronometers are effectively sampling, therefore combining them will help to trace the thermal ...
Weiran Li, Fidel Costa
exaly   +4 more sources

Cooling rates and melt extraction timescales determined by diffusion chronometry on shallow crustal plutonic rocks [PDF]

open access: yesContributions To Mineralogy and Petrology
Abstract Diffusion chronometry has emerged as a valuable tool to track the timescales of magmatic processes and is now routinely applied on erupted volcanic products to infer crystal residence times and mixing-to-eruption timescales. Despite some attempts to apply such a technique to plutonic rocks, slow cooling in these systems complicates ...
Anne-Sophie Bouvier   +2 more
exaly   +4 more sources

Diffusion chronometry of volcanic rocks: looking backward and forward

open access: yesBulletin of Volcanology, 2022
AbstractDiffusion of elements that result in compositional zoning in minerals in volcanic rocks may be used to determine the timescales of various volcanic processes (e.g., residence times in different reservoirs, ascent rates of magmas). Here, we introduce the tool and discuss the reasons for its gain in popularity in recent times, followed by a ...
Ralf Dohmen, Sumit Chakraborty
exaly   +2 more sources

Carbonate-capped seamount subduction accelerates CO2-rich arc magma ascent [PDF]

open access: yesNature Communications
Subduction transports carbon into Earth’s interior, yet how subducted carbon influences arc magma ascent dynamics remains unclear. Here we combine volatile compositions of olivine-hosted melt inclusions with olivine diffusion chronometry at Pagan volcano
Xiaohan Huang   +6 more
doaj   +2 more sources

Multiple mush generations provide insight into the longevity of open-conduit basaltic volcanoes [PDF]

open access: yesScientific Reports
Investigating the dynamics and timescales of magmatic processes in open-conduit basaltic volcanoes is crucial for improving our understanding of explosive eruptions and better assessing volcanic hazards.
Beatrice Schiavon   +9 more
doaj   +2 more sources

Timescales of mixing and mobilisation in the Bishop Tuff magma body: perspectives from diffusion chronometry [PDF]

open access: yesContributions To Mineralogy and Petrology, 2014
We present two-feldspar thermometry and diffusion chronometry from sanidine, orthopyroxene and quartz from multiple samples of the Bishop Tuff, California, to constrain the temperature stratification within the pre-eruptive magma body and the timescales of magma mixing prior to its evacuation.
Colin Wilson   +2 more
exaly   +4 more sources

Ascent rate of the Udachnaya-East kimberlite melts from olivine diffusion chronometry

open access: yesEarth and Planetary Science Letters, 2023
Kimberlite melts are low volume, volatile-rich melts formed in the asthenosphere at depth >150-250 km. Due to their low viscosity and the exsolution of CO2 triggered by their interaction with the sub-cratonic mantle, these melts are highly buoyant and rise rapidly through the lithosphere, ultimately reaching the surface and erupting at sonic to ...
Olga Ageeva   +2 more
exaly   +2 more sources

DiffSim: a user-friendly tool for precise magmatic timescale determination and error propagation via major element diffusion chronometry in magmatic phases

open access: yesFrontiers in Earth Science
Diffusion chronometry is a technique gaining interest in the scientific community related to volcanology and petrology; however, modelling can be challenging for non-expert users.
Eduardo Morgado, Daniel J. Morgan
doaj   +3 more sources

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