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A Machine Learning‐Based Approach to Clinopyroxene Thermobarometry: Model Optimization and Distribution for Use in Earth Sciences [PDF]

open access: yesJournal of Geophysical Research: Solid Earth, 2022
Thermobarometry is a fundamental tool to quantitatively interrogate magma plumbing systems and broaden our appreciation of volcanic processes. Developments in random forest‐based machine learning lend themselves to a data‐driven approach to clinopyroxene
Maurizio Petrelli   +2 more
exaly   +3 more sources

Elastic Thermobarometry [PDF]

open access: yesAnnual Review of Earth and Planetary Sciences, 2023
Upon exhumation and cooling, contrasting compressibilities and thermal expansivities induce differential strains (volume mismatches) between a host crystal and its inclusions. These strains can be quantified in situ using Raman spectroscopy or X-ray diffraction.
Kohn M. J.   +2 more
core   +4 more sources

Eclogite thermobarometry: The consistency between conventional thermobarometry and forward phase‐equilibrium modelling

open access: yesJournal of Metamorphic Geology, 2023
AbstractEclogite thermobarometry is crucial for constraining the depths and temperatures to which oceanic and continental crust subduct. However, obtaining the pressure and temperature (P–T) conditions of eclogites is complex as they commonly display high‐variance mineral assemblages, and the mineral compositions only vary slightly with P–T.
David Hernández‐Uribe   +2 more
openaire   +3 more sources

Thermobar: An open-source Python3 tool for thermobarometry and hygrometry

open access: yesVolcanica, 2022
We present Thermobar, a new open-source Python3 package for calculating pressures, temperatures, and melt compositions from mineral and mineral-melt equilibrium.
Penny Wieser   +6 more
doaj   +3 more sources

The Influence of Undercooling and Sector Zoning on Clinopyroxene–Melt Equilibrium and Thermobarometry [PDF]

open access: yesJournal of Petrology, 2023
Abstract Thermobarometry provides a critical means of assessing locations of magma storage and dynamics in the lead-up to volcanic eruptions and crustal growth. A common approach is to utilise minerals that have compositions sensitive to changes in pressure and/or temperature, such as clinopyroxene, which is ubiquitous in mafic to ...
Alice MacDonald   +4 more
openaire   +5 more sources

THERMOBAROMETRY OF DEPLETED PERIDOTITES

open access: yesГеодинамика и тектонофизика
An assessment was made of the possibility of using olivine thermobarometry for xenoliths of depleted peridotites from the Udachnaya pipe (Yakutia), represented by 76 megacrystalline dunites and 5 megacrystalline harzburgites.
L. N. Pokhilenko   +2 more
doaj   +2 more sources

Garnet Chemical Zoning Based Thermobarometry: Method Evaluation and Applications in the Menderes Massif, Western Turkey

open access: yesGeosciences (Switzerland), 2021
The garnet chemical zoning method (GZM) is a reliable thermodynamic approach for forward modeling pressure-temperature (P-T) paths using observed garnet and bulk rock compositions.
Elizabeth Catlos, Thomas Etzel
exaly   +3 more sources

Mapping Global Lithospheric Mantle Pressure‐Temperature Conditions by Machine‐Learning Thermobarometry

open access: yesGeophysical Research Letters
Comprehending the temperature distribution within Earth's lithospheric mantle is of paramount importance for understanding the dynamics of Earth's interior.
Ben Qin   +5 more
doaj   +4 more sources

Elastic-thermobarometry: methods and applications to ultrahigh pressure metamorphic rocks

open access: yesPlinius, 2020
Ultra-High Pressure (UHP) metamorphic rocks represent the evidence we have for the detailed reconstruction of tectonic processes, which are the source of major natural hazards like deep-focus earthquakes and volcanic eruptions. Mineral inclusions are often the only proof of ultrahigh pressure metamorphism and their study provides insights into the ...
CAMPOMENOSI, NICOLA
openaire   +3 more sources

Fluid Inclusion Thermobarometry as a Tracer for Magmatic Processes

open access: yesReviews in Mineralogy and Geochemistry, 2008
Fluid inclusions in minerals may form in any type of volcanic or plutonic rock ranging from mafic to silicic compositions. Because all igneous rocks reach fluid saturation at some stage during their evolution, fluids trapped as inclusions in magmatic minerals belong to a certain paragenesis or phase assemblage, which may include minerals, melts and one
T. H. Hansteen, A. Klugel
core   +4 more sources

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