Results 151 to 160 of about 2,038 (207)

Nanometric mineral inclusions from a fluid-rich diamond: identification, structure, and implications for deep Earth. [PDF]

open access: yesNat Commun
Wang Y   +18 more
europepmc   +1 more source

Shear heating reconciles thermal models with the metamorphic rock record of subduction. [PDF]

open access: yesProc Natl Acad Sci U S A, 2018
Kohn MJ   +4 more
europepmc   +1 more source

Granitic intrusions enhance strain localization and rapid mantle exhumation along an oceanic detachment fault. [PDF]

open access: yesSci Adv
Poulaki EM   +35 more
europepmc   +1 more source

Incipient continent formation by shallow melting of an altered mafic protocrust. [PDF]

open access: yesNat Commun
Hartnady MIH   +8 more
europepmc   +1 more source

On thermobarometry

open access: yesJournal of Metamorphic Geology, 2008
AbstractThermobarometry, the estimation of the pressure–temperature (P–T) conditions of metamorphism, can be undertaken by using pseudosection calculations as well as by conventional methods. Conventional thermobarometry uses only the equilibrium thermodynamics of balanced reactions between end‐members of minerals, combined with the observed ...
Roger Powell, T J B Holland
exaly   +4 more sources

Amp-TB2: An Updated Model for Calcic Amphibole Thermobarometry [PDF]

open access: yesMinerals (Basel, Switzerland), 2021
Amphibole (Amp) plays a crucial role in the study of several earth and planetary processes. One of its most common applications is in thermobarometry, especially for volcanic-magmatic systems. However, many thermobarometers require the input of melt composition, which is not always available in volcanic products (e.g., partially crystallized melts or ...
Filippo Ridolfi
exaly   +4 more sources

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