Redox-controlled mechanisms of C and H isotope fractionation between silicate melt and COH fluid in the Earth’s interior

to related objects

Location: Deutsche Nationalbibliothek Frankfurt am Main

ISSN: 2197-4284

Extent: Online-Ressource

Language: Englisch

Notes: online resource.

Bibliographic citation: Redox-controlled mechanisms of C and H isotope fractionation between silicate melt and COH fluid in the Earth’s interior ; volume:5 ; number:1 ; day:1 ; month:9 ; year:2018 ; pages:1-17 ; date:12.2018
Progress in Earth and Planetary Science ; 5, Heft 1 (1.9.2018), 1-17, 12.2018

Classification: Geowissenschaften

Creator: Mysen, Bjorn

Contributor: SpringerLink (Online service)

DOI: 10.1186/s40645-018-0203-8

URN: urn:nbn:de:101:1-2018102020475144387412

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:35 AM CEST

Data provider

This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.

Show original at data provider

Associated

Mysen, Bjorn
SpringerLink (Online service)

Other Objects (12)

Silicate solution, cation properties, and mass transfer by aqueous fluid in the Earth’s interior

$Iron isotope fractionation in carbonatite melt systems$

Iron isotope fractionation in carbonatite melt systems

Carbon-bearing silicate melt at deep mantle conditions

$Trace element fractionation between biotite, allanite, and granitic melt$

Trace element fractionation between biotite, allanite, and granitic melt

Nanoscale silicate melt textures determine volcanic ash surface chemistry

Iron alloys of volatile elements in the deep Earth’s interior

Stability of iron-bearing carbonates in the deep Earth’s interior

$High-temperature boron partitioning and isotope fractionation between basaltic melt and fluid$

High-temperature boron partitioning and isotope fractionation between basaltic melt and fluid

Mass transfer in the Earth’s interior: fluid-melt interaction in aluminosilicate–C–O–H–N systems at high pressure and temperature under oxidizing conditions

A discovery of nanoscale sulfide droplets in MORB glasses: Implications for the immiscibility of sulfide melt and silicate melt

How lowermost mantle viscosity controls the chemical structure of Earth’s deep interior

Hochschulschrift

Melt Synthesis, Structural, Characterization and Scaling of Swelling 2:1-Layer Silicate Materials

Silicate solution, cation properties, and mass transfer by aqueous fluid in the Earth’s interior

$Iron isotope fractionation in carbonatite melt systems$

Iron isotope fractionation in carbonatite melt systems

Carbon-bearing silicate melt at deep mantle conditions

$Trace element fractionation between biotite, allanite, and granitic melt$

Trace element fractionation between biotite, allanite, and granitic melt

Nanoscale silicate melt textures determine volcanic ash surface chemistry

Iron alloys of volatile elements in the deep Earth’s interior

Stability of iron-bearing carbonates in the deep Earth’s interior

$High-temperature boron partitioning and isotope fractionation between basaltic melt and fluid$

High-temperature boron partitioning and isotope fractionation between basaltic melt and fluid

Mass transfer in the Earth’s interior: fluid-melt interaction in aluminosilicate–C–O–H–N systems at high pressure and temperature under oxidizing conditions

A discovery of nanoscale sulfide droplets in MORB glasses: Implications for the immiscibility of sulfide melt and silicate melt

How lowermost mantle viscosity controls the chemical structure of Earth’s deep interior

Hochschulschrift

Melt Synthesis, Structural, Characterization and Scaling of Swelling 2:1-Layer Silicate Materials

Silicate solution, cation properties, and mass transfer by aqueous fluid in the Earth’s interior

$Iron isotope fractionation in carbonatite melt systems$

Iron isotope fractionation in carbonatite melt systems

Carbon-bearing silicate melt at deep mantle conditions

$Trace element fractionation between biotite, allanite, and granitic melt$

Trace element fractionation between biotite, allanite, and granitic melt

Nanoscale silicate melt textures determine volcanic ash surface chemistry

Iron alloys of volatile elements in the deep Earth’s interior

Stability of iron-bearing carbonates in the deep Earth’s interior

$High-temperature boron partitioning and isotope fractionation between basaltic melt and fluid$

High-temperature boron partitioning and isotope fractionation between basaltic melt and fluid

Mass transfer in the Earth’s interior: fluid-melt interaction in aluminosilicate–C–O–H–N systems at high pressure and temperature under oxidizing conditions

A discovery of nanoscale sulfide droplets in MORB glasses: Implications for the immiscibility of sulfide melt and silicate melt

How lowermost mantle viscosity controls the chemical structure of Earth’s deep interior

Hochschulschrift

Melt Synthesis, Structural, Characterization and Scaling of Swelling 2:1-Layer Silicate Materials

Cultural heritage institutions wishing to register will find more information here.

Fields marked * need to be filled in.

Username*

Please enter your username

Email*

Please enter your email address

Please do not fill this field

First name

Last name

Password*

Please enter your password

Confirm password*

Please enter the same password

I have read the terms of use and the privacy policy for the collection of personal data and accept them. *

This field is required.

I would like to subscribe to the newsletter of the Deutsche Digitale Bibliothek. See newsletter subscription info.

Account created

Your "My DDB" account has been successfully created. Before you can log in to your account, you must click the confirmation link in the message we just sent to the email address you provided.

Redox-controlled mechanisms of C and H isotope fractionation between silicate melt and COH fluid in the Earth’s interior

Object Details

References and Relationships

Classification and Topics

Contributors, Places and Time

Further information

Data provider

Associated

Other Objects (12)

Silicate solution, cation properties, and mass transfer by aqueous fluid in the Earth’s interior

Iron isotope fractionation in carbonatite melt systems

Carbon-bearing silicate melt at deep mantle conditions

Trace element fractionation between biotite, allanite, and granitic melt

Nanoscale silicate melt textures determine volcanic ash surface chemistry

Iron alloys of volatile elements in the deep Earth’s interior

Stability of iron-bearing carbonates in the deep Earth’s interior

High-temperature boron partitioning and isotope fractionation between basaltic melt and fluid

Mass transfer in the Earth’s interior: fluid-melt interaction in aluminosilicate–C–O–H–N systems at high pressure and temperature under oxidizing conditions

A discovery of nanoscale sulfide droplets in MORB glasses: Implications for the immiscibility of sulfide melt and silicate melt

How lowermost mantle viscosity controls the chemical structure of Earth’s deep interior

Melt Synthesis, Structural, Characterization and Scaling of Swelling 2:1-Layer Silicate Materials

Silicate solution, cation properties, and mass transfer by aqueous fluid in the Earth’s interior

Iron isotope fractionation in carbonatite melt systems

Carbon-bearing silicate melt at deep mantle conditions

Trace element fractionation between biotite, allanite, and granitic melt

Nanoscale silicate melt textures determine volcanic ash surface chemistry

Iron alloys of volatile elements in the deep Earth’s interior

Stability of iron-bearing carbonates in the deep Earth’s interior

High-temperature boron partitioning and isotope fractionation between basaltic melt and fluid

Mass transfer in the Earth’s interior: fluid-melt interaction in aluminosilicate–C–O–H–N systems at high pressure and temperature under oxidizing conditions

A discovery of nanoscale sulfide droplets in MORB glasses: Implications for the immiscibility of sulfide melt and silicate melt

How lowermost mantle viscosity controls the chemical structure of Earth’s deep interior

Melt Synthesis, Structural, Characterization and Scaling of Swelling 2:1-Layer Silicate Materials

Silicate solution, cation properties, and mass transfer by aqueous fluid in the Earth’s interior

Iron isotope fractionation in carbonatite melt systems

Carbon-bearing silicate melt at deep mantle conditions

Trace element fractionation between biotite, allanite, and granitic melt

Nanoscale silicate melt textures determine volcanic ash surface chemistry

Iron alloys of volatile elements in the deep Earth’s interior

Stability of iron-bearing carbonates in the deep Earth’s interior

High-temperature boron partitioning and isotope fractionation between basaltic melt and fluid

Mass transfer in the Earth’s interior: fluid-melt interaction in aluminosilicate–C–O–H–N systems at high pressure and temperature under oxidizing conditions

A discovery of nanoscale sulfide droplets in MORB glasses: Implications for the immiscibility of sulfide melt and silicate melt

How lowermost mantle viscosity controls the chemical structure of Earth’s deep interior

Melt Synthesis, Structural, Characterization and Scaling of Swelling 2:1-Layer Silicate Materials

Related objects

Reset password