The high P-T stability of fluor-apatite in peridotitic and harzburgitic rocks – implications for transport, storage and recycling of phosphorus, volatiles and incompatible trace elements in the slab-mantle wedge system

Creator(s):

Konzett, Jürgen; ORCID: 0000-0003-4223-4078
Pausch, Tristan; ORCID: 0009-0002-7297-7649
Joachim-Mrosko, Bastian; ORCID: 0000-0003-2134-004X

Abstract:

Composition of starting materials and electron microprobe analyses of mineral phases from high-P-T experiments using a model peridotite and a harzburgite doped with fluor apatite and trace elements to study the compositional evolution of apatite and tuite and coexisting silicate and oxide phases as a function of P, T and bulk composition.

How to cite this dataset:

Konzett, J., Pausch, T., Joachim-Mrosko, B., 2024. The high P-T stability of fluor-apatite in peridotitic and harzburgitic rocks – implications for transport, storage and recycling of phosphorus, volatiles and incompatible trace elements in the slab-mantle wedge system, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.60520/IEDA/113399. Accessed 2025-02-22.

DOI Creation Date:

2024-08-06

License:

Creative Commons Attribution 4.0 International [CC-BY-4.0]

Funding source(s):

Austrian Science Fund Grant DOI 10.55776/P33124

Keyword(s):

Coverage Scope: Global
Geographic Location: Earth's upper mantle

User Contributed Keyword(s):

apatite, tuite, fluorine, peridotite, P-T stability, subduction zone

Data Available On:

2024-08-07

Resource Type:

Dataset

Dataset Information

DOI: 10.60520/IEDA/113399

The high P-T stability of fluor-apatite in peridotitic and harzburgitic rocks – implications for transport, storage and recycling of phosphorus, volatiles and incompatible trace elements in the slab-mantle wedge system