A new approach to geobarometry by combining fluid inclusion and clumped isotope thermometry in hydrothermal carbonates

Author:

Honlet Robin1ORCID,Gasparrini Marta2,Muchez Philippe1,Swennen Rudy1,John Cédric M.3

Affiliation:

1. Department of Earth and Environmental Sciences; KU Leuven; Heverlee Belgium

2. IFP Energies Nouvelles; Georesources Department; Rueil-Malmaison Cedex France

3. Department of Earth Science and Engineering and Qatar Carbonate and Carbon Storage Research Centre; Imperial College London; London UK

Funder

Fonds Wetenschappelijk Onderzoek

Qatar Petroleum

Shell

Qatar Science and Technology Park

Publisher

Wiley

Subject

Geology

Reference43 articles.

1. Paleogeographic inversion resulting from large out of sequence breaching thrusts: The León Fault (Cantabrian Zone, NW Iberia). A new picture of the external Variscan Thrust Belt in the Ibero-Armorican Arc;Alonso;Geologica Acta,2009

2. Calibration of the dolomite clumped isotope thermometer from 25 to 350°C, and implications for a universal calibration for all (Ca, Mg, Fe)CO3 carbonates;Bonifacie;Geochimica et Cosmochimica Acta,2017

3. Comparison of clumped isotope signatures of dolomite cements to fluid inclusion thermometry in the temperature range of 73-176 & #xB0;C;Came;Geochimica et Cosmochimica Acta,2017

4. Carrière , K. L. 2006 Neoproterozoic to Holocene tectonothermal evolution of the southern Cantabrian Mountains NW Iberia, revealed by apatite fission-track thermochronology

5. Absolute isotopic abundance ratios and the accuracy of Δ47 measurements;Daëron;Chemical Geology,2016

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