Changes in fluid pathways in a calcite vein mesh (Natih Formation, Oman Mountains): insights from stable isotopes

Author:

Arndt M.1,Virgo S.1,Cox S. F.2,Urai J. L.13

Affiliation:

1. Structural Geology; Tectonics and Geomechanics; Energy and Mineral Resources Group (EMR), RWTH Aachen University; Lochnerstrasse 4-20 52056 Aachen Germany

2. Research School of Earth Sciences; The Australian National University; Canberra ACT Australia

3. German University of Technology; GUtech; Muscat Oman

Funder

Australian Research Council

ExxonMobil Production Deutschland GmbH

GDF SUEZ E&P Deutschland GmbH

RWE Dea AG and Wintershall Holding GmbH

Publisher

Wiley

Subject

General Earth and Planetary Sciences

Reference105 articles.

1. Implications of kinetically controlled mineral-fluid exchange on the geometry of stable-isotope fronts;Abart;European Journal of Mineralogy,2000

2. Grain-scale stable isotope disequilibrium during fluid-rock interaction; 1, Series approximations for advective-dispersive transport and first-order kinetic mineral-fluid exchange;Abart;American Journal of Science,1997

3. Oxygen, carbon and strontium isotope systematics in two profiles across the Glarus thrust: implications for fluid flow;Abart;Contributions to Mineralogy and Petrology,2002

4. Fluid conduits in carbonate-hosted seismogenic normal faults of central Italy;Agosta;Journal of Geophysical Research: Solid Earth,2003

5. Late Albian, Cenomanian and Turonian Natih Supersequence of Oman; type section for Orbiton 7 (103.6-89.0 Ma);Al-Husseini;GeoArabia [Manama],2010

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