Entity

Time filter

Source Type

Oslo, Norway

Buatier M.D.,University of Franche Comte | Cavailhes T.,Montpellier University | Cavailhes T.,DNO International ASA | Charpentier D.,University of Franche Comte | And 4 more authors.
Journal of Structural Geology | Year: 2015

Fault affecting silicoclastic sediments are commonly enriched in clay minerals. Clays are sensitive to fluid-rock interactions and deformation mechanisms; in this paper, they are used as proxy for fault activity and behavior. The present study focuses on clay mineral assemblages from the Point Vert normal fault zone located in the Annot sandstones, a Priabonian-Rupelian turbidite succession of the Alpine foredeep in SE France. In this area, the Annot sandstones were buried around 6-8km below the front of Alpine nappes soon after their deposition and exhumed during the middle-late Miocene. The fault affects arkosic sandstone beds alternating with pelitic layers, and displays throw of about thirty meters. The fault core zone comprises intensely foliated sandstones bounding a corridor of gouge about 20cm thick. The foliated sandstones display clay concentration along S-C structures characterized by dissolution of K-feldspar and their replacement by mica, associated with quartz pressure solution, intense microfracturation and quartz vein precipitation. The gouge is formed by a clayey matrix containing fragments of foliated sandstones and pelites. However, a detailed petrographical investigation suggests complex polyphase deformation processes. Optical and SEM observations show that the clay minerals fraction of all studied rocks (pelites and sandstones from the damage and core zones of the fault) is dominated by white micas and chlorite. These minerals have two different origins: detrital and newly-formed. Detrital micas are identified by their larger shape and their chemical composition with a lower Fe-Mg content than the newly-formed white micas. In the foliated sandstones, newly-formed white micas are concentrated along S-C structures or replace K-feldspar. Both types of newly formed micas display the same chemical composition confirmed microstructural observations suggesting that they formed in the same conditions. They have the following structural formulas: Na0.05 K0.86 (Al 1.77 Fe0.08 Mg0.15) (Si3.22 Al0.78) O10 (OH)2. They are enriched in Fe and Mg compared to the detrital micas. Newly-formed chlorites are associated with micas along the shear planes. According to microprobe analyses, they present the following structural formula: (Al1,48 Fe2,50 Mg1,84) (Si2,82 Al1,18) O10 (OH)8. All these data suggest that these clay minerals are synkinematic and registered the fault activity. In the gouge samples, illite and chlorite are the major clay minerals; smectite is locally present in some samples. In the foliated sandstones, Kubler Index (KI) ((001) XRD peak width at half height) data and thermodynamic calculations from synkinematic chlorite chemistry suggest that the main fault deformation occurred under temperatures around 220°C (diagenesis to anchizone boundary). KI measured on pelites and sandstones from the hanging and footwall, display similar values coherent with the maximal burial temperature of the Annot sandstones in this area. The gouge samples have a higher KI index, which could be explained by a reactivation of the fault at lower temperatures during the exhumation of the Annot sandstones formation. © 2015 Elsevier Ltd.


Kars M.,CNRS Laboratory of Thermodynamics and Energetics of Complex Fluids | Kars M.,Kochi University | Aubourg C.,CNRS Laboratory of Thermodynamics and Energetics of Complex Fluids | Labaume P.,Montpellier University | And 3 more authors.
Minerals | Year: 2014

The diagenetic evolution of the magnetic minerals during burial in sedimentary basins has been recently proposed. In this study, we provide new data from the Grès d’Annot basin, SE France. We analyze fine-grained clastic rocks that suffered a burial temperature from ~60 to >250 °C, i.e., covering oil and gas windows. Low temperature magnetic measurements (10–300 K), coupled with vitrinite reflectance data, aim at defining the magnetic mineral evolution through the burial history. Magnetite is documented throughout the entire studied transect. Goethite, probably occurring as nanoparticles, is found for a burial temperature <80 °C. Micron-sized pyrrhotite is highlighted for a burial temperature >200 °C below the Alpine nappes and the Penninic Front. A model of the evolution of the magnetic assemblage from 60 to >250 °C is proposed for clastic rocks, containing iron sulfides (pyrite) and organic matter. This work provides the grounds for a better understanding of the magnetic properties of petroleum plays. © 2014, by the authors; licensee MDPI, Basel, Switzerland.


Lilloe-Olsen T.,DNO International ASA | Bang N.A.,DNO International ASA
Oil and Gas Journal | Year: 2012

DNO International has become a prime explorer in the Kurdistan region of Iraq. The region was unexplored in 2004 when the Norwegian company became the first western enterprise in 3 decades to sign a production sharing contract there, seemingly an unlikely spot for the small, dynamic company to be setting up operations. DNO covers the entire spectrum, from exploration, to development, to production, a cohesive team that includes geology explorers, providing a solid base for work that brings together all aspects of the geology reservoir-production process. From a geologist's perspective, the geology and geological formations are nothing less than fascinating in this area of Kurdistan. Oil often leaks right to the surface, and at higher temperatures the oil become less viscous and may even create rivers of oil. Integral to DNO's success has been to gain the trust and respect of the local population.

Discover hidden collaborations