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Deepening the Frontier-Porosity Preservation in Deeply Buried (28,000 Feet) Mudstones of the Vienna Basin, Austria


The Vienna Basin is a Neogene pull-apart basin which is situated between the Eastern Alps to the West, the Carpathians to the North-East and the Pannonian Basin to the East. Its principal source rock for oil and gas are Malmian mudstones of the Mikulov Formation. We examined core samples provided by OMV Previous HitfromNext Hit this unit that were recovered Previous HitfromNext Hit depths of 26,800 to 28,060 feet, and studied their microfabrics in argon ion milled samples with a FEI Quanta 400 FEG scanning electron microscope, and quantified their mineralogy with X-ray Previous HitdiffractionNext Hit (XRD). XRD analysis shows that the main components of bulk samples are quartz, calcite and clay, and also reveals minor amounts of ankerite, plagioclase and pyrite. The clay mineralogy of these deep samples was quantified with X-ray Previous HitdiffractionNext Hit through application of the mineral intensity factor (MIF)-method of Moore and Reynolds (1997). The clay fraction of the deep mudstones contains 17-28% illite/smectite (I/S) mixed-layer mineral, 63-70% illite and 9-13% chlorite. R3 ordering with 90% illite in I/S prevails at these great depths. Illite crystallinity was determined using standards Previous HitfromNext Hit Warr and Rice (1994), and increases with temperature and depth. The samples at 28,000 feet depth have not yet reached the anchizone. Whereas we did not expect to find preserved porosity in samples Previous HitfromNext Hit such depths, we nonetheless found significant porosity and a variety of pore types of nanometer to micrometer size range. Although the fabric appears tightly cemented and packed at low magnification, phyllosilicate framework pores up to 2 μm are common in interstitial areas between harder grains, and are in places held open because of “clamping” of phyllosilicate platelets by diagenetic cements. Carbonate framework pores of similar size occur in early diagenetically cemented areas. In addition, the margins of calcite grains have in places undergone partial dissolution (probably due to organic acid production during late diagenesis), leading to pores in the 100 nm to 1 μm size range. Organic matter occurs as two broad categories, amorphous and structured. The latter lacks pore development, whereas the former occurs interstitially between other minerals and shows well developed OM-pores (10-500 nm). Overall, these observations suggest that there is a potential to produce gas Previous HitfromTop very deeply buried mudstones.