17.02.2015 Views

overpressures role in generating and sealing shale gas ... - Cnr -cme

overpressures role in generating and sealing shale gas ... - Cnr -cme

overpressures role in generating and sealing shale gas ... - Cnr -cme

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

M.V.Batistatu<br />

OVERPRESSURES ROLE IN<br />

GENERATING AND SEALING SHALE<br />

GAS & WET SHALE ACCUMULATIONS


Overpressures Role <strong>in</strong> Generat<strong>in</strong>g <strong>and</strong><br />

Seal<strong>in</strong>g Shale Gas & Wet Shale Accumulations<br />

• Generat<strong>in</strong>g conditions:<br />

Pellitic lithology<br />

Anoxic environment<br />

Organic matter source/content<br />

Organic metamorphism<br />

Hydrocarbon generation<br />

Expel / seal processes<br />

Quantitative evaluation


Overpressures Role <strong>in</strong> Generat<strong>in</strong>g <strong>and</strong><br />

Seal<strong>in</strong>g Shale Gas & Wet Shale Accumulations<br />

Oil W<strong>in</strong>dow,<br />

Thermal Gas


Overpressures Role <strong>in</strong> Generat<strong>in</strong>g <strong>and</strong><br />

Seal<strong>in</strong>g Shale Gas & Wet Shale Accumulations


Overpressures Role <strong>in</strong> Generat<strong>in</strong>g <strong>and</strong> Seal<strong>in</strong>g<br />

Shale Gas & Wet Shale Accumulations<br />

• Overpressures generat<strong>in</strong>g processes<br />

1. Overburden effect<br />

2. Tectonic stresses<br />

3. Increases <strong>in</strong> fluid volume<br />

4. Osmosis<br />

5. Hydrostatic


Overpressures Role <strong>in</strong> Generat<strong>in</strong>g <strong>and</strong> Seal<strong>in</strong>g<br />

Shale Gas & Wet Shale Accumulations


Overpressures Role <strong>in</strong> Generat<strong>in</strong>g <strong>and</strong> Seal<strong>in</strong>g<br />

Shale Gas & Wet Shale Accumulations<br />

• Overpressured <strong>shale</strong>s effects:<br />

Layers limits impermeability<br />

Higher porosity<br />

Higher temperature<br />

Reactions/processes velocity<br />

Primary migration delay <strong>and</strong>/or stopp<strong>in</strong>g<br />

Low expell<strong>in</strong>g rate 10 to 15%<br />

<br />

Higher <strong>in</strong> situ (<strong>shale</strong>) hydrocarbon potential


Overpressures Role <strong>in</strong> Generat<strong>in</strong>g <strong>and</strong> Seal<strong>in</strong>g<br />

Shale Gas & Wet Shale Accumulations<br />

• Case study:


Overpressures Role <strong>in</strong> Generat<strong>in</strong>g <strong>and</strong> Seal<strong>in</strong>g<br />

Shale Gas & Wet Shale Accumulations


Overpressures Role <strong>in</strong> Generat<strong>in</strong>g <strong>and</strong> Seal<strong>in</strong>g<br />

Shale Gas & Wet Shale Accumulations


Overpressures Role <strong>in</strong> Generat<strong>in</strong>g <strong>and</strong> Seal<strong>in</strong>g<br />

Shale Gas & Wet Shale Accumulations<br />

Seismic<br />

cross section<br />

Eastern<br />

Carpathians<br />

Outer Flisch<br />

Zone


Overpressures Role <strong>in</strong> Generat<strong>in</strong>g <strong>and</strong> Seal<strong>in</strong>g<br />

Shale Gas & Wet Shale Accumulations<br />

• Filed conditions:<br />

• High pressures<br />

• Thrust tectonics<br />

• Compressional stress<br />

• Wet <strong>shale</strong> maturity<br />

• Significant depth<br />

• Salt seal


Overpressures Role <strong>in</strong> Generat<strong>in</strong>g <strong>and</strong> Seal<strong>in</strong>g<br />

Shale Gas & Wet Shale Accumulations<br />

• Conclusions:<br />

<br />

<br />

<br />

<br />

<br />

Overpressures affect <strong>in</strong> a significant manner the generat<strong>in</strong>g<br />

<strong>and</strong> expell<strong>in</strong>g processes for a shally formation<br />

Impermeable seals provided by rapid sedimentation&<br />

overload at the layers’ limits stop fluids expel from source<br />

rock<br />

Overpressure enable a faster chemical /thermal<br />

geochemical metamorphism thus the generation <strong>and</strong> even<br />

overmaturity of hydrocarbons is enhanced<br />

Many of source rock formations from Carpathians orogenic<br />

belt may represent favorable conditions for the existence of<br />

<strong>shale</strong> <strong>gas</strong> type accumulations<br />

Overpressured <strong>shale</strong> formations may represent an<br />

important doma<strong>in</strong> for <strong>shale</strong> <strong>gas</strong>& wet <strong>shale</strong> hydrocarbons<br />

accumulation


THANK YOU !

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!