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<strong>Petroleum</strong> <strong>Geology</strong> <strong>of</strong> <strong>the</strong> <strong>Tyler</strong> <strong>Formation</strong><br />

(Pennsylvanian), <strong>North</strong> <strong>Dakota</strong><br />

T.O. Nesheim and S.H. Nordeng<br />

#16581<br />

33-053-02794-00-00<br />

Whiting Oil and Gas Corp.<br />

Curl 23-14


NDGS <strong>Tyler</strong> Publications within <strong>the</strong> Past Two Years:<br />

GI-127, GI-132, GI-144, GI-146, GI-148, GI-151, RI-111<br />

*Core Workshop at AAPG-RMS 2011


Spearfish <strong>Formation</strong><br />

Amsden <strong>Formation</strong><br />

<strong>Tyler</strong> <strong>Formation</strong><br />

Otter <strong>Formation</strong><br />

Madison Group<br />

Bakken-Three Forks fms.


Approximate Current<br />

Extent <strong>of</strong> Bakken-Three<br />

Forks Development Area


Basin Centered <strong>Petroleum</strong> System<br />

(Resource Play)<br />

• 1) Regionally extensive organic-rich source rock<br />

-Kerogen Type (Oil vs. Gas)<br />

• 2) Maturation <strong>of</strong> <strong>the</strong> source-rock (oil generation)<br />

• 3) Expulsion <strong>of</strong> generated oil from source rock<br />

• 4) Accumulation <strong>of</strong> expelled oil in adjacent rock<br />

• 5) Extraction <strong>of</strong> oil from <strong>the</strong> reservoir rock


Basin Centered <strong>Petroleum</strong> System<br />

(Resource Play)<br />

• 1) Regionally extensive organic-rich source rock<br />

-Kerogen Type (Oil vs. Gas)<br />

• 2) Maturation <strong>of</strong> <strong>the</strong> source-rock (oil generation)<br />

• 3) Expulsion <strong>of</strong> generated oil from source rock<br />

• 4) Accumulation <strong>of</strong> expelled oil in adjacent rock<br />

• 5) Extraction <strong>of</strong> oil from <strong>the</strong> reservoir rock


Williston Basin Source Rocks (Dow, 1974)<br />

Publication:<br />

Dow, W.G., 1974, Application <strong>of</strong> Oil –Correlation and Source-Rock Data to<br />

Exploration in Williston Basin: AAPG Bulletin, v. 58, no. 7, p. 1253-1262.


Amerada Petroluem Corporation<br />

Herman May U. #1 (NDIC: 291)<br />

Spud Date: 4/6/1953<br />

-First well drilled in Billings County<br />

-Produced from <strong>the</strong> Madison<br />

-Oil show in sandstone at 8,200-8,225 ft.


Amerada Petroluem Corporation<br />

Dan Cheadle Unit #1 (NDIC: 518)<br />

Spud Date: 12/30/1953<br />

-Produced from <strong>the</strong> “Heath” (<strong>Tyler</strong>) Pool<br />

-IP: 117 BBLS Oil & 3 BBLS Water<br />

-Cum Prod: 74,691 BBLS Oil & 13,156 BBLS Water


Dickinson-Fryburg Trend<br />

Cumulative <strong>Tyler</strong> Production<br />

285 wells → >84 million bbls. Oil = >294,000 bbls. oil per well


Example <strong>of</strong> a Productive <strong>Tyler</strong> Well<br />

Core<br />

Karsky-State #1<br />

Spud Date: 6/22/1967<br />

Field: Dickinson<br />

Cum. Oil: 1,711,142 BBLS<br />

Cum Gas: 61,485 MCF<br />

Cum. Water: 768,761 BBLS<br />

WBPC 2012 – Core Workshop


Production History <strong>of</strong> <strong>the</strong> <strong>Tyler</strong> <strong>Formation</strong><br />

2011 NDGS Geo Newsletter Vol. 38 No. 1


Area <strong>of</strong> next slide<br />

2011 NDGS Geo Newsletter Vol. 39 No. 1


Paleogeography Map <strong>of</strong> <strong>the</strong> <strong>Tyler</strong> <strong>Formation</strong> (J.H. Barwis, 1990)<br />

Dickinson-Fryburg Trend<br />

A<br />

A’


Lith<strong>of</strong>acies <strong>of</strong> <strong>the</strong> <strong>Tyler</strong> <strong>Formation</strong><br />

Publication: RI-111


Basin Centered <strong>Petroleum</strong> System<br />

(Resource Play)<br />

• 1) Regionally extensive organic-rich source rock<br />

-Kerogen Type (Oil vs. Gas)<br />

• 2) Maturation <strong>of</strong> <strong>the</strong> source-rock (oil generation)<br />

• 3) Expulsion <strong>of</strong> generated oil from source rock<br />

• 4) Accumulation <strong>of</strong> expelled oil in adjacent rock<br />

• 5) Extraction <strong>of</strong> oil from <strong>the</strong> reservoir rock


Free Oil/S1 + Reactive Kerogen/S2 (mg HC / g Sample)<br />

Previously Collected TOC and RockEval Core Data<br />

A Few Samples:<br />

“Excellent” quality source<br />

rocks w/ 6-12 wt. % TOC<br />

Most Samples:<br />

“Good” quality source<br />

rocks w/ 1-4. wt. % TOC<br />

Government Taylor A-1 (NDIC # 4627, SE¼<br />

SE¼, Sec. 9, T139N, R103W)<br />

Publication: GI-127<br />

State <strong>of</strong> <strong>North</strong> <strong>Dakota</strong> #41-36 (NDIC #:<br />

4789, NE¼ NE¼, Sec. 36, T137N, R100W)


Recently Collected TOC<br />

and RockEval Data<br />

30.2 wt. % TOC<br />

32.8 wt. % TOC<br />

Publication: GI-132


Total Organic Carbon Map <strong>of</strong> <strong>the</strong> <strong>Tyler</strong> Fm.<br />

Publication: GI-148<br />

TOC Map Notes:<br />

-Over 650 drill cuttins samples were analyzed<br />

for 54 wells for TOC wt. %.<br />

-Sampled drill cuttings, which were typically<br />

collected in 10 ft. intervals & sometimes 30 ft.<br />

-Samples were analyzed at Wea<strong>the</strong>rford Labs<br />

using <strong>the</strong> LECO TOC method.<br />

-The <strong>Tyler</strong> TOC map (left) depicts <strong>the</strong> average<br />

TOC wt. % <strong>of</strong> <strong>the</strong> entire <strong>Tyler</strong> section.


Publication: RI-111


Total Organic Carbon Map <strong>of</strong> <strong>the</strong> <strong>Tyler</strong> Fm.<br />

Publication: GI-148<br />

TOC Map Notes:<br />

-Sampled drill cuttings, which were typically<br />

collected in 10 ft. intervals & sometimes 30 ft.<br />

-Samples were analyzed at Wea<strong>the</strong>rford Labs<br />

using <strong>the</strong> LECO TOC method.<br />

-The <strong>Tyler</strong> TOC map (left) depicts <strong>the</strong> average<br />

TOC wt. % <strong>of</strong> <strong>the</strong> entire <strong>Tyler</strong> section.<br />

-Over 650 samples were analyzed for 54 wells<br />

with TOC wt. % varying from 0.03% to<br />

22.04%, average <strong>of</strong> 1.36%


#17430<br />

Publication: GI-151<br />

#11484


d<br />

c<br />

b<br />

a<br />

#17430<br />

Publication: GI-151<br />

#11484


<strong>Tyler</strong> <strong>Formation</strong> Source Rock Intervals<br />

d<br />

c<br />

b<br />

a<br />

Publication: GI-151


Total Organic Carbon Map <strong>of</strong> <strong>the</strong> <strong>Tyler</strong> Fm.<br />

Publication: GI-148<br />

TOC Map Notes:<br />

-Sampled drill cuttings, which were typically<br />

collected in 10 ft. intervals & sometimes 30 ft.<br />

-Samples were analyzed at Wea<strong>the</strong>rford Labs<br />

using <strong>the</strong> LECO TOC method.<br />

-The <strong>Tyler</strong> TOC map (left) depicts <strong>the</strong> average<br />

TOC wt. % <strong>of</strong> <strong>the</strong> entire <strong>Tyler</strong> section.<br />

-Over 650 samples were analyzed for 54 wells<br />

with TOC wt. % varying from 0.03% to<br />

22.04%, average <strong>of</strong> 1.36%


Basin Centered <strong>Petroleum</strong> System<br />

(Resource Play)<br />

• 1) Regionally extensive organic-rich source rock<br />

-Kerogen Type (Oil vs. Gas)<br />

• 2) Maturation <strong>of</strong> <strong>the</strong> source-rock (oil generation)<br />

• 3) Expulsion <strong>of</strong> generated oil from source rock<br />

• 4) Accumulation <strong>of</strong> expelled oil in adjacent rock<br />

• 5) Extraction <strong>of</strong> oil from <strong>the</strong> reservoir rock


Composite RockEval Data Set<br />

Publication: RI-111


Kerogen Type Based on TOC Content<br />

Organic-rich intervals in <strong>the</strong><br />

<strong>Tyler</strong> dominantly contain<br />

Type I/Type II Kerogen<br />

(prone to generating oil).<br />

There is a trend in <strong>the</strong> <strong>Tyler</strong><br />

that as organic carbon<br />

content declines <strong>the</strong><br />

hydrogen index also declines<br />

while <strong>the</strong> oxygen index<br />

increases<br />

Publication: RI-111


d<br />

c<br />

b<br />

a<br />

#17430<br />

Publication: GI-151<br />

#11484


Basin Centered <strong>Petroleum</strong> System<br />

(Resource Play)<br />

• 1) Regionally extensive organic-rich source rock<br />

-Kerogen Type (Oil vs. Gas)<br />

• 2) Maturation <strong>of</strong> <strong>the</strong> source-rock (oil generation)<br />

• 3) Expulsion <strong>of</strong> generated oil from source rock<br />

• 4) Accumulation <strong>of</strong> expelled oil in adjacent rock<br />

• 5) Extraction <strong>of</strong> oil from <strong>the</strong> reservoir rock


Thermal Maturation<br />

Publication: GI-148


Basin Centered <strong>Petroleum</strong> System<br />

(Resource Play)<br />

• 1) Regionally extensive organic-rich source rock<br />

-Kerogen Type (Oil vs. Gas)<br />

• 2) Maturation <strong>of</strong> <strong>the</strong> source-rock (oil generation)<br />

• 3) Expulsion <strong>of</strong> generated oil from source rock<br />

• 4) Accumulation <strong>of</strong> expelled oil in adjacent rock<br />

• 5) Extraction <strong>of</strong> oil from <strong>the</strong> reservoir rock


(Meissner, 1978)


Publication: GI-144


Basin Centered <strong>Petroleum</strong> System<br />

(Resource Play)<br />

• 1) Regionally extensive organic-rich source rock<br />

-Kerogen Type (Oil vs. Gas)<br />

• 2) Maturation <strong>of</strong> <strong>the</strong> source-rock (oil generation)<br />

• 3) Expulsion <strong>of</strong> generated oil from source rock<br />

• 4) Accumulation <strong>of</strong> expelled oil in adjacent rock<br />

• 5) Extraction <strong>of</strong> oil from <strong>the</strong> reservoir rock


Area <strong>of</strong> significant<br />

Bakken/Three Forks<br />

Production


Conclusions:<br />

1) The <strong>Tyler</strong> <strong>Formation</strong> contains organic-rich intervals consisting <strong>of</strong> Type<br />

I/Type II kerogen (excellent quality, oil-prone source rocks).<br />

2) TTI modeling and Tmax data indicate <strong>Tyler</strong> source rocks are <strong>the</strong>rmally<br />

mature and have undergone intense oil generation.<br />

3) Fluid overpressure in <strong>the</strong> <strong>Tyler</strong> Fm. fur<strong>the</strong>r indicates <strong>the</strong>rmally maturity<br />

<strong>of</strong> source rocks and that generated <strong>Tyler</strong> oil is still in place (minimal<br />

migration).<br />

4) Two separate petroleum systems exist within <strong>the</strong> <strong>Tyler</strong> <strong>Formation</strong>, a<br />

nor<strong>the</strong>rn petroleum system and a sou<strong>the</strong>rn petroleum system.<br />

5) The sou<strong>the</strong>rn <strong>Tyler</strong> petroleum system may extend beyond <strong>the</strong> current<br />

Bakken/Three Forks play.


Bakken <strong>Formation</strong><br />

<strong>Tyler</strong> <strong>Formation</strong><br />

“Everyone likes parfaits!”


References<br />

Barwis, J.H., 1990 Flood-Tidal Delta Reservoirs, Medora-Dickinson Trend, <strong>North</strong> <strong>Dakota</strong>, in Barwis, J.H., and o<strong>the</strong>rs, eds., Sandstone <strong>Petroleum</strong> Reservoirs:<br />

New York, Springer-Verlag, p. 389-412.<br />

Dow, W. G., 1974, Application <strong>of</strong> oil-correlation and source-rock data to exploration in Williston Basin, American Association <strong>of</strong> <strong>Petroleum</strong> Geologists Bulletin:<br />

V 58, p 1253-1262.<br />

Meissner, F.F., 1978, <strong>Petroleum</strong> geology <strong>of</strong> <strong>the</strong> Bakken <strong>Formation</strong> Williston Basin, <strong>North</strong> <strong>Dakota</strong> and Montana: in D. Rehig, ed., 1978 Williston Basin<br />

Symposium: Montana Geological Society, Billings, Montana, p. 207-227.<br />

Nesheim, T.O., and Nordeng, S.H, 2010, <strong>North</strong> to South Cross-Section <strong>of</strong> <strong>the</strong> <strong>Tyler</strong> <strong>Formation</strong> (Pennsylvanian) with RockEval Data, <strong>North</strong> <strong>Dakota</strong> , Geological<br />

Investigation No. 132, <strong>North</strong> <strong>Dakota</strong> Geological Survey.<br />

Nesheim, T.O., and Nordeng, S.H, 2011, Correlation <strong>of</strong> Fluid Overpressure and Hydrocarbon Presence in <strong>the</strong> <strong>Tyler</strong> <strong>Formation</strong>, Geological Investigation No.<br />

144, <strong>North</strong> <strong>Dakota</strong> Geological Survey.<br />

Nesheim, T.O., and Nordeng, S.H, 2012, Source Rock Intervals within <strong>the</strong> <strong>Tyler</strong> <strong>Formation</strong>, Geological Investigation No. 151, <strong>North</strong> <strong>Dakota</strong> Geological Survey.<br />

Nordeng, S.H. and Nesheim, T.O., 2010, Resource Potential <strong>of</strong> <strong>the</strong> <strong>Tyler</strong> <strong>Formation</strong>, Geological Investigation No. 127, <strong>North</strong> <strong>Dakota</strong> Geological Survey.<br />

Nordeng, S. H. and Nesheim, T. O., 2011, Determination <strong>of</strong> subsurface temperatures and <strong>the</strong> fraction <strong>of</strong> kerogen in <strong>the</strong> <strong>Tyler</strong> <strong>Formation</strong> that has converted to<br />

petroleum within <strong>the</strong> Rauch Shapiro Fee #21-9, Billings County, <strong>North</strong> <strong>Dakota</strong>, Geological Investigation No. 146, <strong>North</strong> <strong>Dakota</strong> Geological Survey.<br />

Nordeng, S.H. and Nesheim, T.O., 2012, A Preliminary Evaluation <strong>of</strong> <strong>the</strong> Resource Potential <strong>of</strong> <strong>the</strong> <strong>Tyler</strong> <strong>Formation</strong> (Penn.) Based on a Combination <strong>of</strong> a<br />

Kinetically Based Maturation Index, Organic Carbon Content & Interval Thickness, Geological Investigation No. 148, <strong>North</strong> <strong>Dakota</strong> Geological Survey.<br />

Passey, Q. R., Creaney, S., Kulla, J. B., Moretti, F. J., Stroud, J. D., 1990, A practical model for organic richness from porosity and resistivity logs: American<br />

Association <strong>of</strong> <strong>Petroleum</strong> Geologists Bulletin, v. 74, p. 1777-1794.


Thank you for your time.<br />

Questions???


Future Study<br />

Data to Collect: Cut several spatially distributed, complete cores <strong>of</strong> <strong>the</strong> <strong>Tyler</strong><br />

<strong>Formation</strong> for both <strong>the</strong> nor<strong>the</strong>rn and sou<strong>the</strong>rn petroleum systems. Benefit:<br />

Better understand <strong>the</strong> geology -> find potential horizontal targets that are<br />

laterally continuous.<br />

Data to Collect: Core analysis data (porosity, permeability, oil saturation % vs.<br />

water saturation %). Benefit: Figure out <strong>the</strong> vertical extent and distribution <strong>of</strong><br />

generated oil.<br />

Data to Collect: Wirelogs <strong>of</strong> <strong>the</strong> <strong>Tyler</strong> section (e.g. Neutron-Density Porosity,<br />

Sonic Travel Time, Gas Log-Chromatograph). Benefit: Geologic mapping <strong>of</strong><br />

source rocks and potential reservoirs. Log analysis techniques (e.g. Oil<br />

saturations).<br />

Data to Collect: Drill Stem Tests. Benefits: Test productive capability.


Oil Variations Between Source Rock Intervals<br />

Publication: GI-151


70-80% Oil Saturation<br />

Potential Horizontal Targets<br />

Interbedded Shale and Limestone


Maximum Shale Resistivity – Lower <strong>Tyler</strong><br />

Publication: GI-132


Maximum Shale Resistivity – Lower <strong>Tyler</strong><br />

c<br />

b<br />

a<br />

Publication: GI-132


Maximum Shale Resistivity – Lower <strong>Tyler</strong><br />

d<br />

Publication: GI-132


Publication: GI-151

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