Primary Workshop Objectives 1) Understand how oil and gas are formed, trapped, discovered and developed. 2) Become familiar with the disciplines and skills involved in finding and producing oil and gas. 3) Recognize the basic tools, equipment and processes used in finding, developing, producing and refining oil and gas. 4) Understand the industry language and terminology that you are likely to encounter. ©SCA, LLC 1 Petroleum Industry Process Overview 1. 2. 3. 4. 5. Basin Analysis (Global Exploration) Play Concepts Exploration Fairways Exploration Leads & Prospects Exploration & Appraisal Drilling ©SCA, LLC 2 INTRODUCTION • Basic Terminology • Global Consumption, Production & Reserves ©SCA, LLC 3 Natural Oil Seeps La Brea Tar Pits • Located in Los Angeles, California • Abundant plant & animal life preserved • Bacterial degradation alters the oil to asphalt (tar) and releases methane gas • Skeletons recovered include mammoths, dire wolves, bears, ground sloths, the saber-toothed cats and one human. • Oldest know organic material = 38,000 years ©SCA, LLC 4 Terminology: What is Petroleum? condensate) oil) • Petroleum: a natural yellow-to-black flammable liquid • hydrocarbon found beneath the earth’s surface Hydrocarbon: an organic compound made up of carbon and hydrogen atoms ©SCA, LLC 5 Terminology: Oil Gravity *API = American Petroleum Institute 50 45 40 35 API Gravity • Oil density is expressed in terms of API* gravity measured in degrees (example 40o) • API gravity is related to Specific Gravity, the weight of a volume of liquid divided by the weight of the same volume of water. • APIo >10 floats on water • APIo <10 sinks in water 30 25 Light Ghawar = 34o Prudhoe Bay = 28o Medium 20 15 WATER Heavy 10 Oil Sands = 8o 5 0 0.75 0.80 0.85 0.90 0.95 1.00 1.05 Specific Gravity APIo = 141.5/SG -131.5 ©SCA, LLC 6 Terminology: What is Natural Gas? • Natural gas is a mixture of hydrocarbons - primarily methane (CH4) but often including ethane, propane, butane and also impurities like water and CO2. • Natural gas occurs separately or in association with oil in a reservoir. • Methane, the simplest hydrocarbon containing one carbon and four hydrogen atoms, is colorless and odorless. ©SCA, LLC 7 Terminology: A Barrel of Oil The 42-gallon barrel originated in the 1860s when producers stored and transported petroleum in wooden barrels. ©SCA, LLC 8 Terminology: Oil Measurements symbol # of bbls bbl 1 MBO 1,000 MMBO 1,000,000 BBO 1,000,000,000 usage basic unit well production/day, small field reserves field reserves giant field reserves (>500mmbo) BOPD = Barrels of oil /day BOE = Barrels of Oil Equivalent (1 bbl = 5.6 mcfg) ©SCA, LLC 9 Terminology: A Cubic Foot of Gas • One cubic foot of natural gas has about 1031 Btus • One Btu (British Thermal Unit) is the heat required to raise the temperature of one pound of water one degree Fahrenheit. ©SCA, LLC 10 Terminology: Gas Measurement A typical home uses 100-150 mcfg/yr symbol # of ft3 MCF 1,000 MMCF 1,000,000 BCF 1,000,000,000 TCF 1,000,000,000,000 Usage basic unit well production/day field reserves giant field reserves MCFG/D = thousands of cubic feet of gas per day BOE = Barrels of Oil Equivalent (5.6 mcfg = 1 boe) ©SCA, LLC 11 Upstream, Midstream, & Downstream • The Upstream oil sector, also called the Exploration and Production (E&P) sector, is involved in the search for and recovery of crude oil and natural gas. • The Midstream sector refers to the processing, storage, marketing and transportation of crude oil, natural gas, and natural gas liquids such as ethane, propane and butane. • The Downstream sector, which includes oil refineries, petrochemical plants, petroleum product distribution, retail outlets and natural gas distribution companies, provides many common products such as gasoline, diesel, jet fuel, natural gas, and heating oil, plus asphalt, lubricants, synthetic rubber, plastics, fertilizers, pesticides, and pharmaceuticals. ©SCA, LLC 12 Transporting Petroleum Transporting Petroleum Transporting Petroleum Upstream Offshore Platform Oil Field Oil Field Midstream Pipeline Tanker Refinery Pipeline Consumers Tank Truck !"#$% Local Distributor Mobil Downstream Industrial Customers JMA Railroad Tank Cars after World Book Encyclopedia 24803 ©SCA, LLC 13 INTRODUCTION • Basic Terminology • Global Consumption, Production & Reserves ©SCA, LLC 14 Global Energy Consumption 1990 - 2035 555 EIA, International Energy Outlook 2010 ©SCA, LLC 15 Global Consumption by Region OECD: Organization for Economic Co-operation and Development (34 countries incl. US, Europe, S. Korea, Japan, Australia, etc!) ©SCA, LLC 16 Global Energy Consumption by Fuel Type ©SCA, LLC 17 Global Oil Production Top 10 !"##$%& ,%"-$&./%0$%& 2,& 4/%5& 89$5%& 8%5%-%& ;<=$>?& @<5<A"<B%& C"D%$E& 2.F& '()*+& '')1+& 1)3+& 6)7+& 6):+& 7):+& 3)1+& 3)3+& 3)(+& 3)'+& Global = 86.1 MMBO/D (2010 ave.) BP Statistical Review of World Energy, 2010 http://www.bp.com/statisticalreview ©SCA, LLC 18 Global Gas Production Top 10 2,& !"##$%& 8%5%-%& 4/%5& H?/D%I& 89$5%& J%E%/& .BK</$%& H<E9</B%5-#& 45-?5<#$%& BP Statistical Review of World Energy, 2010 http://www.bp.com/statisticalreview ©SCA, LLC '*)(+& '*):+& 6)'+& 7)G+& 3)7+& ()*+& ()*+& ()G+& ()6+& ()6+& 19 Global Oil Reserves Distribution Global proved oil reserves = 1.333 trillion bbls. BP Statistical Review of World Energy, 2010 http://www.bp.com/statisticalreview ©SCA, LLC 20 Global Gas Reserves Distribution Global proved gas reserves = 6,618 TCF (187.5 trillion cu. meters) BP Statistical Review of World Energy, 2010 http://www.bp.com/statisticalreview ©SCA, LLC 21 Billions of Barrels of Oil Equivalent Prud h oe Bay, Alaska, USA Faro o zan-Marjan, Saud i Arabia/Iran The World’s Biggest Fields Man ifa, Saud i Arabia Zakum, Abu Dh abi, UAE Ch icontepec, Mexico Berri, Saud i Arabia Abq aiq , Saud i Arabia Kash ag an, Kazakstan Ro mash kino, Vo lga-Ural, Russia Marlim, Camp os, Brazil Ag h ajari, Iran Gach saran, Iran Samo tlo r, West Siberia, Russia Marun , Iran Kirkuk, Iraq Ah waz, Iran Rumaila, Iraq Ten g iz, Kazakstan Safan iya-Khafji, Saud i Arabia/Neutral Zone Bo livar Coastal, Ven ezuela Burg an , Kuwait Gh awar, Saud i Arabia 0 50 100 ©SCA, LLC 22 The World’s Giant Fields Authors: Mann, P., M.K. Horn, I. Cross. ©SCA, LLC 23 Peak Oil • The point in time when the maximum rate of global oil production is reached. • Following Peak Oil, the rate of production enters terminal decline. • Peak oil is not the time at which the world runs out of oil, but the point at which global production begins steady decline. • M. King Hubbert developed this theory in 1956 and accurately predicted that US oil production would peak between 1965 and 1970. ©SCA, LLC 24 Global Oil Production Forecasts http://www.theoildrum.com/story/2006/11/13/225447/79 ©SCA, LLC 25 World’s Biggest Oil Companies “BIG OIL” Based on reserves Source: Oil & Gas Journal, 9/6/2010 ©SCA, LLC 26 INTRODUCTION • Basic Terminology • Global Consumption, Production & Reserves ©SCA, LLC 27 Geology • • • • • Introduction to Geologic Age Plate Tectonics Rock Types and Reservoirs Types of Petroleum Traps Mapping ©SCA, LLC ‹#› Introduction to Geologic Age Fathers of Modern Geology The earth is very old. James Hutton 1726-1797 ©SCA, LLC ‹#› Principle of Original Horizontality ,E/%LM>%L?5&D%#&?/$K$5%BBI&9?/$A?5E%B&0<>%"#<&#<-$N<5E%/I& O%/L>B<#&#<PB<&Q/?N&R"$-#&"5-</&E9<&$5R"<5><&?Q&K/%S$EI)&& Cliffs of Moher, Ireland ©SCA, LLC ‹#› Principle of Superposition 45&%5I&#">><##$?5&?Q&/?>T&B%I</#U&E9<&?B-<#E&B$<#&%E&E9<& 0?P?N&D$E9&#">><##$S<BI&I?"5K</&&B%I</#&BI$5K&%0?S<)&& Younger Younger Older Erosion Deposition Sea Level This is the basis for determining the relative ages of all strata and their contained fossils. ©SCA, LLC ‹#› Geologic Age ,E/%LM>%L?5&E9%E&D%#&?/$K$5%BBI&9?/$A?5E%B&%5-&$#&5?D& $5>B$5<-&?/&Q?B-<-&N"#E&9%S<&#"V</<-&WE<>E?5$>X&-$#E"/0%5><& ?S</&K/<%E&O</$?-#&?Q&LN<&#"0#<Y"<5E&E?&-<O?#$L?5)& Siccar Point (Scotland) where Hutton observed in 1788 that 345 million year old rocks unconformably overlie 425 million year old rocks. ©SCA, LLC ‹#› Fathers of Modern Geology Faunal Succession William Smith 1769-1839 Fossils are found in a sequence progressing from older to younger, and that sequence can be found in rocks elsewhere, indicating correlation between locations. ©SCA, LLC ‹#› Faunal Succession • Fossilized plants and animals contained in sedimentary rock layers succeed each other in time, with younger layers lying on top of (shallower than) older layers. • The vertical sequence of fossils occurs in a specific order that allows sedimentary rocks to be dated and correlated across and between continents. Example: A fossilized mammoth tusk will never occur in the same sedimentary rock formation as a Tyranosaurus Rex bone because the two lived millions of years apart. 65,000,000 years old 150,000 years old ©SCA, LLC ‹#› Geologic Age Proterozoic Stromatolites (600 MYBP) Silurian Ammonites (425 MYBP) Cretaceous shark teeth (100 MYBP) Eocene fossil fish (50 MYBP) ©SCA, LLC ‹#› Please do not turn the page ©SCA, LLC ‹#› Geologic Age 1st occurrence earth's origin Yrs BP Annual Equivalent 4.7 Billion 1-Jan bacteria 3.5 Billion 3-Apr dinosaurs 250 Million 12-Dec Greeks, Romans 2 Thousand 31 Dec, 11:59:47 PM ©SCA, LLC ‹#› Geologic Age 1st Occurrence Yrs BP Annual Equivalent earth's origin 4.7 Billion 1-Jan bacteria 3.5 Billion 3-Apr algae, protozoa 1.5 Billion 6-Sep fungi 1.0 Billion 14-Oct sponge 700 Million 7-Nov jellyfish 650 Million 11-Nov worms, clams 570 Million 17-Nov fish 500 Million 22-Nov sharks/insects 390 Million 1-Dec amphibians 350 Million 4-Dec reptiles 300 Million 8-Dec dinosaurs 250 Million 12-Dec mammals 200 Million 15-Dec Neanderthals 200 Thousand 31-Dec (11:38:00 PM) people 100 Thousand 31-Dec (11:49:00 PM) Greeks, Romans 2 Thousand 31-Dec (11:59:47 PM) 1st land plants ~470 mm yrs. BP 1st land animals ~450 mm yrs. BP ©SCA, LLC 38 Geologic Age Methods for age dating and correlating rocks include: fossils, stable isotopes, paleomagnetics, and sedimentary cycles. ©SCA, LLC ‹#› Biostratigraphy: Trilobites 300 million years ©SCA, LLC ‹#› Trilobite Fossils !"#$%#&'()#*+$+,*-%,+(( .#/0,%+,(+1#(( 23456375()%88%0,(9:&;(<#=0:#(":#&#,*>(( ?*8+&()0@,*+%,&A()0:0$$0( ©SCA, LLC ‹#› Geoscience • • • • • Introduction to Geologic Age Plate Tectonics Rock Types and Reservoirs Types of Petroleum Traps Mapping BC.DE( ©SCA, LLC ‹#› Plate Tectonics& • Z9<&T<I&O/$5>$OB<&?Q&OB%E<&E<>E?5$>#&$#&E9%E&E9<&B$E9?#O9</<&<=$#E#&%#&#<O%/%E<&%5-& -$#L5>E&!"#!$%&#'()*!"+U&D9$>9&/$-<&?5&E9<&R"$-[B$T<&WS$#>?[<B%#L>&#?B$-X& %#E9<5?#O9</<)&& • .BE9?"K9&#?B$-U&E9<&%#E9<5?#O9</<&9%#&/<B%LS<BI&B?D&S$#>?#$EI&%5-&#9<%/&#E/<5KE9& %5-&>%5&R?D&B$T<&%&B$Y"$-&?5&K<?B?K$>%B&LN<&#>%B<#& Plate Tectonics Types of plate boundaries ©SCA, LLC ‹#› Plate Tectonics Earthquakes (yellow), Volcanoes (red) and Plate Boundaries (blue) ©SCA, LLC ‹#› The San Andreas Fault The San Andreas Fault is the Boundary between the North American Plate and the Pacific Plate USGS graphic These plates are moving past one another at a rate of about one inch per year. ©SCA, LLC ‹#› Plate Tectonics 140 million years ago ©SCA, LLC ‹#› Plate Tectonics& • ?"F+,6?8<%+,(#+:89(G( • H:#6I#,0J+,%+,6 K0@:0,%+,(!0@:$#( L0$M(.#"0&%F0,&& Plate Tectonics Modeling of tectonic plate movements helps geoscientists predict the location and dimensions of sedimentary basins capable of containing hydrocarbon accumulations. 75 million years ago ©SCA, LLC ‹#› • I+J"+,%+,(N4O()+(P( Q+*#(G( • H0&*(I#,0J+,%+,6 K0@:0,%+,(!0@:$#( L0$M(.#"0&%F0,&& Plate Tectonics& Plate Tectonics Mid Ocean Ridge & Sea Floor Spreading ©SCA, LLC ‹#› Plate Tectonics & Plate Tectonics The locations of certain fossil plants and animals on present-day, widely separated continents form definite patterns. & Geology • • • • • Introduction to geologic age Plate tectonics Rock types and reservoirs Types of petroleum traps Mapping ©SCA, LLC ‹#› Hydrocarbon Reservoirs Hydrocarbons Exist in a Reservoir ©SCA, LLC ‹#› Sandstones • A sedimentary (clastic) rock deposited by water or wind erosion and composed of cemented, sand-sized mineral grains. • Most sanstones are composed of quartz and feldspar; the most common minerals in the earth’s crust. • Deposition occurs when the sand grains settle from suspension in water, such as when a river enters an ocean. • Cementation occurs with burial and compaction along with the precipitation of minerals within the pore spaces between sand grains. ©SCA, LLC ‹#› Sandstone ©SCA, LLC ‹#› Sandstone Reservoirs Pore space Sand Grains Permeability Good Porosity = Lots of Space for Oil & Gas ©SCA, LLC 58 Hydrocarbon Reservoirs Porosity Gas/ Oil Contact Oil/ Water Contact Sand Grain ©SCA, LLC ‹#›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`&H?/N%/TU& '*_1`&]&a%BT</U&'*_1X)& ©SCA, LLC ‹#› Oil Sands • Oil Sands, sometimes called Tar Sands, are generally loosely consolidated sandstone formations saturated with highly viscous crude oil. • The oil is “heavy” or tar-like because the lighter fractions of the oil have been lost, and the remaining fractions have been bio-degraded by bacteria. • Not the same as “oil shale” ©SCA, LLC ‹#› Oil Sands Canada’s Alberta oil sands deposits cover 54,000 square miles, an area larger than the state of Florida, and hold an estimated 175 billion barrels of crude oil. Tar Sands Open Pit Mining Alberta, Canada Photograph: Suncor Energy It takes two tons of tar sands (4,410 lbs.) to make one barrel of oil Athabasca Oil Sands ©SCA, LLC ‹#› Why are Oil Sands important? • Approximately 2/3 of the world's total crude oil resources are estimated to exist in oils sands. • Canada and Venezuela are estimated to have 1.7 trillion barrels and 1.8 trillion barrels of oil sands related crude respectively • Conventional oil resources remaining worldwide (mostly in the Middle East) are estimated to total 1.75 trillion barrels. ©SCA, LLC ‹#› Unconventional or Resource Plays Conventional Reservoirs • can be produced at economic flow rates • will produce economic volumes of oil and gas • do not require massive stimulation treatments, special recovery processes or leadingedge technology. Unconventional Reservoirs • cannot be produced at economic flow rates • do not produce economic volumes of oil and gas without assistance from massive stimulation treatments or special recovery processes and technologies ©SCA, LLC ‹#› Unconventional or Resource Plays: Shale Oil and Shale Gas • Oil Shale is a source rock, reducing the risk of finding hydrocarbons. • Shales have low permeability and do not naturally produce hydrocarbons at commercial rates. • Shale reservoirs require high organic content, brittle lithology and natural or man-made fractures. • Hydraulic fracturing (made-made reservoir fractures) and horizontal drilling (increasing well bore exposure to the reservoir and natural fractures) make “unconventional” shale formations commercial. ©SCA, LLC ‹#› Shale Gas - US& Technically Recoverable Shale Gas Resources ! 482 trillion ft3 ©SCA, LLC ‹#› Shale Gas - US& After The Gold Rush: A Perspective on Future U.S. Natural Gas Supply and Price Posted on The Oil Drum by A. Berman February 8, 2012 ©SCA, LLC ‹#› Shale Gas Plays – Fractured Reservoirs Conventional Core from Marcellus Shale Reservoir ©SCA, LLC ‹#› Shale Gas Plays – Fractured Reservoirs ©SCA, LLC ‹#› Shale Gas Plays - Global& Technically Recoverable Shale Gas Resources ! 48 shale gas basins ! 32 countries ! ~70 shale gas formations ! Global (excl. US) = 5,760 trillion ft3 ! Global + US = 6,622 trillion ft3 EIA World Shale Gas Resources Report: April 2011 Global Proved Reserves ~6,609 trillion ft3 (January 1, 2010) ©SCA, LLC ‹#› Geoscience • • • • • Introduction to Geologic Age Plate Tectonics Rock Types and Reservoirs Types of Petroleum Traps Mapping ©SCA, LLC ‹#› Trap Types: Structural Traps • Structural traps form when potential reservoir formations are deformed by tectonic movement or faulting. • Typical structural traps include anticlines, folds, salt domes and faults. • Structural traps are the most common types of trapping mechanism because they are easier to identify than other trap types, sometimes visible at the earth’s surface. ©SCA, LLC ‹#› Fault Traps: Normal Fault Normal Fault ©SCA, LLC ‹#› Fault Traps: Normal Fault ©SCA, LLC ‹#› Fault Traps: Growth Faults ©SCA, LLC ‹#› Fold Traps: (Anticlines or 4-way Closures) Gas Oil Water ©SCA, LLC ‹#› Salt Dome Trapping Mechanism ©SCA, LLC ‹#› Avery Island Salt Dome Surface expression of a buried salt feature ©SCA, LLC ‹#› Trap Types: Stratigraphic Traps • Stratigraphic traps occur when the reservoir formation is sealed by surrounding, impermeable formations. • Trapping may occur due to lateral changes in the reservoir formation itself, called perm barriers or pinchouts. • Sedimentary features such as reefs (carbonates) also form stratigraphic traps. http://www.wsgs.uwyo.edu/Topics/WYEconomics/Economics-Fluids.aspx ©SCA, LLC ‹#› Carbonate Traps • Carbonate formations, commonly limestone, dolomite and chalk, consist primarily of calcite and its derivatives which form by the activity of marine organisms such as coral and algae. • Carbonate rocks can be clastic in origin, formed from the eroded by-products of coral reefs. • Carbonate rocks can be good reservoirs due to the formation of porosity by dissolution. • Their brittle nature lends itself to fracturing, which provides reservoir permeability. ©SCA, LLC ‹#› Carbonates: Modern Analog Grand Bahamas Bank (Carbonate Factory) Reef Front Deep Water Island of Eleuthera (Bahamas) ©SCA, LLC ‹#› Carbonates: Modern Analogs ©SCA, LLC ‹#› Carbonate Reefs on Seismic Data Carbonate Reef Porosity ©SCA, LLC ‹#› Carbonates: Ghawar Field World’s Largest Oil & Gas Field • Jurassic limestone deposited on a continental shelf • Exposed in tidal zone • Converted to Dolomite • Volume reduction results in large porosity increase • April ‘10 reserves: 65+ BBO produced, EUR = 100+ BBO ?":%8(ZO5O(:#&#:/#&'(( • (Y[\(]]E(":0R@$#R( • (5OO\(]]E(D^L( Current daily production Oil gas 5 million bbls 2 billion feet3 ©SCA, LLC ‹#› Geology • • • • • Introduction to Geologic Age Plate Tectonics Rock Types and Reservoirs Types of Petroleum Traps Mapping ©SCA, LLC ‹#› Mapping: Topographic Contour Maps A line on a map that represents a constant value of the data being mapped is called a contour line. The structure map is like a surface topographic map drawn on an underground formation. ©SCA, LLC ‹#› Mapping: Structure Maps -2500 -4,000 -1150 -1000 -2000 -3000 -4000 -5000 -6000 -7000 -8000 1 Mile ©SCA, LLC ‹#› Interpretive Contouring -10,140 m-10,137 -10,120 -10,120 m m-10,123 m m -10,142 m-10,124 -10,104 m-10,125 N m-10,118 m-10,086 m-10,104 m -10,101 m-10,098 m-10,103 -10,120 Structure Map (Depth) XYZ Formation Top 1000 ft -10,140 Contour Interval = 10 feet ©SCA, LLC ‹#› Interpretive Contouring ©SCA, LLC ‹#› Interpretive Contouring - Faults ©SCA, LLC ‹#› Geology • • • • • Introduction to Geologic Age Plate Tectonics Rock Types and Reservoirs Types of Petroleum Traps Mapping ©SCA, LLC ‹#› Please do not turn the page ©SCA, LLC ‹#› _#0801%$(?1#( e5<&I<%/&f8B?>Tg& earth's origin 4.7 Billion 1-Jan bacteria 3.5 Billion 3-Apr algae, protozoa 1.5 Billion 6-Sep fungi 1.0 Billion b/<[& 14-Oct 8%N0/$%5& sponge 700 Million 7-Nov jellyfish 650 Million 11-Nov worms, clams 570 Million 17-Nov Fish 500 Million 8%N0/$%5& sharks/insects 390 Million c<S?5$%5& 1-Dec amphibians 350 Million reptiles 300 Million 4-Dec 8%/0?5$Q</?"#& 8-Dec dinosaurs 250 Million Z/$%##$>& 12-Dec mammals 200 Million d"/%##$>& 15-Dec Neandertals 200 Thousand bB<$#E?><5<& 31-Dec (11:38:00 PM) people 100 Thousand 31-Dec (11:49:00 PM) Greeks, Romans 2 Thousand 31-Dec (11:59:47 PM) 22-Nov Exploration • • • • Sedimentary Basins Generation of Oil and Gas Regional Geology Leases, Licenses and PSA’s ©SCA, LLC 94 Sedimentary Basin • A depression in the Earth’s crust, caused by plate tectonic activity in which erosional products such as sand and silt (sediments) accumulate. • Sedimentary basins are the starting point for the exploration process. ©SCA, LLC 95 The Gulf of Mexico Basin Basin formed ~200 million years ago. Salt deposited ~150 million years ago. Area: 615,000 mi2 (1.6 million km") Water depth: 14,383 ft., 2.7mi. or (4,384 m) deep in the Sigsbee Trough 32,000+ feet of sedimentary fill, through present day ©SCA, LLC 96 Basin Sedimentary Deposition Houston Gulf of Mexico Yucatan Peninsula ©SCA, LLC 97 North America Sedimentary Basins ©SCA, LLC 98 North America Sedimentary Basins 75-100 million years ago The Western Interior or Cretaceous Seaway ©SCA, LLC 99 Sedimentary Basins • As basins form they are filled with sediments such as sand and silt, generally transported into the basin by rivers. • The increasing weight of the sediment fill causes the basin to subside further allowing for the influx of additional sediments. • As the sediments are buried, they are subjected to increasing pressure and become lithified to form sandstone and shale. • Basin subsidence can continue for millions of years, resulting thousands of feet/kilometers of sediment thickness. • Under the proper conditions, a petroleum system may form. ©SCA, LLC 100 Exploration • • • • Sedimentary Basins Generation of Oil and Gas Regional Geology Leases, Licenses and PSA’s ©SCA, LLC 101 Generation of Oil and Gas • Crude oil and natural gas result from organic materials that are buried with fine grained sediments to form shale or source rocks. • The organic materials are vast quantities of microscopic plants and animals such as algae and plankton (not dinosaurs). • With increasing depth of burial, the organic matter is exposed to pressure and temperatures that cause a chemical reaction resulting in the formation of liquid and gaseous hydrocarbons. • The depth at which these changes occur is called the “oil window”. • With greater depth, oil undergoes thermal cracking (similar to refining) and is converted into natural gas. ©SCA, LLC 102 Generation of Oil and Gas Increasing Temperature w/ Depth degrees F 0 100 200 300 400 Increasing Pressure w/ Depth 500 0 PSI 0 930 1,860 2,790 3,720 4,650 5,580 6,510 7,440 8,370 9,300 10,230 11,160 12,090 13,020 13,950 14,880 5,000 0 15,000 5000 20,000 10000 25,000 30,000 35,000 Temperature increases @ ~15 degrees F/ft. depth/feet depth/feet 10,000 15000 20000 25000 30000 Pressure increases @ ~0.465 psi/ft. 35000 ©SCA, LLC 103 Please do not turn the page ©SCA, LLC ‹#› The Petroleum System The combination of geologic processes that result in the generation, migration, trapping and preservation of hydrocarbons in the subsurface is called the Petroleum System (“basin plumbing”). • Generation: formation of hydrocarbons in the source rocks. • Migration: movement of the generated hydrocarbons from the source to the reservoir formations. • Accumulation: sealing and trapping of the migrating hydrocarbons in the reservoir. • Preservation: preservation of the trapped hydrocarbons in the reservoir to the present day ©SCA, LLC 105 !"#$%&"'()*+,#"(,) Sea Level Sea Floor _+&(I+"( `;(IQE!^LD( Pressure & Temperature E%8(Q#1( Gas/Oil Contact Increasing c+*#:(Q#1( Oil/Water Contact 5`O0(X(a(YO0(I( Oil Window 3[O0(X(a(5b[0(I( Generation a9</<&D%#&^$0</$%&D9<5&!$h$5K&0<K%5i& a9I&$#&E9%E&$NO?/E%5Ei& Petroleum System& • ?"F+,6?8<%+,( • H:#6I#,0J+,%+,6 K0@:0,%+,(!0@:$#( L0$M(.#"0&%F0,&& Petroleum System Adequate column, closure?& Location map of 1981-82 Ivory Coast 3-D seismic survey showing structure of Albian unconformity. Contours in meters.& In-line 525 crossing A-1X well location, Espoir field, IVORY COAST showing clear definition of rotated fault block beneath Albian unconformity. & _#,#:+F0,A()%1:+F0,A(?$$@J@8+F0,d( • • !0@:$#(L0$M(K9"#A()+*@:%*9A(.#"*-A(K#J"#:+*@:#A(]@:%+8( e%&*0:9( )%1:+F0,(H+*-T+9&d(X+@8*&A(@,$0,=0:J%*9(&@:=+$#d( H:#&#:/+F0,d( • • • X+@8*(f@g*+"0&%F0,(0=(:#&#:/0%:(*0(&#+8(+$:0&&(=+@8*d( X+@8*(FJ%,16(":#a"0&*6J%1:+F0,d( K0"(!#+8d( Petroleum System& Petroleum System Adequate quality & quantity of Source Rock?& Petroleum System Adequate quality, quantity of Source Rock?& Petroleum System Adequate Quality & Quantity of Source Rock?& Petroleum System Adequate quality, quantity of Source Rock?& Petroleum System Adequate quality, quantity of Source Rock?& !%#::+(Q#0,#( !%#::+(Q#0,#( !%#::+(Q#0,#( 8?5K?& 8?5K?& 8?5K?& 8?5K?& Natural Oil Seeps Coal Oil Point seep field: • Located offshore California near Santa Barbara • Oil seepage averages 130-150 barrels of oil per day • 55,000 barrels of oil per year • Seeps in this area are well documented by early explorers and coast-dwelling Chumash Indians. ©SCA, LLC 125 Petroleum Systems Sea Level Sea Floor Gas Cap Increasing TRAP Pressure & Temperature Oil Leg Gas/Oil Contact Water Leg Oil/Water Contact 140o F / 60o C Oil Window 350o F / 175o C GENERATION ©SCA, LLC 126 Prospect Risking& factor justification Source 1.00 oil is present in nearby fields Migration 1.00 oil is present in correlative formation nearby Reservoir 0.75 seismic character is similar to productive interval nearby Trap 0.25 faults extend into younger section, possible breach Seal 0.95 formation is overlain by thick shale total 0.18 = 1 in 5.6 Exploration Prospect Risk 2. Commercial Risk • Reserve size • Reservoir productivity • Product price • Commercial Terms !$#T&$#&E9<&>9%5><&?Q&Q%$B"/<)&25></E%$5EI&/<Q</#&E?&E9<&/%5K<& %5-&S%/$%5><&Q?/&%5I&$5O"E&?/&?"EO"E&O%/%N<E</& High Develop 3. Reserves Uncertainty Mid • Reservoir area • Pay thickness • Reservoir quality • Recovery factor Discovery Low Decision To Drill 1. Discovery Risk • Source • Migration • Reservoir • Closure • Containment High SubCommercial Hold/Reevaluate Mid Low Sell/Trade/ Farm-out / Abandon Failure Note: Risk AAPG Imperial Barrel Training Course – October 9, 2010 = Uncertainty ©SCA, LLC 26 & Please do not turn the page ©SCA, LLC ‹#› Exploration • • • • • • Sedimentary Basins Generation of Oil and Gas Regional Geology Field Geology, Surface Mapping, and Aerial Photos Exploration Risk Leases, Licenses and PSA’s ©SCA, LLC 130 The Exploration Process Exploration License Paleogeography (Basins) source reservoir migration trap Regional Geology Exploration Leads & Prospects Exploration Plays ©SCA, LLC 131 The Exploration Process Source: API - Offshore Access to Oil & Natural Gas Resources ©SCA, LLC 132 Exploration Terms • Play: a geographic area containing prospects with common stratigraphic and/or structural characteristics, or a generic geologic setting or play type such as a sub-salt play. • Lead: an exploration opportunity that demonstrates the basic characteristics of a hydrocarbon trap including reservoir rock, trapping mechanism, surrounding formation seals, and a likely pathway to the source rock. • Prospect: a lead that has been sufficiently analyzed to establish a reasonable probability of finding commercial hydrocarbons. • Drill-Ready: A prospect on which leasing, permitting, budgeting, etc !. are complete. ©SCA, LLC 133 Gulf of Mexico Sub Salt Play ©SCA, LLC 134 Sub Salt Play ©SCA, LLC 135 Sub Salt vs. Pre-Salt Plays ©SCA, LLC 136 Exploration Play Types Sometimes a play is defined by common technology requirements such as: Deep Water Play: Exploration activity located in offshore areas where water depths exceed approximately 1,000 feet (305 m), requiring advanced drilling and production technology. Deep water targets can be geologically similar to targets drilled in shallow water or onshore. Horizontal Play: Drilling a well vertically from the surface to a subsurface location just above the target reservoir, then deviating the well from a “kickoff point” to penetrate the objective reservoir horizontally and remaining within the reservoir to the desired bottom hole location. ©SCA, LLC 137 Please do not turn the page ©SCA, LLC ‹#›