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Dynamic Earth
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Robert Gordon University 1
ENM200 Subsurface
Petroleum Geology:
Dynamic Earth
- An introduction to Geology and
Petroleum Geology for non-
geologists entering the Oil and Gas
Industry
Dr Bryan T Cronin ([email protected])
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Objectives of Petroleum Geology course
Half of Subsurface Module, ENM200
Academic lecturer: Dr Bryan Cronin
Petroleum Geology: 3 components:
- Our Dynamic Earth (5+ hours teaching)
- Petroleum Geology (5+ hours teaching)
- Online activities.
Assessed work half of the assessed work in this module will be on Petroleum Geology
Exam you will have to do two questions from the Petroleum Geology part of the module (which has three in total, 2 x Petroleum Geology and 1 x Formation Evaluation)
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Why study Petroleum Geology?
The processes of formation, accumulation and storage of hydrocarbons are all geological
Petroleum Geology: Finding OilReservoir Engineering, Well Engineering,
Production and facilities : Getting it out
Safety, the environment and decommissioning: Cleaning up during and afterwards
LECTURE 2
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Field Development: where does the geology come in?
1. Exploration: seismic character, external reservoir body geometry, seal and trap configuration, HC pathways
2. Appraisal: STOIIP (stock tank oil initially in place), rates of recovery, aquifer (size and pressure)?
3. Planning: Optimum depletion plan, Platform#? Well#?
4. Development: Injection and production, completions and workovers?
5. Management: Infills, workovers, enhanced recovery, reinjection, monitoring and surveillance
i.e. we need reservoir description a knowledge of the geology from the start (1), then the need intensifies (2), then a more complete picture is both
necessary and possible (3-5)
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Introduction to Petroleum Geology
1. Dynamic Earth (plate tectonics)
2. Crustal Composition (atoms-minerals-
rocks)
3. Geological time, correlation + maps
4. Rock Deformation and synthesis
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1. Our dynamic earth
An introduction to geology
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Global Earthquake Zones
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Global Volcano Zones
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50 Ma in the future ...
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2. Crustal Composition
From atoms to rocks
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Oil and Gas Reservoir Lithologies
Type Mineralogy Origin Main Porosity
Sandstone SiO2 Detrital Matrix
Limestone CaCO3 Biogenic Matrix
Chalk CaCO3 Biogenic Matrix
Dolomite MgCO3 Diagenetic Matrix/Fracture
Others Various Various Fracture
(Basement, shales, etc)
CA
RB
ON
AT
ES
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Robert Gordon University 41Halite planes and cleavage
Robert Gordon University 42Quartz crystal seen on SEM
Robert Gordon University 43Clay structure
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The Rock
Cycle
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Rock Cycle:
Graphic
Representation
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Weathering of different materials
Erodability
of minerals
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Ice-wedging
(Mechanical
Weathering)
Robert Gordon University 48Quartz Sandstone
(note matrix: no overgrowth)
Robert Gordon University 49Quartz in cordierite sillimanite gneiss
Robert Gordon University 50Clean sandstone under SEM
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Muscovite in Kyanite Schist, XPL, Shetland
minerals in an metamorphic rock
Robert Gordon University 52Zircons in Biotite, from Biotite-Kyanite Schist,
Ross of Mull, Scotland (PPL) can date the rock
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Zoned plagioclase crystal from Cornish Granite:
Igneous rock under the microscope
Robert Gordon University 54Bioclastic Sandstone
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Rock Textures
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Where are igneous rocks found?