Earths Structure
1 - Solid inner iron core 2 - Liquid outer iron core 3 - Lower Mantle 4 - Transition Zone 5 - Asthenosphere 6 - Lithosphere 7 - Crust
Rock Types
Igneous - Crystallisation of molten material
Metamorphic - Recrystallisation of older rocks
Sedimentary - Formed by accumulation of particles as sediments, followed by burial and compaction. Majority of hydrocarbon accumulations.
Stratigraphy
Sediments accumulated in layers over time. Layers analysed.
Geological Structures
Sedimentary rocks are deformed over time by the stress strain caused during burial or during plate tectonics.
Petroleum Play
Determine where hydrocarbons are likely to occur.
Considerations - Rock (source, maturity, reservoir and seal) migration (primary, secondary, timing)