Sns basin pp
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The document summarizes the Southern North Sea Basin located between England and the Netherlands. It discusses the basin's history of producing over 43 trillion cubic feet of gas from 123 gas fields. The tectonic setting involved a triple plate collision during the Caledonian orogeny, which initiated rift basins. The main petroleum system involves Carboniferous source rocks from equatorial swamps that charged Permian reservoirs effectively sealed by salt deposits. While well explored, the basin remains prospective for further hydrocarbon discoveries like the underexplored Dinantian Carbonate Play.
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Chapter 14new Notes
The document summarizes key topics about the ocean floor covered in Chapter 14, including the different regions of the ocean floor and features found in each region. It discusses features such as mid-ocean ridges, trenches, seamounts, guyots, continental shelves, slopes, and rises. It also covers types of seafloor sediments and resources that can be obtained from the seafloor like oil, natural gas, and minerals.
History
Over the past 600 million years, plate tectonics has caused continents to collide and break apart multiple times, forming different continental configurations. The most recent configuration was the supercontinent Pangea in the Permian period. Since then, Pangea has broken apart, with continents and fragments drifting to their current positions. Throughout this time, sea levels, temperatures, atmospheric composition and dominant life forms have varied in response to changing geological and environmental conditions.
History
Over the past 600 million years, plate tectonics has caused continents to collide and break apart multiple times, forming different continental configurations. The most recent configuration was the supercontinent Pangea in the Permian period. Since then, Pangea has broken apart, with continents and plates continuing to move and collide, opening and closing oceans. Mountain building, climate changes, and sea level fluctuations have occurred throughout this time in connection with these continental movements and collisions.
The Geology of the south Cardigan Bay coast.
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Assessment of Exploration Opportunities within the Taranaki Basin, New Zealand
Completed a technical assessment of the petroleum potential of the Taranaki Basin. Defined the key plays, petroleum systems, leads/prospects, and risks. Made recommendations on future exploration activity based on prevailing technical and economic conditions. Datasets were regional in scale, with 2D seismic and well data (e.g. petrophysical logs, cores, core analysis results, pressures, fluids, well tests).
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The Cambay Basin is an intracratonic rift graben located in northwest India that began forming following the Deccan Traps volcanic event in the late Cretaceous. The basin is filled with up to 8km of Tertiary sedimentary rocks. Major source rocks include the thick Cambay Shale deposited in the early Eocene during a transgression. Hydrocarbon reservoirs are found in the Olpad Formation, Hazad delta sands, and Miocene formations. Multiple petroleum plays exist, including those in the Paleocene-early Eocene, middle Eocene, and late Eocene-Oligocene sequences. The Cambay Shale is a prolific source of oil and gas in the
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The document discusses the origins and formations of various geological features including the Earth, petroleum and natural gas, coal, coral reefs, mountains, rivers, rocks, and oceans. It explains that the Earth originated from a single dense point that exploded outward, and petroleum and natural gas were formed from ancient organic materials compressed over long periods of time. Coal is formed through the decomposition and compaction of plant materials in swamps. Coral reefs are formed by coral secreting calcium carbonate skeletons in warm, clear waters. Mountains are formed through tectonic deformation of the Earth's crust. Rivers flow downhill from their source due to gravity and form river systems as tributaries join the main course. Rocks form through
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Sns basin pp
- 1. Southern North Sea Basin by Nabil Bin Idris SGI 140005 Powerpoint Templates Page 1
- 2. Powerpoint Templates Page 2 Outline • Location • History • Tectonic Setting • Evolution of the Basin • Petroleum Systems • Conclusions
- 3. Powerpoint Templates Page 3 Location Southern North Sea basin Lies between England and The Netherlands Gas producing basin UKCS,Geological Basins
- 4. Powerpoint Templates Page 4 History Southern North Sea Basin has produced around 43.4 trillion cubic feet (tcf) of gas from 123 gas fields by year end of 2009. Some 856 exploration and appraisal wells led to the discoveries of : Rotliegen play 8337 Mboe Triassic play 883 Mboe Carboniferous play 726 Mboe Exploration begin in 1960’s with the discovery of Groningen gas field
- 5. Powerpoint Templates Page 5 Tectonic Setting The North Sea was the site of a triple plate collision zone during the Caledonian orogeny The extension of Caledonian Orogeny initiated the rift basins Early Devonian saw extensional tectonic regime forming a series of graben Variscan Orogeny compression cause the inversion and erosion Rifiting reactivated in Triassic – Jurassic The inversion and erosion in Cretaceous – Teritary resulted in thining and onlap of the Chalk
- 6. Powerpoint Templates Page 6 Evolution of Basin Early Permian, NW Europe is a hot, barren landscape Ephemeral lakes become saline Dessert sand forms preserved the Carboniferous fern forests Salt précipitation formed as sea become saline Land emerged in Middle Jurassic and sand deposited along the coast Upper Jurassic, North Sea below sea level became rift zone Mudstone with algae content deposited followed by sand End Cretaceous white chalk deposited Erosional material deposited in North Sea Subsidence cause SR to depth forming o&g
- 7. Powerpoint Templates Page 7 Petroleum System The Carboniferous source rock comprise mostly Westphalian and some Namurian coals. The products of burial of the equatorial swamps of a foreland basin Permian sand become good reservoir due to thickness, porosity & permeability Effectively seal by Permian salt
- 8. Powerpoint Templates Page 8 Conclusion The southern North Sea is still unexplored for hydrocarbon play The Dinantian Carbonate Play has a huge potential for hydrocarbon
- 9. Powerpoint Templates Page 9 THANK YOU Q & A
- 10. Powerpoint Templates Page 9 THANK YOU Q & A