Petroleum Geology Conference

Slides:



Advertisements
Similar presentations
Overview of Seismic Interpretation
Advertisements

Geology of the Thaumasia region, Mars: plateau development, valley origins, and magmatic evolution by James M. Dohm, Kenneth L. Tanaka.
Bathymetry, Gravity and Magnetic Images of the Mediterranean water of the Nile Delta, Egypt, using GIS Technique, Part IV Interpretation of Gravity Data.
The Structural and Geodynamic Evolution of the Black Sea Basin Stuart Egan & David Meredith The Structural and Geodynamic Evolution of the Black Sea Basin.
Kazuya Fujita Department of Geological Sciences
Phanerozoic Tectonic Evolution of the Chukotka-Arctic Alaska Block: Problems of the Rotational Model Boris A. Natal’in Istanbul Technical University.
The Arctic Alaska-Canada Connection Revisited Jaime Toro, West Virginia University Frances Toro, DOE NETL Ken Bird, USGS Chris Harrison, GSC.
Heat Flow Drilling as a Geothermal Exploration Tool Chris Matthews Technical Manager Australian Geothermal Energy Association Australian Geothermal Energy.
Fault Mechanics and Strain Partitioning Session Axen, Umhoefer, Stock, Contreras, Tucholke, Grove, Janecke.
Tano Basin - Onshore to Shallow Offshore. Current licensing map.
Hosted by the Institute of Geology the
Sedimentary Geology Geos 240 – Chapter 2 Collecting the Data Part 2 – Regional Geophysical Data Dr. Tark Hamilton Camosun College.
Seismic Stratigraphy – identifying the seismic sequence
Department of Geology and Geological Engineering
Maps of eroded thicknesses of Triassic, Jurassic and Cretaceous sediments: (a) eroded thickness of the Triassic; (b) Lower and Middle Jurassic; (c) Upper.
Continental shelf offshore San Pedro/Long Beach showing general location of the Wilmington Graben in red Small circles are earthquake epicenters Line of.
Merged map showing the Late Jurassic tectonic framework of the Danish Central Graben after Ineson et al. Merged map showing the Late Jurassic tectonic.
Seismic Interpretation
Measured and modelled vitrinite reflectance and present-day temperature data in a selection of wells in the study area: (a, b) modelled vitrinite reflectance.
Main structural features of the East Siberian Sea Shelf.
Simplified stratigraphic chart showing the age of the main depth maps used in the 3D model (dashed lines). Simplified stratigraphic chart showing the age.
Basin evolution and destruction in an Early Proterozoic continental margin: the Rinkian fold–thrust belt of central West Greenland by John Grocott, and.
Disturbance of seafloor sediments on high-latitude shelves.
Calculated maturity (vitrinite reflectance values; Sweeney & Burnham 1990) at the top of the Hot Shale unit over four time steps: (a) modelled maturity.
Main sedimentary basins of the Siberian Arctic Shelf (modified from Grantz et al. 2009). Main sedimentary basins of the Siberian Arctic Shelf (modified.
Tectonic interleaving along the Main Central Thrust, Sikkim Himalaya
Interpreted ranges of effective fracture apertures.
by Jashar Arfai, and Rüdiger Lutz Petroleum Geology Conference
The burial history of three 1D extractions from the 3D model: (a) 1D burial history at the location of well C-16-1 in the Central Graben; (b) of well B-11-2.
The early Quaternary North Sea Basin
Chapter 1 Introduction to the geology of Myanmar
Schematic overview of depositional environments occurring in the terrestrial and marine realm which are mentioned in the text. Schematic overview of depositional.
Chapter 1 An overview of the petroleum geology of the Arctic
Merged map showing the Late Jurassic tectonic framework of the Danish Central Graben after Ineson et al. Merged map showing the Late Jurassic tectonic.
(a) Location map and the subdivision (northern, southern, central) of the study area. (a) Location map and the subdivision (northern, southern, central)
by Satish C. Singh, and Raphaële Moeremans
Geological Society, London, Memoirs
by Alan M. Roberts, Nick J. Kusznir, Graham Yielding, and Hugh Beeley
Water supply maps for northern France created by British military geologists during World War II: precursors of modern groundwater development potential.
Summary of bulk porosity measurements and bulk porosity interpretation from LWD density neutron data recorded in the horizontal well. Summary of bulk porosity.
South China Sea crustal thickness and oceanic lithosphere distribution from satellite gravity inversion by Simon Gozzard, Nick Kusznir, Dieter Franke,
The Petroleum Geology of NW Europe: 50 years of learning – a platform for present value and future success. An overview by Bruce Levell, and Mike Bowman.
Geologic Maps Lecture 38.
Examples of the first seafloor and sub-seafloor acoustic mapping records used to interpret submarine glacial landforms. Examples of the first seafloor.
Calculated maturity (vitrinite reflectance values: Sweeney & Burnham 1990) at the top of the Posidonia Shale unit over four time steps: (a) modelled maturity.
by Duncan Macgregor, John Argent, and Pamela Sansom
Simplified cross-section illustrating internal structure and inferred stratigraphy of the South Chukchi and North Chukchi basins. Simplified cross-section.
Geometry and key elements of the Central Andaman Basin and East Andaman Basin. Geometry and key elements of the Central Andaman Basin and East Andaman.
Summary diagram of the Upstream Exploration and Production Value Chain illustrating the range of uncertainty and value creation from access to cessation.
The three fracture end members (microfractures, joints and seismically identified faults) that comprise the Lancaster conceptual model. The three fracture.
Evidence from Rb–Sr mineral ages for multiple orogenic events in the Caledonides of Shetland, Scotland by S. Walker, M. F. Thirlwall, R. A. Strachan, and.
(a) Multibeam-bathymetric image of Malangsdjupet cross-shelf trough on the Norwegian shelf, showing submarine landforms in the trough and on the adjacent.
(a) Map of the stretching (β) factor for the Late Jurassic rift at 155 Ma, based on Roberts et al. (a) Map of the stretching (β) factor for the Late Jurassic.
Geological Society, London, Memoirs
Schematic cross-section from the eastern Alcock Rise across the East Andaman Basin, SE offshore Myanmar. Schematic cross-section from the eastern Alcock.
Stratigraphy of the well known basins of the eastern Arctic.
by Alan M. Roberts, Andrew D. Alvey, and Nick J. Kusznir
Pressure derivative plot from 205/21a-6 DST data.
The composite BGR seismic reflection line (line 1 in Fig
Russia, FSU and the Circum-Arctic: ‘the final frontier’
Summary geology of the North Sea and broader region illustrating the principal reservoir and source systems, and showing the range of papers covered in.
Geological Society, London, Memoirs
(a) Location map and the subdivision (northern, southern, central) of the study area. (a) Location map and the subdivision (northern, southern, central)
Extract from the Intersect full-field simulation model exhibiting a pressure drawdown snapshot over a particular reservoir depth in relation to the horizontal.
Boundary conditions for the basin modelling include: (a) the history of palaeowater depth (PWD) and (b) sediment–water interface temperature (SWIT) that.
Transformation ratio evolution of the Hot Shale layer in the John Graben extracted from the 3D basin model for three different reaction kinetics after.
by Alan M. Roberts, Nick J. Kusznir, Graham Yielding, and Hugh Beeley
Maps of Australia showing the location of the NGSA sample sites (dots) and (a) labelled geological regions of Australia (Blake & Kilgour 1998), and (b)
Crustal cross-sections with Moho from gravity-anomaly inversion along line 1. Crustal cross-sections with Moho from gravity-anomaly inversion along line.
Structure of the Laptev Rift System (after Drachev et al
Presentation transcript:

Petroleum Geology Conference ERRATUM Petroleum Geology Conference Volume 7(1):1-6 January 4, 2011 © Petroleum Geology Conferences Ltd. Published by the Geological Society, London

Schematic geological cross-sections based on re-interpretation of deep seismic reflection and refraction data acquired and published by SMG (Sharov et al. 2005; Ivanova et al. 2006): (a) through the Eastern Barents and South Kara basins based on seismic transect 2-AP, (b) though the North Kara Province based on seismic transect 3-AP. Schematic geological cross-sections based on re-interpretation of deep seismic reflection and refraction data acquired and published by SMG (Sharov et al. 2005; Ivanova et al. 2006): (a) through the Eastern Barents and South Kara basins based on seismic transect 2-AP, (b) though the North Kara Province based on seismic transect 3-AP. Location is shown in Figures 3 and 5. Bold numbers from 1 to 6 in (a) and from 1 to 5 in (b) denote seismic stratigraphic units (see the text for the details). Geological Society of London Petroleum Geology Conference series 2010;7:1-6 © Petroleum Geology Conferences Ltd. Published by the Geological Society, London

Main sedimentary basins of the Siberian Arctic Shelf (modified from Grantz et al. 2009). Main sedimentary basins of the Siberian Arctic Shelf (modified from Grantz et al. 2009). Bold numbers denote the following basins: 1, Southwest Laptev Basin; 2, Ust' Lena Rift; 3, Omoloy Graben; 4, Ust' Yana Graben; 5, Bel'kov Rift; 6, Anisin Rift; 7, New Siberian Rift; 8, Tas–Takh Depression; 9, East Siberian Sea Basin; 10, New Siberian–Wrangel Basin; 11, Longa Basin; 12, Northwind Basin. BRFB, Brooks Range Fold Belt. Geological Society of London Petroleum Geology Conference series 2010;7:1-6 © Petroleum Geology Conferences Ltd. Published by the Geological Society, London

Structure of the Laptev Rift System: (a) simplified depth-to-basement map of the Laptev Shelf based on 2D seismic and ERS-2 gravity data; (b) cross-section based on geological data and published BGR regional seismic lines (Franke et al. 2000, 2001). Structure of the Laptev Rift System: (a) simplified depth-to-basement map of the Laptev Shelf based on 2D seismic and ERS-2 gravity data; (b) cross-section based on geological data and published BGR regional seismic lines (Franke et al. 2000, 2001). Location of the cross-section is shown in (a). Bold numbers in (a) denote following elements of the rift system: 1, Southwest Laptev Rift Basin; 2, Ust' Lena Rift; 3, East Laptev Horst; 4, Stolbovoi Horst; 5, Shiroston Horst; 6, Anisin Rift; 7, Bel'kov Rift; 8, Svyatoi Nos Graben; 9, Kotel'nyi High; 10, New Siberian Rift; 11, De Long High. SAS (?) in (b) denotes possible offshore projection of the South Anyui Suture. Geological Society of London Petroleum Geology Conference series 2010;7:1-6 © Petroleum Geology Conferences Ltd. Published by the Geological Society, London

Main structural features of the East Siberian Sea Shelf. Main structural features of the East Siberian Sea Shelf. NSR, ESSB and LB denote New Siberian Rift, East Siberian Sea Basin and Longa Basin accordingly. Bold line indexed G–H shows location of a cross-section given in Figure 14. The italic capital letters index the following islands: KT, Kotel'nyi; NS, Novaya Sibir'; BL, Bol'shoi Lyakhov. The accuracy of the scale bar increases towards 75°N. Geological Society of London Petroleum Geology Conference series 2010;7:1-6 © Petroleum Geology Conferences Ltd. Published by the Geological Society, London

Main structural elements of the Chukchi Shelf (modified from Grantz et al. 2009). Main structural elements of the Chukchi Shelf (modified from Grantz et al. 2009). Bold solid line labelled ‘J–I’ shows location of cross-section given in Figure 16. Capital italic letters denote: HT, Hanna Trough; SCB, South Chukchi Basin; KSB, Kotzebue Sound Bay. The accuracy of the scale bar increases towards 75°N. Geological Society of London Petroleum Geology Conference series 2010;7:1-6 © Petroleum Geology Conferences Ltd. Published by the Geological Society, London

Simplified cross-section illustrating internal structure and inferred stratigraphy of the South Chukchi and North Chukchi basins. Simplified cross-section illustrating internal structure and inferred stratigraphy of the South Chukchi and North Chukchi basins. Based on seismic data acquired and published by DMNG and TGS-Nopec (Petrovskaya et al. 2008; Verzhbitsky et al. 2008) and ERS-2 gravity data. Location is given in Figures 3 and 15. The bold numbers are indexes of the seismic sequences in the South Chukchi Basin after Tolson (1987). The alpha-numeric indexes CS-1 through CS-6 denote seismic sequences identified in the North Chukchi and the New Siberian–Wrangel basins (see text for further details). LCU, Lower Cretaceous Unconformity; MBU, Mid Brookian Unconformity. NSWFB denotes the New Siberian–Wrangel Foreland Basin. Geological Society of London Petroleum Geology Conference series 2010;7:1-6 © Petroleum Geology Conferences Ltd. Published by the Geological Society, London