Introducing the Energy Geoscience Series

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Copyright © 2009 Pearson Education, Inc. Publishing as Pearson Addison-Wesley Chapter 16 RESOURCES AND THE ENVIRONMENT AT THE GLOBAL LEVEL.
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Figure 1. The Modified Dual Pathway Model.
BACK SOLUTION:
Maps of eroded thicknesses of Triassic, Jurassic and Cretaceous sediments: (a) eroded thickness of the Triassic; (b) Lower and Middle Jurassic; (c) Upper.
كيف تجعل حياتنا أكثر سهولة
Merged map showing the Late Jurassic tectonic framework of the Danish Central Graben after Ineson et al. Merged map showing the Late Jurassic tectonic.
by Agus M. Ramdhan, and Neil R. Goulty
Measured and modelled vitrinite reflectance and present-day temperature data in a selection of wells in the study area: (a, b) modelled vitrinite reflectance.
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.
Interpreted ranges of effective fracture apertures.
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.
Chapter 1 Introduction to the geology of Myanmar
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)
Figure 1 Flow diagram detailing the systematic review process.
by Alan M. Roberts, Nick J. Kusznir, Graham Yielding, and Hugh Beeley
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,
by Philip S. Ringrose Petroleum Geoscience Volume 23(3):
Fig. 1 Flow chart of included patients for analyses
Fig. 1 Flow chart for selection of study subjects
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.
Unless provided in the caption above, the following copyright applies to the content of this slide: Published on behalf of the European Society of Cardiology.
Calculated maturity (vitrinite reflectance values: Sweeney & Burnham 1990) at the top of the Posidonia Shale unit over four time steps: (a) modelled maturity.
The geochemistry of oil in Cornish granites
Modified at -
by Duncan Macgregor, John Argent, and Pamela Sansom
Comparison between seafloor bathymetry derived from a P-Cable 3D seismic survey (b) and multibeam bathymetry (a) in an area dominated by iceberg plough.
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.
Figure 1. International migrants by region of residence, 2015 Source: UN DESA, Figure 1. International migrants by region of residence, 2015.
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.
(a) Outcrop evidence of overpressure along the Sagaing Fault: sandstones injected into a bedded Miocene sandstone. (a) Outcrop evidence of overpressure.
Blow-ups of seismic image (a) along strike-slip fault shown in Figure 13.4a, (b) large fold along profile PGS08-12 and (c) along profile PGS08-06 near.
Sensitivity of crustal thickness and continental lithosphere thinning determined from gravity inversion to sediment thickness used in the gravity inversion.
Pressure ridge west of the Yangon–Naypyidaw–Mandalay Expressway, south of Naypyidaw ( ° N, ° E): (a) view of the ridge; (b) more coherent.
Illustration of the main dissonance factors hindering adoption of low-carbon energy solutions: (a) the lack of social and economic support for low-carbon.
Diagram showing the local impact of the deformation band network on oil saturation in model LL_1ORD, illustrating the controls of the deformation bands.
(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.
Calculated maturity (vitrinite reflectance values: Sweeney & Burnham 1990) at the top of the Namurian–Visean unit over four time steps: (a) Late Carboniferous;
Schematic cross-section from the eastern Alcock Rise across the East Andaman Basin, SE offshore Myanmar. Schematic cross-section from the eastern Alcock.
Data-driven workflow to obtain dynamic fluid-flow model and structural data from acquired drone images. Data-driven workflow to obtain dynamic fluid-flow.
Linking natural fractures to karst cave development: a case study combining drone imagery, a natural cave network and numerical modelling by Quinten Boersma,
Comparison of graphic log systems illustrating the difference in geological message between (a) use of basic symbols used with ‘artistic flexibility’ and.
Spectrum of terrestrial infrared radiation (Sportisse 2010).
Global mean surface temperature increase as a function of cumulative total global CO2 emissions from various lines of evidence. Global mean surface temperature.
Orientation of SHmax over the non-gas-bearing structure in Quadrant 43, derived from analysis of borehole breakouts in well 43/12-1. Orientation of SHmax.
by Alan M. Roberts, Andrew D. Alvey, and Nick J. Kusznir
Pressure derivative plot from 205/21a-6 DST data.
Knowledge v. solution skills matrix from Roberts (1963) as reported in Stapledon (1996). Knowledge v. solution skills matrix from Roberts (1963) as reported.
Figure 1 Grant agencies and charitable foundations supporting Plan S.
The composite BGR seismic reflection line (line 1 in Fig
Russia, FSU and the Circum-Arctic: ‘the final frontier’
Map showing the geographical locations of the contributions to the Atlas of Submarine Glacial Landforms (yellow dots). Map showing the geographical locations.
Road cut in NW suburbs of Naypyidaw, illustrating strike-slip faulting and folding affecting Miocene Kyaukkok and Obogon formations. Road cut in NW suburbs.
A pair of Terra Satellite images of North Reef Island, North Andaman before (left) and after (right) the 2004 earthquake. A pair of Terra Satellite images.
Summary geology of the North Sea and broader region illustrating the principal reservoir and source systems, and showing the range of papers covered in.
(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.
(a) Global CO2 emissions from fossil-fuel combustion, cement manufacture, and gas flaring and global population, 1800 – 2014 (sources: carbon emissions.
Figure 1 ABCDE of primary prevention.2
Illuminated 3D perspective displays (with 7
Maps of Australia showing the location of the NGSA sample sites (dots) and (a) labelled geological regions of Australia (Blake & Kilgour 1998), and (b)
(a) Dot map showing the distribution of the top Jenks class of the Spearman correlation coefficients (rs > 0.52; red circles) of NGSA AR samples with respect.
Map of SW England (after Moon 2010), showing sample sites for oil residues at Wheal Speed, North Treskerby and South Crofty, and samples used for comparison.
Crustal cross-sections with Moho from gravity-anomaly inversion along line 1. Crustal cross-sections with Moho from gravity-anomaly inversion along line.
by Qiqi Wang, S. E. Laubach, J. F. W. Gale, and M. J. Ramos
Gall bladder volumes (mean (SEM)) in the fasting state, during, and after modified sham feeding (MSF) and in response to cholecystokinin (CCK) infusion.
Presentation transcript:

Introducing the Energy Geoscience Series by Philip S. Ringrose Petroleum Geoscience Volume ():petgeo2019-070 May 23, 2019 © 2019 The Author(s). Published by The Geological Society of London for GSL and EAGE. All rights reserved

Sketch illustrating the range of renewable and low-carbon energy solutions likely to dominate studies in applied geoscience during the energy transition (modified from Ringrose 2017). Sketch illustrating the range of renewable and low-carbon energy solutions likely to dominate studies in applied geoscience during the energy transition (modified from Ringrose 2017). Philip S. Ringrose Petroleum Geoscience 2019;petgeo2019-070 © 2019 The Author(s). Published by The Geological Society of London for GSL and EAGE. All rights reserved