Calculated maturity (vitrinite reflectance values: Sweeney & Burnham 1990) at the top of the Namurian–Visean unit over four time steps: (a) Late Carboniferous;

Slides:

Advertisements

Similar presentations

Chapter 7: Earth Materials as Time Keepers

Advertisements

Natural Resources Bedrock Geology Coastlines. Natural Resources Nova Scotia Geology Precambrian to Carboniferous: undifferentiated intrusive rocks Precambrian:

End Show Slide 1 of 40 Copyright Pearson Prentice Hall 17-1 The Fossil Record.

Earth’s Geologic History based on fossils

Source Rock BY: ABDELRAHMAN AHMED ALI ABDELRAHMAN UNDER SUPERVISOR OF:

OPK-3 Mud Gas Analysis Fig. 1 Comparison of d15N nitrogen vs. d13C methane measured on a RFT Gas sample from OPK-3A vs. samples within NAM's concession.

Online Gifts Buy for wishes happy mother's day to yours choice and with happy gifts find here:

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.

The Geologic Time Scale

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.

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.

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.

Log data from 205/21a-6 across an interval of Fractured Basement and an interval of Fault Zone. Log data from 205/21a-6 across an interval of Fractured.

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.

Unit 3 Review (Calculator)

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)

Geological Society, London, Engineering Geology Special Publications

Summary of bulk porosity measurements and bulk porosity interpretation from LWD density neutron data recorded in the horizontal well. Summary of bulk porosity.

Determining the Function Obtained from a Series of Transformations.

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.

62 – Sequences and Series Day 1 Calculator Required

Geological Society, London, Engineering Geology Special Publications

The Carnian Pluvial Episode and the origin of dinosaurs

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

Calculate 9 x 81 = x 3 3 x 3 x 3 x 3 3 x 3 x 3 x 3 x 3 x 3 x =

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.

Summary diagram of the Upstream Exploration and Production Value Chain illustrating the range of uncertainty and value creation from access to cessation.

Geologic Time Scale The following fold-over is depicted using colored paper – this was for demonstration purposes only. Use 7 white blank sheets of paper.

Geologic Timeline based on Fossils

The three fracture end members (microfractures, joints and seismically identified faults) that comprise the Lancaster conceptual model. The three fracture.

The glaciated trough of the Gasterntal, looking up-valley from the Stock hill; the 1908 tunnel breakthrough created a valley-floor sinkhole in the woodland.

(a) Map of the Isle of Skye (Scotland), with a box denoting Brothers’ Point (Rubha nam Brathairean), where the two theropod teeth described here (NMS G

Classification of NMS G , NMS G

Isolated neotheropod teeth from the Middle Jurassic of the Isle of Skye, Scotland. Isolated neotheropod teeth from the Middle Jurassic of the Isle of Skye,

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.

Map showing approximate limits of Northern Hemisphere ice sheets at the present day and during the Last Glacial Maximum (LGM). Map showing approximate.

Sensitivity of crustal thickness and continental lithosphere thinning determined from gravity inversion to sediment thickness used in the gravity inversion.

(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.

Comparison of graphic log systems illustrating the difference in geological message between (a) use of basic symbols used with ‘artistic flexibility’ and.

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.

Rafts of chalk emplaced within shallow marine sands and gravels of the Wroxham Crag Formation, exposed in the cliff face at Sidestrand, Norfolk; the upper.

The composite BGR seismic reflection line (line 1 in Fig

Russia, FSU and the Circum-Arctic: ‘the final frontier’

(a) Southern Scotland and northern England coalfield exposure and locality of the Greenburn surface mine and (b) regional mineral resource geology of the.

Map showing the geographical locations of the contributions to the Atlas of Submarine Glacial Landforms (yellow dots). Map showing the geographical locations.

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)

Introducing the Energy Geoscience Series

Ferric iron content of garnet and spinel from mantle rocks plotted as a function of the calculated log fO2 using equations (9)–(11). Ferric iron content.

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.

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)

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.

Presentation transcript:

Calculated maturity (vitrinite reflectance values: Sweeney & Burnham 1990) at the top of the Namurian–Visean unit over four time steps: (a) Late Carboniferous; (b) Late Triassic; (c) Late Jurassic and (d) the present day. Calculated maturity (vitrinite reflectance values: Sweeney & Burnham 1990) at the top of the Namurian–Visean unit over four time steps: (a) Late Carboniferous; (b) Late Triassic; (c) Late Jurassic and (d) the present day. (e)–(h) The calculated transformation ratios for the same time steps as above. The calculated transformation ratios are based on Burnham (1989) TIII for the Namurian–Visean source rock. Jashar Arfai, and Rüdiger Lutz Petroleum Geology Conference series 2018;8:67-86 © 2018 The Author(s). Published by the Geological Society, London