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

Slides:



Advertisements
Similar presentations
Concentration My main idea of concentration is poster(or illustration) with positive messages. Most of artwork has messages. I respect any message that.
Advertisements

computer
© UNT in partnership with TEA1 7 th Grade Career Exploration Module Career Focus: Video Game Programmer.
Adobe Illustrator.  Graphic design can be thought of as a visual language that is used to convey a message to an audience.  A graphic design is a visual.
Graphic Designer Kenny Paresa. Job Description Graphic designers-a.k.a. graphic artists- plan, analyze, and create solutions to communication problems.
:44:53.
Time Remaining 20:00.
BY SCHUYLER BAILEY. Why I Want to be a Graphic Designer o I enjoyed my Web Page Design class o Doing things on computers makes me feel accomplished.
Creativity, Culture and Innovation International EU Colloquium.
Engineering Geology William Shehata.
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.
Experience the Magic of Online Ordering
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.
Disturbance of seafloor sediments on high-latitude shelves.
Chapter 3 – part2.
Calculated maturity (vitrinite reflectance values; Sweeney & Burnham 1990) at the top of the Hot Shale unit over four time steps: (a) modelled maturity.
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.
Quarterly Journal of Engineering Geology and Hydrogeology
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.
Schematic overview of depositional environments occurring in the terrestrial and marine realm which are mentioned in the text. Schematic overview of depositional.
Quarterly Journal of Engineering Geology and Hydrogeology
Stoke 100 Reads Reading log Name: Class:.
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)
Liberation of selenium from alteration of the Bowland Shale Formation: evidence from the Mam Tor landslide by John Parnell, Liam Bullock, Joseph Armstrong,
Diversity in the science and practice of engineering geology
Geological Society, London, Engineering Geology Special Publications
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.
Quarterly Journal of Engineering Geology and Hydrogeology
Stoke Reads On Reading log Name: Class:.
Geological Society, London, Engineering Geology Special Publications
Comparison between seafloor bathymetry derived from a P-Cable 3D seismic survey (b) and multibeam bathymetry (a) in an area dominated by iceberg plough.
Summary diagram of the Upstream Exploration and Production Value Chain illustrating the range of uncertainty and value creation from access to cessation.
Quarterly Journal of Engineering Geology and Hydrogeology
Advances in engineering geology in the UK 1950–2018
The m long and 70 m wide 3D seismic survey vessel Ramform Atlas, part of the fleet of the marine geophysical company PGS. This vessel belongs to.
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
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.
Pressure ridge west of the Yangon–Naypyidaw–Mandalay Expressway, south of Naypyidaw ( ° N, ° E): (a) view of the ridge; (b) more coherent.
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.
Approximately 2 m diameter shaft exposed at the site of the Nottingham Business Park near Strelley. Approximately 2 m diameter shaft exposed at the site.
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 ‘Oil Patch Warrior’, a statue in the Dukes Wood Nature Reserve commemorating the 44 roughnecks who arrived from Oklahoma in 1942 to develop the Dukes.
Schematic cross-section for the Outer Wash, showing the ground conditions interpreted by the British Geological Survey (1991). tk, Undivided Mesozoic Strata.
(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.
Cropwell Bishop gypsum quarry.
NW–SE section across Figure 2 showing the regional dip (exaggerated) of the post-Palaeozoic strata and the NW-facing scarp slopes of the Permian strata.
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)
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.
Crustal cross-sections with Moho from gravity-anomaly inversion along line 1. Crustal cross-sections with Moho from gravity-anomaly inversion along line.
Editorial by Eddie Bromhead, and Daren Gooddy
Presentation transcript:

Comparison of graphic log systems illustrating the difference in geological message between (a) use of basic symbols used with ‘artistic flexibility’ and (b) computer-generated log. Comparison of graphic log systems illustrating the difference in geological message between (a) use of basic symbols used with ‘artistic flexibility’ and (b) computer-generated log. After Stapledon (1986). While computer logging has come a long way since 1986, a degree of inflexibility remains in graphically illustrating important geological features. Mark J. Eggers Geological Society, London, Engineering Geology Special Publications 2016;27:1-18 © 2016 The Author(s). Published by The Geological Society of London