#HAMPSON RUSSELL NEW PROJECT SETUP SOFTWARE#

September 2008 see the Installation Geoview and eLOG Guide or the Geoview online help. Click the View3D.wdb item in the Available List and click OK. Click the View3D folder of the HRS/data directory to bring up a list of databases in that folder. To load this database for the first time, click Open to bring up the Directory Chooser. For this tutorial, a database has already been created for you. A database is identified by the extension wdb. When you first launch Geoview, the first window that you see is the Opened Database List, which displays your recently used databases.

On a Unix workstation, go to a command window and type: Geoview On a PC, click the Start button and select the Geoview option on the Programs / HRS applications menu. If you are unfamiliar with the use of Geoview, please refer to the Guide to GEOVIEW and eLOG documentation. Geoview is the application manager that acts as a launch pad for other Hampson-Russell programs.

#HAMPSON RUSSELL NEW PROJECT SETUP SOFTWARE#

September 2008 2 View3D Starting Hampson-Russell Software The first step is to start the Geoview program.

Two data slices: seismic target and scaled porosity, positioned at the same place as the horizon file.

Each well contains a sonic log (p wave), density log, porosity log and a checkshot file.

An attribute volume, scaled_porosity.vol, which is a 3D post-stack data set.

A SEG-Y file, seismic.vol, which is a 3D post-stack data set.

The data set for this tutorial consists of: This tutorial takes you through the most important options and features of View3D. The general objective is to better visualize, illustrate and spatially analyze the data from HRS programs. 45 2 View3D 1 GUIDE TO VIEW3D Introduction to View3D View3D is a program used to view wellbore paths, well data, seismic data and attribute data as a three dimensional volume. 37 Emphasizing Value Ranges and Setting Transparency: Visual Control. 21 Showing Traces and Color Plots Together. Our results indicate that the geophysical data along the borehole image the change of the composition of the rocks which probably originates from magmatic intrusions and have been overprinted by geological processes, rather than from fracture zones.View3D GuideIntroduction to View3D. We show that the combination of these data allows us to distinguish between rocks from mafic and sedimentary origin. This study combines data from the COSC-1 borehole with different geophysical measurements to better understand the lithology and structure of the Seve Nappe Complex. The challenge remains to image the remnant of these processes in high detail but at the same time over a large area. Former collision zones that are closer to the surface these days allow the investigation of these processes much better, for example at the COSC-1 borehole in the central Scandinavian Caledonides. However, these processes and the conditions at which they take place are difficult to study because of the great depth at which they occur. Plain Language SummaryДЄreas where continents collide experience different kind of deformation. Our results suggest that ductile-deformed middle crustal reflectivity is primarily a function of pre-orogenic lithological variations which has to be considered when deciphering mountain building processes. Their setting indicates that the Seve Nappe Complex consists of the remnants of a volcanic continental margin. Reflections in the Seve Nappe Complex are not as distinct as in greater depths but continuous and several of them can be linked to magmatic intrusions, which have been metamorphically overprinted. Our results indicate that reflections along the borehole are primarily caused by compositional rather than textural changes. Especially gamma ray logs in combination with density data are powerful tools to distinguish between mafic and felsic lithologies in log-core correlation. This is one of the few studies that shows that core-log-seismic integration in metamorphic rocks allows to identify the spatial distribution of major lithological units. This study combines data from the COSC-1 borehole with different seismic measurements to provide constraints on the spatial lithological and textural configuration of the Seve Nappe Complex. Ancient exhumed collision zones allow us to investigate these processes much better, for example at the COSC-1 borehole in the central Scandinavian Caledonides. However, the physical and chemical conditions at which these zones operate and the deformation processes that enable up to hundreds of km of tectonic transport are still unclear because of the depth at which they occur and the challenges in imaging them. Continental collision causes deformation in the crust along shear zones.

Hampson russell new project setup