Depth contour maps for the Rotliegend formations of the                     central Saar-Nahe Basin, SW Germany

AbstractThe present study is focused on the subsurface geology of Bannu Basin, a part of western Indus foreland Pakistan. For this purpose, some regional seismic profiles and deep exploratory wells data have been used in integration.A total of ten mappabale seismic reflection events have been identifed which are representative of specific geological units. In general, based on the seismic the formation trends, the horizons are dipping in the northwest direction of the study area. The area generally deepens toward the northwest due to sediments load toward the northwest. The seismic profile MWI-83 shows a unique faults bounded anticlinal structure that has also been mapped on the two-dimmensional contour maps. This could be regarded as potential hydrocarbon entrapment. The regional seismic profiles are contoured for the entire grid in both time and depth domain to obtain the clearer image of the subsurface individual stratigraphic units. The 2D contour maps for Lower Permian aged Warcha Sandstone, Middle Triassic aged Tredian Formation and Early Jurrasic aged Datta Formation have been prepared using gridded TWT of the seismic profiles. The time and depth contour maps of the Datta Formation and Tredian Formation show a four way clouser oriented in the southeast dierction. The area of the closure was computed which is 24 Sq km approximately. Furthermore, the formation tops of the five wells have been used to correlate the wells for understanding the lateral and vertical variations in the stratigraphic layers. The correlation shows that the Datta Formation’s thickness increases at the centre of the basin whereas decreases on the east and south flanks of the basin. Reasons of Wells failure were concluded on the basis of the final well report and concluded that these well failure occur due to poor quality of the data and also due to some mechanical problems. Reservoircharacterization using statistical rock physics and petrophysics coupled with core data analysis can provide further insights into the hydrocarbon exploration.

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From reflection elements to structure — A look at the history of data interpretation

Geophysics ◽

10.1190/1.3465562 ◽

2010 ◽

Vol 75 (5) ◽

pp. 75A121-75A128

Author(s):

Klaus Helbig

Keyword(s):

Data Acquisition ◽

Magnetic Recording ◽

Data Interpretation ◽

Journal Articles ◽

Contour Maps ◽

New Methods ◽

Field Office ◽

Depth Contour ◽

History Of ◽

Ray Geometry

Traditionally, input acquired in the field consisted of the original paper records; output submitted to the client consisted of structural sections and depth-contour maps of selected interfaces. Before the introduction of magnetic recording, it was common practice to do the conversion in the field office. Tools for this conversion ranged from slide rules and desk calculators to wavefront charts. These tools were based on the geometry of rays in media where velocity is a function of depth only. The detailed algorithms underlying the conversion were often developed in the exploration companies and — originally — were carefully guarded. But at least the underlying principles were exchanged throughout the industry through books, journal articles, and presentations at meetings, such as noted in nearly 300 references in C. H. Dix’s Seismic Prospecting for Oil (1952) . The techniques of data acquisition and data interpretation have changed considerably, but the underlying principles of ray geometry are the same. Therefore, many new methods are based on ideas formulated in the early times of the industry.

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Uncertainty analysis of runoff estimates from runoff-depth contour maps produced by five automated procedures for the northeastern United States

10.15760/etd.6197 ◽

2000 ◽

Author(s):

Gary Bishop

Keyword(s):

United States ◽

Uncertainty Analysis ◽

Northeastern United States ◽

Contour Maps ◽

Depth Contour ◽

Runoff Depth ◽

Automated Procedures

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Analysis of the 9th November 1990 flare

International Astronomical Union Colloquium ◽

10.1017/s025292110006454x ◽

2000 ◽

Vol 179 ◽

pp. 229-232

Author(s):

Anita Joshi ◽

Wahab Uddin

Keyword(s):

Image Processing ◽

Two Dimensional ◽

Temporal Behaviour ◽

Contour Maps ◽

Dimensional Measurements ◽

Processing Software ◽

Image Processing Software

AbstractIn this paper we present complete two-dimensional measurements of the observed brightness of the 9th November 1990Hαflare, using a PDS microdensitometer scanner and image processing software MIDAS. The resulting isophotal contour maps, were used to describe morphological-cum-temporal behaviour of the flare and also the kernels of the flare. Correlation of theHαflare with SXR and MW radiations were also studied.

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Small Computer System for Micrograph Analysis

Proceedings, annual meeting, Electron Microscopy Society of America ◽

10.1017/s0424820100097879 ◽

1981 ◽

Vol 39 ◽

pp. 270-271

Author(s):

J. F. Hainfeld ◽

J. S. Wall

Keyword(s):

Large Range ◽

Small Computer ◽

Black And White ◽

Contour Maps ◽

Points Of Interest ◽

Computer Aided Analysis ◽

Specialized Hardware ◽

Additional Memory ◽

Selection Of ◽

Publication Quality

Cost reduction and availability of specialized hardware for image processing have made it reasonable to purchase a stand-alone interactive work station for computer aided analysis of micrographs. Some features of such a system are: 1) Ease of selection of points of interest on the micrograph. A cursor can be quickly positioned and coordinates entered with a switch. 2) The image can be nondestructively zoomed to a higher magnification for closer examination and roaming (panning) can be done around the picture. 3) Contrast and brightness of the picture can be varied over a very large range by changing the display look-up tables. 4) Marking items of interest can be done by drawing circles, vectors or alphanumerics on an additional memory plane so that the picture data remains intact. 5) Color pictures can easily be produced. Since the human eye can detect many more colors than gray levels, often a color encoded micrograph reveals many features not readily apparent with a black and white display. Colors can be used to construct contour maps of objects of interest. 6) Publication quality prints can easily be produced by taking pictures with a standard camera of the T.V. monitor screen.

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Two structural states of the Z-band in cardiac and skeletal muscle

Proceedings, annual meeting, Electron Microscopy Society of America ◽

10.1017/s0424820100157097 ◽

1989 ◽

Vol 47 ◽

pp. 1022-1023

Author(s):

J.P. Schroeter ◽

M.A. Goldstein ◽

J.P. Bretaudiere ◽

L.H. Michael ◽

R.L. Sass

Keyword(s):

Skeletal Muscle ◽

Cross Section ◽

Real Space ◽

Contractile State ◽

Contour Maps ◽

False Color ◽

Grey Scale ◽

Fourier Filtering ◽

Cardiac Muscles ◽

Enhancement Algorithm

We have recently established the existence of two structural states of the Z band lattice in cross section in cardiac as well as in skeletal muscle. The two structural states are related to the contractile state of the muscle. In skeletal muscle at rest, the Z band is in the small square (ss) lattice form, but tetanized muscle exhibits the basket weave (bw) form. In contrast, unstimu- lated cardiac muscle exhibits the bw form, but cardiac muscles exposed to EGTA show the ss form.We have used two-dimensional computer enhancement techniques on digitized electron micrographs to compare each lattice form as it appears in both cardiac and skeletal muscle. Both real space averaging and fourier filtering methods were used. Enhanced images were displayed as grey-scale projections, as contour maps, and in false color.There is only a slight difference between the lattices produced by the two different enhancement techniques. Thus the information presented in these images is not likely to be an artifact of the enhancement algorithm.

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