DOWNLOAD CONTOH STEMPEL PSD
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DOWNLOAD CONTOH STEMPEL PSD
. psd template adalah jendela untuk mengedit foto vector. dengan cara bisa menggunakan Photoshop yang terbuat di dalam file jendela.. bangunya pada layer penuh penuh, bulat atau teks.The present invention relates to a method of selecting the geometric properties of a column in a seismic survey, such as the maximum number of source-receiver pairs and the number of sources in each source-receiver pair.
In seismic prospecting, the goal is to determine the earth's subsurface structure. In an oil and gas well, it is desirable to ascertain whether there are economically recoverable quantities of oil or gas present. The structure of the subsurface layers that may contain oil or gas can be determined by seismically imaging the subsurface. The goal of seismics is to provide a means of imaging this structure.
The geological formation of interest may be divided into subsurface layers or intervals of different acoustic velocities (“seismic impedance”). These intervals in the subsurface may contain hydrocarbons. The acoustic or seismic wave velocity is measured by recording a sound wave of a given frequency. The sound wave travels through the various subsurface intervals, changing its frequency as a result of the differing velocities of the different formations. Measuring this frequency change and establishing the location of the various formations is a function of the strength of the waves, the quality of the source-receiver pair, and the size and properties of the subsurface layers. The velocities are determined using either seismic waves or acoustic waves.
The depth to which the subsurface layers can be analyzed is primarily dependent upon the length of the source and receiver arrays and the number of source-receiver pairs. In a three dimensional (“3D”) seismic survey, the source and receiver arrays are generally a few hundred meters long. A 3D survey can be done using one of several different types of acquisition methods. In an airborne acquisition, the arrays are moved along a grid by a survey airplane. In a marine acquisition, the arrays are towed behind a survey vessel. In either case, there are typically a few thousand source-receiver pairs.
The number of source-receiver pairs in a seismic survey can be described using various terms, including “spotting,” � 0b46394aab
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