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Bathymetric mapping is the first step in any underwater and sea bed investigation, especially for petroleum exploration. In most we face with a complex of sand and gravel covering the bottom of the sea. Differentiate these two type of seafloor covering material is the case of many research in offshore exploration. In this article We investigated a practical case history to define and show the differences of sand and gravel in their images. The images were obtained by the Yellow-Fin side scan sonar instrument and p...

Defining the mineral potential of the sea floor could be handled by different methods, but the prerequisites for each methods is to clear the conditions of precipitation environment such as physico – chemical conditions and also it depends on the type of precipitant. The appearance of any mineral in the sea floor strongly depends on the aqueous environment and the physical prosperities of the mineral. In this article, first of all, I considered the physiographic regions of the sea floor in entire the world, an a...

In this article I considered the design of a computer simulation model that approximates the exploration of a petroleum basin when exploration is conducted sequentially and according to geological hypothesis with costs and performance characteristics typical of an exploration firm. These features lead naturally to a model design in which a state of nature is created. The exploration firm initially has no knowledge of this state, only of hypothesis. In this model also, exploration decision are made according to pri...

A standard imaging method in seismic data processing is the simulation of a zero offset section from seismic reflection data. In traditional imaging methods, e. g. NMO/DMO/stack, an accurate macro velocity model is needed. Common reflection surface (CRS) stack is a new data driven method, introduced in recent years which remove the necessity of making this model and just use the surface velocity to simulate zero offset section (2D) or volume (3D). In this article, we drive the CRS stacking on a synthetic data to o...

Making macro velocity model is the most important part in any seismic data processing system. It is a very time consuming and none accurate step in conventional methods like NMO/DMO/stack. In this article, we drive a velocity model for a synthetic data with new introduced tomographic inversion method. This method uses the kinematic wavefield attributes which would yield from common reflection surface (CRS) stacked data. These attributes are normal (N) wave and normal incidence point (NIP) wave curvatures. The tomo...

The Sabzevar ophiolite is a highly dismembered ophiolite complex located along the northern boundary of the Central Iranian Microcontinet (CIM) and is one of the internal groups of ophiolites and colored melange. The area has various lithological units that are the cause of Sabzevar colored melange zone. There are many chromite pods in the area but the high topography and mountainous condition and inability to trace the hidden lenses, many of them are not explored yet. A mathematical- genetic model could be helpfu...