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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...

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...