The case area under study from geogeraphical point of view is located in 35 15 to 33 30 and E from 48 30 to 47 00 and involve parts of Lorestan northe western and Kermanshah south western parts wich extends partly to Alashtar , Noorabad, Harsin and Kermanshahks. This climatical and montanious area has a cold and rainy climate.The highest part in the peak is the Gareen mountain in Alashtar with the height of 3500 meters. The volcanic rocks in the north west of Noorabad are in the district of Zagross within Sanandaj and sirjsn.The above mentioned Ophiolite is a main part dd into of Kermanshah Ophiolite. The high Zagross is divided into three parts wich includes:limeston Bistoon , akhtaran Ophiolite and Radiolarits.The rocks of this complex from lower .to upper layers include Peridutits, Gabro layers, Isotop Gabroes, alittle Plagiogeranite, Daik, Bazalt, Andesite and some other rocks.The Petrogeraohic studies revealed that the primary inorganics have beer analyzed into secondary inorganic Ophiolite such as Iron Oxidation and Colorite. As well, the organics in there rocks include calco pyroxene, Bornits, Malacits, Azorits and metal Oxidation.The analysis of some of the Geogemical samples of some areas, a considerable amount og TI, Mn, and Cu is seen.In reality, the basic purpose of this research is about the Cu inorganic volcanic rocks (Andesite and Bazalte)The Anomal areas are more related wich heterologous of (Colorite, Epidote,seresite and Propelitic). Hower, the results of the Ophiolite volcanic showed that these rocks include Cu Anomali.the cases under study in Basalt, Andesite, Riolite, Tracits and Dasits related to calcalcalen were in volcanic areas with economical Kansares of metal elements such as Mn, Cu, V, Ti, Co, Cr along witch Alteramafic and mafic rocks. Since a big part of Ophiolite are composed of these rocks making Kansares of these elements in these Ophiolites is not avoidable the accomplishment of focal analysis of minerals by means of Microprobe started.This is because such Tasks can help in recognizing minerals compositional Zoning , Freguency of secondary elements which are rare as well as determining the Kind of environment.