Bidkhan region is located in central Iran structural zone as a part of the Urumieh-Dokhtar magmatic arc which is evolved during the Arabia-Eurasia convergence. In this region, quaternary deformations were consistent with recent faults activities [1] - [5] . From a lithological perspective, Bidkhan region is divided into three distinct and separable parts. The exterior part, which is formed by volcaniclastic, volcanogenic, and sedimentary deposits and interior part, which is divided into two parts of central and the surrounding ring. These two internal parts are formed by volcanic and subvolcanic outcrops. They have an intermediate to acidic chemical composition. Moving from margins to the center, alteration intensity varies from low (propylitic) to severely altered (phyllic, alunite, advanced argillic and potassic) [6] . Altered rocks such as propylitics, phyllics, albites, sericites, argillics, alunites, kaolins, carbonates, silicas, advanced argillics, potassics and malachites exist in Bidkhan region and especially in the central part of this area. Alteration is a characteristic of this region. It is necessary to note that alteration is observed in this region from propylitic zone to phyllic, alunite and potassic. Several conditions and circumstances are necessary for an event to become the main phenomenon in a region. Alteration of the interior outcrops has developed geochemical as the main phenomenon. Without a doubt, this geochemical phenomenon has made Bidkhan region as one of the biggest severely altered integrated sets of Iran [7] .

The position of Bidkhan rocks was studied on various diagrams Tas (Cox 1979) diagram: In which, SiO₂ is on the horizontal axis and Na₂O + K₂O are on the vertical axis. 30 samples were analyzed for this diagram (Figure 1). It can be observed that the rocks of this region are generally intermediate to acidic and vary from sub-alka- line to alkaline, which is a general trend. Based on the diagram, these rocks are in three ranges of trachyandesite, andesite and dacite, which is in accordance with microscopic and field observations [8] .

Examining Tas (Le Bas 1986) diagram confirmed the results of the above diagram. Based on this diagram, these rocks are generally intermediate to acidic, sub-alkaline, and are placed within three ranges of trachyandesite, andesite and dacite (Figure 2) [9] .

Tas (Middle Most 1994) diagram is newer than the previous ones. 30 analyzed samples are presented on the diagram to validate the previous diagrams. It is also observed in this diagram that these rocks were from three types of trachyandesite, andesite and dacite (Figure 3). It seems that magmatic origin of these rocks was andesitic and other trachyandesitic and dacitic rocks were created by other processes such as differentiation and digestion of walls from andesitic magma [10] .

The most important tectonic structures that exist are main, reverse, and relatively long quadruplet faults that have a northern-southern trend and movement. Fracture and minor faults of the strike slip with high density exist within the interstitial space of these main faults. In fact, Bidkhan valley is one of these main faults that are connected to the southern heights from its south side. This is the main fault of Bidkhan that have converted into the main drainage of Bidkhan catchment area over time. Width of this drainage has become extended because of mechanical weathering. Other main faults in Bidkhan area are also placed and observed in a direction similar to this valley fault. Total fracture networks created by main and minor faults allows for smooth movement of magmatic fluids. There is a severely altered integrated set of rocks in Bidkhan. Despite its youth, lithology and the events causing this set are remarkable. Important, various, and different events that have geochemical-geo- logical aspects occur with high density in this area. All kinds of alterations along with sulfide stock works, leachings, and supergenes are among these events. It is also noteworthy to mention the phenomena of hot springs that make travertine and are located in the vicinity of this area (outside of Bidkhan region). They are a part of these evidence collections [11] .

R₁, R₂ Plot (De La Roche 1980) diagram is adjusted according to the chemistry of these regional rocks (Figure 4). 30 analyzed samples, R₁ = 4Si − 11(Na + K) − 2(Fe + Ti) in the x-axes and R₂ = 6Ca + 2Mg + Al in y-axes were plotted on this diagram. These rocks were placed within three ranges of andesite, latite, dacite, and trachydacite with little differences, which is close to the observations for sections petrology.

On Harker diagram, main oxides were plotted against SiO₂. Valuable information can be gained from the changing trend of these oxides compared to SiO₂ increase. This diagram is presented in (Figure 5) and the following results were obtained:

1) Na₂O with a negative slope, decreases with the increase of SiO₂ and has a sharp (steep) slope. It was determined that generally in these three types of rocks, with the increase of silica, sodium is decreased. But more specifically, with the increase of silica, sodium is also increased with a gentle slope in each type.

2) K₂O can also be observed in three rock types of this diagram. This diagram demonstrates that andesitic rocks of this region do not show a significant change in the amount of potassium against the increase of SiO₂. But other rocks of this region show a decrease in potassium with a gentle slope from the increase of silica.

3) CaO decreases in relation to the increase of silica with a steep slope.

4) MgO shows the same decrease slope of calcium in respect to the increase of silica.

5) Al₂O₃ shows an overall decrease, which means aluminium decreases with the increase of silica. With a more careful examination, it is evident that increase exists in all the separate types of rocks for this region. Andesitic rocks demonstrate positive gentle slope and dacite rocks demonstrate a positive steep slope.

6) TiO₂ decreases with the increase of silica.

7) FeO or iron oxide also decreases with the increase of silica.

Therefore, it was concluded that even though the changing trends for main oxides of igneous rocks are somewhat linear and it actually shows magmatic differentiation in these rocks, factors such as alteration and magmatic contamination affected this trend (Table 1).

As it was observed in the diagrams of previous section, rocks of this region are in the range of sub-alkaline, which also tend to alkaline. After plotting the 30 samples on Miashiro 1974 diagram for SiO₂ on x and y axes, it was observed that almost all the samples are in the range of calc-alkaline series (Figure 6).

Studying AFM diagram, which is a triangular diagram, showed that Bidkhan rocks are among calc-alkaline series (Figure 7). On this diagram, A = (K₂O + Na₂O), F = FeO_t and M = MgO.

SiO₂-K₂O (Peccerillo & Taylor 1976) diagram divides the magmatic series of Bidkhan rocks into two series. Andesitic rocks are calc-alkaline and the other rocks of this region are in the range of the above potassic calc- alkaline series (Figure 8).

On A/CNK − A/NK Plot (Shand 1943) diagram, x-axes is A/NK = AL₂O₃/(Na₂O +K₂O) and y-axes is A/CNK = AL₂O₃/(CaO + Na₂O+K₂O). An examination of this diagram reveals that majority of these rocks are

in the range of metaluminous rocks and some of them are in the range of peraluminous rocks (Figure 9). According to microscopic evidences, it can be concluded that this high level of aluminum in the rocks is due to the argillization and increase of aluminum by alteration (Table 1).

Geotectonic diagrams, which are triangular diagrams by (Pearce et al. 1977), are an attempt to study the type of magmatism in relation to tectonic processes. According to this diagram, magma source for the rocks of this region was caused by orogenry. Based on the existing information and this diagram, this magma was caused by the subduction of the oceanic crust under the continental crust (Figure 10) and (Table 1).

Even in small quantities, the existence of azurite and malachite in an exploration area has significant exploratory value. The importance of malachite is not only due to being a remarkable mineral in exploration and foundation activities, but also mostly because of the importance of a process known as malachitization. Impacts of malachitization can be observed in many areas of Bidkhan. The analogous phenomena in the malachite outcrops of these regions is feldspar crystals that are converted into a set of secondary minerals such as sericite, illite, and other clay minerals and amphibole crystals are completely altered and their framework is filled up by malachite. There is also malachite within frameworks of some feldspar crystals. Secondary minerals of the outcrops from these regions consist of sericite, illite, clay minerals, malachite, apak, oxides-hydroxides of iron, chlorite, epidote and quartz (Figure 11) [12] .

The process for the formation of porous quartzes is a kind of alteration which is observed in Bidkhan along with geodes. In this kind of alteration, the empty space between quartz grains is partially filled with all kidns of minerals. This alteration is caused by the reaction between acidic fluids and the surrounding rocks and leads to the loss of the majority of constituents except for quartz and rutile parts. Places around alteration zones are the best location for observing porous quartzes. Many hand samples and also petrographic and mineralographic samples of Bidkhan region demonstrate alteration of quartz (porous). By moving from the region of alteration for porous quartz into the alteration region, many alterations such as quartz-alunite, quartz-kaolinite, and even perhaps pyrophyllite can be reached. Geodes are also valuable for exploratory studies along with the other evidences. Such geodes are also found in Bidkhan’s set. Alteration of porous quartz is usually created in the center and core of many ores and Au-Cu mineralization-with high sulphidation. In addition, these evidence can be observed in the upper parts of some porphyry ores and also in epithermal environments. Many traces of subsidence exist in Bidkhan and since faults play the main role in geological fluid dynamics, traces of subsidence are seen in fault zones. Since Bidkhan region has a significant density of main and secondary faults, almost all the central parts of Bidkhan bear traces of subsidence within themselves. These traces have different dimensions, from centimeters up to meters wide. The hand sample presented in the following figure shows pores that are caused by subsidence and are filled with silica, oxide, and iron hydroxides. Sometimes, these pores and cavities are also filled with malachite and azurite crystals (Figure 12).

1) Morphology of Bidkhan resembles a ring shape or a ring structure of huge dimensions with several tens of kilometers. This huge ring in the outside edge is very lofty, which is quickly converted into a foothill towards the central direction with a negative steep slope (Figure 13).

2) Based on the Ore-Mineral findings in Bidkhan region, it can be concluded that “erosion surface” includes the central part and is shaped like a ring around the central and upper part of leaching zone. Erosion surface is for all the surfaces of the central part of Bidkhan. By performing deep excavations, some parts could be reached in which minerals and other related and expected sets exist in the supergene zone (Figure 13).

3) Folds have an almost northwest-southeast trend. The impacts of these folds can mostly be seen on the parts that are outside the studied region of Bidkhan. Considering that this region is located in a way that its surrounding units are all folded symmetrically, it can be concluded that this symmetry is in accordance with positioning of an intrusive body (rocks) in the central section of Bidkhan. Due to the homogenous tension caused by this symmetrical uplift, folded surrounding units became symmetrical and they were folded in a dome shaped pattern. This dome shaped pattern folding can be observed across the heights surrounding the central part of Bidkhan (Figure 14).

4) Lithology of Bidkhan can be divided into 5 parts: Central part, middle volcaninc ring or belt, svsfacies, “unit C_g” external volcanogenic part, dykes and intrusive rocks and quartz deposits. C_g unit forms the heights of Bidkhan region. Heights are practically insurmountable due to their outward steep slope. C_g unit is extended in all directions and also extends to far distances from Bidkhan region. Based on the existing evidence, nomenclature of Bidkhan under the name of “Bidkhan’s Caldera” is a controversial subject. Simply existing the morphology similar to a caldera cannot be a good reason for this nomenclature. On the contrary, there are numerous evidences that make the caldera of Bidkhan ambiguous. C_g unit is not a Lahar but rather a conglomerate and a cutting, although, determination of this very subject also requires research and academic projects to be carried out. In addition to the common mechanism for the creation of caldera, there is a possibility that formation of dome shaped structure for Bidkhan is caused by uplift and positioning of an intrusive body. With this presump-

tion, the igneous outcrops existing in Bidkhan region can be considered the product of the same igneous source activities. According to the age of the available units in Bidkhan’s caldera and their method of deformation, it can be concluded that late alpine orogeny phases cause the creation of the current structural condition of Bidkhan region (Figure 14).

The authors thank Islamic Azad University South Tehran branch for support of this research. This paper presents the research project entitled “Rapture and Land Deformation Statistical Analysis for Earthquake along the Selected Active Fault in Central Iran” is extracted.

Ahmad Adib,Alireza Ashofteh, (2015) Studying Petrology and Determining Tectonic Setting of Bidkhan Area Southeast of Iran. Open Journal of Geology,05,677-688. doi: 10.4236/ojg.2015.510060