Petrology of Intrusive Bodies of Azizabad-Tinamo Area in the South of Songour, Iran

In terms of structural divisions of the Iran’s earth crust, the studied area is considered as a part of the Sanandaj-Sirjan structural zone and Zagros Thrust. In this area, there are two gabbroic-dioritic and syenitic igneous intrusive bodies. The host rocks of these intrusive bodies are upper Cretaceous limestones and formed by contactmetamorphism at the contact zone between hornfels rocks and skarn. Field and geochemical datasets represent that all various rocks within these intrusive bodies have been originated from the same magma. The process of fractional crystallization and probably a small amount of contamination and assimilation has also played a role in the evolution of parent magma. Generally, these magmas are sub-alkaline and lie in themagmatic range of tholeiitic and calc-alkaline series. Samples investigated are metaluminous and peralkaline.


Introduction
The studied area is located in the 1:100,000-scale geological map of Songour and the west of Iran (Figure 1).
The some parts of the stratigraphic units in the studied area belong to Sanandaj-Sirjan structural zone and other parts are related to Zagros Thrust Zone, which marked by the large fractures and multiple thrusts, and resulted to structural complexity of the area (Figure 2).This area, by the following of geological events in the area, was under the influence of different deformation phases whether orogenic or epeirogenic, the emplacement of intrusive bodies, metemorphism, and other geological events.Figure 2. Structural and sedimentary zones of Iran [2].
Given that the Sanandaj-Sirjan zone having NW-SE trending is parallel to the Zagros Thrust Faults, and by considering that this zone has severely affected by these faults activities in during different geological periods after the Cretaceous, as a result, in the area investigated the severe effects of tectonic activities could be well observed due to the proximity to the Main Zagros Fault.Among these features, it can be referred to thrust nappes, the presence of thrust faults with Quaternary age, regional metamorphism and intrusion of gabbroic to syenitic bodied and a small amount of granite.
The rocks cropping out in the studied area belong to the Mesozoic and Cenozoic era and the oldest of them is related to the Upper Cretaceous.These intrusions are Tertiary in age and have been injected in the upper Eocene-Oligocene due to the Pyrenean orogenic phase.
This study aims to determine the formation mechanism of gabbros, syenites and granites, discover the genetic relationship among the intrusive bodies of the region, and determine the change and frequency of major and trace elements in the rocks of the region.

Geological and Tectonic Setting
The area studied with coordinates of 47˚30' to 47˚40' east longitude and 34˚30' to 34˚40' north latitude is located in the southern part of 1:100,000 geological sheet of Songour and mountainous area with rough topography, and covers an area of over 280 square kilometers.The area of the intrusions outcrops in this region is about 25 square kilometers (Figures 3-5).Many faults in this area are of thrust or high angle reverse type, but there are less normal and strike-slip faults.One of the characteristics of the faults in the area is their seismicity so that until now several major earthquakes have been occurred in the region and caused the destruction of houses.Faults in the area are the valley-building.This means that the valleys and waterways have been created in trend of some faults due to slip, displacement and crushing caused by faulting and subsequent erosion.In the late Eocene and probably during the Pyrenean orogeny [3], governing compressive forces on the region along with other geological processes have caused to intrusion and emplacement of intrusive bodies in the studied area.Under the influence of the same orogenic phase, the contact metamorphism as well as metasomatism resulting from emplacement of intrusion have been occurred and caused the formation of skarn units in Deh Asyab and the position to form in the marble limestones in the studied area as well.This phase also resulted in folding and possibly faulting of the older units.

Petrology
According to 19 different type of rocks using ICP-MS and alkaline fusion technique the analysis (Table 1 and Table 2) and the geochemical diagrams of rocks nomenclature [4] and [5], most samples in the studied area would be fallen in the range of the gabbro, gabbro-diorite, diorite, monzonite, syenite, quartz monzonite and granite (Figure 6 and Figure 7).
In the diagram AFM [6], the samples would be fallen in both of tholeiitic and calcalkaline range.In the diagrams Na 2 O/SiO 2 [6], and K 2 O/SiO 2 [7], most samples are plotted in alkaline and sub-alkaline basalt fields.These diagrams represent an almost disorder linear trend for samples in the area studied.These disorders could be resulted from the crustal contamination of some intrusive magmas and increase in the amount of K 2 O within them, which of course does not reject the same origin of all magmas of   the area (Figures 8-10).
Based on the aluminum saturation diagram [8], 18 samples are in metaluminous and peralkaline fields.One example is in field of peraluminous, indicting the igneous origin of all the samples (Figure 11).SiO 2 , of course, higher Co content would be consumed within initial Mg-bearing minerals especially olivine.The scattered points on the diagrams are another evidence for the existence of the assimilation and magma mixing or only one of these two processes.
Cr would be removed from the magma as chromite mineral in the early stages of crystallization.Also, Cr would be accumulated in pyroxenes, especially the ultra-basic pyroxenes.Based on the diagram Cr vs. SiO 2 , Cr has more concentrated in four samples (normal) and two syenite samples (abnormal).This abnormal concentration could be resulted from the assimilation and magma mixing processes, of course, at the smallscale, because has created anomaly only in two samples.

Conclusion
According to petrographic and mineralogical studies of thin sections of rocks collected from the studied area, the intrusive igneous rocks in the region from basic to acidic terms include gabbro, gabbro-diorite, diorite, quartz-bearing syenodiorite, syenite, quartz-bearing syenite and granite, which gabbroic and syenitic rocks contain the largest volume in the area studied.The most studied samples are saturated with silica and in terms of the aluminum saturation are peralkaline and metaluminous.Generally, almost all the lithological and geochemical diagrams indicate a single source for these samples.It appears that the basaltic magma originated from the mantle, has intruded into the crust by weakness point of the crust namely the Zagros Main Thrust located in the south part of intrusive bodies.This magma has slightly fractionated in situ during solidification and this resulted in the formation of rocks from gabbro to syenite and granite, which of course, from the time of stopping until the magma has been cooled and solidified, the main basaltic intrusive (confirmed by large volume of gabbros) was able to contaminate with the crust and led to increase in some elements, such as potassium.In the Eocene and Oligocene magmatism of the Zagros Thrust and Sanandaj-Sirjan zones including the studied area, the cause of high compression by tensile and opening forces is acceptable.

Figure 8 .
Figure 8. Determination of magmatic series diagram using the major element oxides data [6].

Table 1 .
Chemical analysis of intrusive pluton in south of Songour.

Table 2 .
Chemical analysis of intrusive pluton in south of Songour.