Fluorine Qhrabad Kurdistan region

States KORDESTAN
Author Mansour Samimi Namin
Published At 14 March 1973

Summary

Qhrabad at 32 km (straight line) south east of turpentine placed way - from Chapan located 30 km turpentine (d Rjadh asphalt turpentine Court valley) towards the south branch is (this road well too Sanandaj goes) after over 10 km in the supernatant of road machinery road towards the left hand, which is split after passing through Castle Valley Tvfy Abad Yhay votes to reach Qhrabad. Last road section which is not a good situation and is 12 miles Qhrabad Last Abadi is my road car it ends be.

Description

Introduction: Mr. President, while proud of Mahabad Drnahyh geological studies and especially border line between de Rmtalat square and rectangle Tkat Map 300 meters south of Mahabad Abad Abadi angry vessels of fluorine thickness approximately 5 / 1 m were treated. Like crystals rather The large green fluorine attention from local residents were Abadi streak that was the symbol is about 5 / 1 meter automatically block level and also Drtqyb geological studies around the mountain springs, while forty Talk Bayd Alyjan residents and adjacent villages or similar works Zvjvd Ten Dratraf themselves are driven. because Mr. proud race time due to stenosis could not exactly place the symbol of fluorine and also other places that local people come around Abadi Alyjan crystals have the same extravagance are seeing so far immediately and studies next steps to build and study reports and prosecutions related to fluorine and Mynralzasyvn de Rick limited area in accordance with a specific plan has been Andkhvastar. within the area recommended by Mr honor under race is shown in Figure 1. The area southeast part square of Mahabad and southwest and northwest Chha Rgvsh Takab Sanandaj and northwest quadrangles quadrangles Marivan is included. except that the rectangle part Marivan Other sections respectively in the number one map (scale 1:100000) has been shown by Messrs. Aftkharnzhad - Alavi Naien Vzahdy has been studied. Mamvrt before the gentlemen geologists call groups and geological data collected from the area required Nmvdm Now what geological information is included in the report related to the gentlemen geologists are. After reaching Abadi Abadi Dhban Qhrabad the information that is likely four to five months after the loss was covered in snow in 1350 while de Rtph a shepherd immediately south of Abadan angry piece of stone that look like glass and color glass or water Khvshrngy had treated and brought to Abadan. people imagined that one of these stone jewelry Vqymty has been poured and all the hills, where the main block and coarse crystals and blue together Khvshrng And to have collected at their homes. (Angry Abad village de Rhr home a few pieces of crystal, fluorine has been collected.) Discovered gemstone Rnzdyk de Abad village wrath are common in neighboring villages so that later I presented examples of people fluorine Rural stone there so I used to answer questions were the type of stone that is found near Qhrabad. Geological area Fluorine and the surrounding area with all schist metamorphic rocks and sand by Rgchh cut quartz and limestone and dolomite are often Andtshkyl has been Mrmryz·h. Schist parts are mountainous areas because post de Rmqabl atmospheric erosion compared with limestone and dolomite are softer. highlands area and dolomitic lime and limestones have formed. streaks in the south Abadi Qhrabad fluorine at the top of the heights and dolomitic limestone located. age of lime is not completely clear, but some of the limestone deposits in the northern highlands and Southern region has been diagnosed shall Cretaceous. metamorphic rocks of the age are attributable to Cambrian Shysthabh blade. within schist and dolomite Azahk usually a lot of lenses, some have been completely transformed, perhaps there is some age, they are one with the Shysthay. parts Map No. 1 and granite are that age it has been referred to the Cretaceous.   Fluorine vein Qhrabad Qhrabad at 32 km (straight line) south east of turpentine placed way - from Chapan located 30 km turpentine (d Rjadh asphalt turpentine Court valley) towards the south branch is (this road well too Sanandaj goes) after over 10 km in the supernatant of road machinery road towards the left hand, which is split after passing through Castle Valley Tvfy Abad Yhay votes to reach Qhrabad. Last road section which is not a good situation and is 12 miles Qhrabad Last Abadi is my road car it ends be. Fluorine vein in the hills with the relative height of approximately 100 m de Rjnvb Qhrabad village which automatically Kshbdh East West and its material is limestone and dolomite, has been formed. Along the east-west, but few classes together and eaten in two adjacent valleys Qhrabad limestones that breaks its slope is nearly vertical. Abadi away with horizontal streaks is about 300 Mtrmy. Chahy form fluorine vein location and depth of one meter Qtrtqryba replica. Bottom of the well due to rainfall and soil is covered cast. Streaks as real surface manifestation Nd Arend and not even 4 meters in length, for example veins follow   Be. Upwards on a hill in the soils in the seam Vshkaf limestone blocks were tiny particles of fluorine had been broadcast. Although the streak does not continue with the same initial conditions, but certainly in the gaps Dygrahk also have non-fluorine since the block has been formed . a fully along the northwest and southeast over about 50 meters from the effects of fluorine were followed up avulsion. local said that from this point of the hill there is fluorine. but due to the fact that on this place before license had been informed organization . So much searching, this was done about its significance. However, fluorine in the form of lime is not completely clear, but if some level of operation will be done was clear the situation. Fluorine crystals or red white or blue glass is Khvshrng. Good samples have also collected a few pieces of fluorine from the Sandy soils around the wells and multi-sample of local people to the museum were collected. No samples with fluorine Mynralyzasyvn metal was observed, and even materials such as quartz or barite, which often is associated with veins of fluorine did not exist. Just contact surface fluorine with lime seeds from planning Kalsyt there. Seemed that fluorine alternative in the form of lime has been. Grddaya known for being very fine crystals fluorine Drahk distributed or not attached to a sample of limestone was studied by fluorine. and the results annum as follows: Petrology studies by Mr. Brbryan exactly the same results in harvest. in other parts of the hill any type silicic veins was observed, but few on the hill Pydashd quartz crystal. (a big one cm) and net short Khvshrng fluorine in the hills south Abadi Qhrabad Azaynk·h been formed and exactly what is needed to form surface exploration operations deep and has an idea to be obtained from the stored value. Other areas visited So that part of the geological rocks were formed from parts of words that are Shysthay blade Cambrian limestone and dolomite lenses Mrmryz·h been due to elevations formed Skhtyshan Andvtph Abadi Qhrabad south of the fluorine has been formed of one block is limestone.  

tags: KORDESTAN