Petrography and geochemistry of igneous rocks and Sb and Au mineralization in Sefidsang and Dargiaban areas, southeastern Iran

Abstract: The Sefidsang and Dargiaban areas are located in the Sistan suture zone. The geological units of the areas are flysch-like rocks, granitoid body, subvolcanic mass, acidic and intermediate dikes and recent deposit. The igneous rocks are granite, micro-granite, granodiorite, granodiorite por...

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Main Authors: Mohammad Boomeri, halimeh mojadadi moghadam, Habib Biabangard
Format: Article
Language:fas
Published: University of Isfahan 2018-11-01
Series:پترولوژی
Subjects:
Online Access:http://ijp.ui.ac.ir/article_23559_6dc7dbcf39b55ba13c597eb1a0c67be2.pdf
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author Mohammad Boomeri
halimeh mojadadi moghadam
Habib Biabangard
author_facet Mohammad Boomeri
halimeh mojadadi moghadam
Habib Biabangard
author_sort Mohammad Boomeri
collection DOAJ
description Abstract: The Sefidsang and Dargiaban areas are located in the Sistan suture zone. The geological units of the areas are flysch-like rocks, granitoid body, subvolcanic mass, acidic and intermediate dikes and recent deposit. The igneous rocks are granite, micro-granite, granodiorite, granodiorite porphyry and diorite porphyry. The phyllic and propylitic alterations observe with subvolcanic mass and argillic alteration occurs around the mineralized silicic veins. The important mineralization in the area is epithermal type quartz-stibnite veins. The phyllic and propylitic alterations and Cu, Pb and Zn anomalies associated with the subvolcanic rocks in the area are probably indication of a porphyry mineralization system. The Sefidsang granite is an S-type granitoid while the Dargiaban granite is an I-type granitoid and both of them are peraluminous. The igneous rocks are mainly calc-alkaline in magmatic series. Tectonic setting of the igneous rocks in the Dargiaban and Sefidsang is related to convergent zones and similar to those of the subduction, collisional and post-collisional environments. The S-type granite and microgranitic dikes were generated from partial melting of metagreywackes and subvolcanic bodies and intermediate dikes were generated from partial melting of amphibolite. The chondrite-normalized and primitive-normalized diagrams show the igneous rocks are characterized by LREE and LILE enrichment relative to HREE and HFSE. The enrichment of Th, Rb, K and Pb and the depletion of Zr, Ti and Nb are more consistent with melts generated from the metasomatized mantle and lower crust.
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spelling doaj.art-6c77bc4d8da449b387f8c4896682ca242023-08-02T02:10:16ZfasUniversity of Isfahanپترولوژی2228-52102322-21822018-11-019319321610.22108/ijp.2018.110097.107723559Petrography and geochemistry of igneous rocks and Sb and Au mineralization in Sefidsang and Dargiaban areas, southeastern IranMohammad Boomeri0halimeh mojadadi moghadam1Habib Biabangard2Acadimic member of Geology department, Sciences college , University of Sistan and Baluchestanph.D student of Geochemistry/ Geology, Faculty of Science,University of Sistan and Baluchestan, Zahedan, IranAcademic member of Department of Geology, Faculty of Sciences, University of Sistan and Baluchestan, Zahedan, IranAbstract: The Sefidsang and Dargiaban areas are located in the Sistan suture zone. The geological units of the areas are flysch-like rocks, granitoid body, subvolcanic mass, acidic and intermediate dikes and recent deposit. The igneous rocks are granite, micro-granite, granodiorite, granodiorite porphyry and diorite porphyry. The phyllic and propylitic alterations observe with subvolcanic mass and argillic alteration occurs around the mineralized silicic veins. The important mineralization in the area is epithermal type quartz-stibnite veins. The phyllic and propylitic alterations and Cu, Pb and Zn anomalies associated with the subvolcanic rocks in the area are probably indication of a porphyry mineralization system. The Sefidsang granite is an S-type granitoid while the Dargiaban granite is an I-type granitoid and both of them are peraluminous. The igneous rocks are mainly calc-alkaline in magmatic series. Tectonic setting of the igneous rocks in the Dargiaban and Sefidsang is related to convergent zones and similar to those of the subduction, collisional and post-collisional environments. The S-type granite and microgranitic dikes were generated from partial melting of metagreywackes and subvolcanic bodies and intermediate dikes were generated from partial melting of amphibolite. The chondrite-normalized and primitive-normalized diagrams show the igneous rocks are characterized by LREE and LILE enrichment relative to HREE and HFSE. The enrichment of Th, Rb, K and Pb and the depletion of Zr, Ti and Nb are more consistent with melts generated from the metasomatized mantle and lower crust.http://ijp.ui.ac.ir/article_23559_6dc7dbcf39b55ba13c597eb1a0c67be2.pdfsb mineralizationsubvolcanic igneous rockszahedan granitoidsistan suture zone
spellingShingle Mohammad Boomeri
halimeh mojadadi moghadam
Habib Biabangard
Petrography and geochemistry of igneous rocks and Sb and Au mineralization in Sefidsang and Dargiaban areas, southeastern Iran
پترولوژی
sb mineralization
subvolcanic igneous rocks
zahedan granitoid
sistan suture zone
title Petrography and geochemistry of igneous rocks and Sb and Au mineralization in Sefidsang and Dargiaban areas, southeastern Iran
title_full Petrography and geochemistry of igneous rocks and Sb and Au mineralization in Sefidsang and Dargiaban areas, southeastern Iran
title_fullStr Petrography and geochemistry of igneous rocks and Sb and Au mineralization in Sefidsang and Dargiaban areas, southeastern Iran
title_full_unstemmed Petrography and geochemistry of igneous rocks and Sb and Au mineralization in Sefidsang and Dargiaban areas, southeastern Iran
title_short Petrography and geochemistry of igneous rocks and Sb and Au mineralization in Sefidsang and Dargiaban areas, southeastern Iran
title_sort petrography and geochemistry of igneous rocks and sb and au mineralization in sefidsang and dargiaban areas southeastern iran
topic sb mineralization
subvolcanic igneous rocks
zahedan granitoid
sistan suture zone
url http://ijp.ui.ac.ir/article_23559_6dc7dbcf39b55ba13c597eb1a0c67be2.pdf
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