Petrogenisis of Mafic- intermediate Magmatism, East of Sanandaj; A New approach with careful monitoring of geochemical evidences
The East Sanadaj magmatic rocks of the northern Sanandaj-Sirjan Zone, part of Zagros Orogen, comprise several intrusive bodies that were generated during northeastward subduction of Neo-tethys beneath the Iranian sector of the Eurasian plate. From the east Sanadaj to Galali, mafic- intermediate intr...
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| Format: | Article |
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University of Isfahan
2019-02-01
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| Series: | پترولوژی |
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| Online Access: | http://ijp.ui.ac.ir/article_23155_c1646561e37705bf2ab2e91c71c98481.pdf |
| _version_ | 1797722059967561728 |
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| author | Sanaz Yajam |
| author_facet | Sanaz Yajam |
| author_sort | Sanaz Yajam |
| collection | DOAJ |
| description | The East Sanadaj magmatic rocks of the northern Sanandaj-Sirjan Zone, part of Zagros Orogen, comprise several intrusive bodies that were generated during northeastward subduction of Neo-tethys beneath the Iranian sector of the Eurasian plate. From the east Sanadaj to Galali, mafic- intermediate intrusions of Late Jurassic age, have significant out crops in Kangareh, Saranjianeh, Ghorveh, Shanevareh and Galali. These rocks are calc-alkaline, metaluminous (ASI=0.51-0.95) and mostly magnesisan. As SiO2 increases, the chemistry of rocks changes to ferroan and high-K. These rocks present enrichment of LILE relative to HFSE, the low LREE/HREE fractionation ((La/Lu)N=1.5-14.6) considerably flatter chondrite-normalized REE profiles, Eu positive anomaly (Eu/Eu*= +0.63-+3.75). Primitive features of Sr - Nd isotopes Combined with HFSE and REE ratios, as source indicators, prove the mantle derived magma as a source of these rocks. Geochemical modelings indicate mafic- intermediate rocks of east Sanadaj, originated from spinel lherzolithic magma with hydrous components such as amphibole. Fractionation of these hydrous minerals have important role in evolution of magma. The combined monitoring of geochemical data and REE patterns, isotopic data were performed in order to unravel the compositional changes from calc-alkaline-magnesisn rocks to high alkaline-ferroan rocks of this area. The results denied bimodality of source magma and confirmed the important role of differentiation in magma evolution. |
| first_indexed | 2024-03-12T09:42:04Z |
| format | Article |
| id | doaj.art-697e7b431d7042c781393b0d42f6e715 |
| institution | Directory Open Access Journal |
| issn | 2228-5210 2322-2182 |
| language | fas |
| last_indexed | 2024-03-12T09:42:04Z |
| publishDate | 2019-02-01 |
| publisher | University of Isfahan |
| record_format | Article |
| series | پترولوژی |
| spelling | doaj.art-697e7b431d7042c781393b0d42f6e7152023-09-02T13:07:47ZfasUniversity of Isfahanپترولوژی2228-52102322-21822019-02-019411113210.22108/ijp.2018.110126.108023155Petrogenisis of Mafic- intermediate Magmatism, East of Sanandaj; A New approach with careful monitoring of geochemical evidencesSanaz Yajam0Department of Geology, Payame Noor University, 19395-3697 Tehran, I. R. of IranThe East Sanadaj magmatic rocks of the northern Sanandaj-Sirjan Zone, part of Zagros Orogen, comprise several intrusive bodies that were generated during northeastward subduction of Neo-tethys beneath the Iranian sector of the Eurasian plate. From the east Sanadaj to Galali, mafic- intermediate intrusions of Late Jurassic age, have significant out crops in Kangareh, Saranjianeh, Ghorveh, Shanevareh and Galali. These rocks are calc-alkaline, metaluminous (ASI=0.51-0.95) and mostly magnesisan. As SiO2 increases, the chemistry of rocks changes to ferroan and high-K. These rocks present enrichment of LILE relative to HFSE, the low LREE/HREE fractionation ((La/Lu)N=1.5-14.6) considerably flatter chondrite-normalized REE profiles, Eu positive anomaly (Eu/Eu*= +0.63-+3.75). Primitive features of Sr - Nd isotopes Combined with HFSE and REE ratios, as source indicators, prove the mantle derived magma as a source of these rocks. Geochemical modelings indicate mafic- intermediate rocks of east Sanadaj, originated from spinel lherzolithic magma with hydrous components such as amphibole. Fractionation of these hydrous minerals have important role in evolution of magma. The combined monitoring of geochemical data and REE patterns, isotopic data were performed in order to unravel the compositional changes from calc-alkaline-magnesisn rocks to high alkaline-ferroan rocks of this area. The results denied bimodality of source magma and confirmed the important role of differentiation in magma evolution.http://ijp.ui.ac.ir/article_23155_c1646561e37705bf2ab2e91c71c98481.pdfmafic magmatismgeochemistryreend-sr isotopespetrogenesiseast of sanandajsanandaj-sirjan zone |
| spellingShingle | Sanaz Yajam Petrogenisis of Mafic- intermediate Magmatism, East of Sanandaj; A New approach with careful monitoring of geochemical evidences پترولوژی mafic magmatism geochemistry ree nd-sr isotopes petrogenesis east of sanandaj sanandaj-sirjan zone |
| title | Petrogenisis of Mafic- intermediate Magmatism, East of Sanandaj;
A New approach with careful monitoring of geochemical evidences |
| title_full | Petrogenisis of Mafic- intermediate Magmatism, East of Sanandaj;
A New approach with careful monitoring of geochemical evidences |
| title_fullStr | Petrogenisis of Mafic- intermediate Magmatism, East of Sanandaj;
A New approach with careful monitoring of geochemical evidences |
| title_full_unstemmed | Petrogenisis of Mafic- intermediate Magmatism, East of Sanandaj;
A New approach with careful monitoring of geochemical evidences |
| title_short | Petrogenisis of Mafic- intermediate Magmatism, East of Sanandaj;
A New approach with careful monitoring of geochemical evidences |
| title_sort | petrogenisis of mafic intermediate magmatism east of sanandaj a new approach with careful monitoring of geochemical evidences |
| topic | mafic magmatism geochemistry ree nd-sr isotopes petrogenesis east of sanandaj sanandaj-sirjan zone |
| url | http://ijp.ui.ac.ir/article_23155_c1646561e37705bf2ab2e91c71c98481.pdf |
| work_keys_str_mv | AT sanazyajam petrogenisisofmaficintermediatemagmatismeastofsanandajanewapproachwithcarefulmonitoringofgeochemicalevidences |