Study of iron mineralization in Tekieh Bala iron index, based on mineralogical and geochemical evidence
Abstract The Tekieh Bala iron index is located in the south east of Kordestan province in Sanandaj- Sirjan geotectonic zone. Exposed rocks at the study area are including granite, gabbro, diorite, quartzmonzonite, quartzmonzodiorite and actinolite schist to chlorite schist.Orebody is located in the...
Main Authors: | , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | Persian |
Published: |
University of Isfahan
2018
|
Subjects: | |
Online Access: | https://doi.org/10.22108/ijp.2017.81995.0 https://doaj.org/article/7895352b50be4805a2e6a3d239234dca |
id |
ftdoajarticles:oai:doaj.org/article:7895352b50be4805a2e6a3d239234dca |
---|---|
record_format |
openpolar |
spelling |
ftdoajarticles:oai:doaj.org/article:7895352b50be4805a2e6a3d239234dca 2023-10-01T03:57:11+02:00 Study of iron mineralization in Tekieh Bala iron index, based on mineralogical and geochemical evidence Mehrdad Barati Zahra Ghilzar Khojasteh meisam Gholipoor 2018-01-01T00:00:00Z https://doi.org/10.22108/ijp.2017.81995.0 https://doaj.org/article/7895352b50be4805a2e6a3d239234dca FA per University of Isfahan http://ijp.ui.ac.ir/article_22468_a8f17d867753d2fd42481c615c2871c1.pdf https://doaj.org/toc/2228-5210 https://doaj.org/toc/2322-2182 2228-5210 2322-2182 doi:10.22108/ijp.2017.81995.0 https://doaj.org/article/7895352b50be4805a2e6a3d239234dca پترولوژی, Vol 8, Iss 32, Pp 167-196 (2018) Tekieh Bala Kordestan province Schist Magnetite Kiruna-type Petrology QE420-499 article 2018 ftdoajarticles https://doi.org/10.22108/ijp.2017.81995.0 2023-09-03T00:43:01Z Abstract The Tekieh Bala iron index is located in the south east of Kordestan province in Sanandaj- Sirjan geotectonic zone. Exposed rocks at the study area are including granite, gabbro, diorite, quartzmonzonite, quartzmonzodiorite and actinolite schist to chlorite schist.Orebody is located in the fault-beratited zone. Magnetite, hematite, goethite, limonite and pyrite included iron minerals in this index. Epidotization, chloritization, sericitization, actinolitization and silicification are the main alteration around the orebody. Geochemical studies of major and trace elements from the magnetite ore and use of diagrams provided by the various researchers shows that this index placed in group of iron oxide deposits, IOA sub-type and IOCG-type. REE Studies have shown, patterns of these elements, and calculated differential parameters emphasize the similarity of this deposit and IOA-type. Ore forming fluids were formed in differentiation and crystalization of intermediate intrusions rocks as a iron-rich hydrothermal fluids, mixing with the meteoric waters has been led to change in the environmental conditions and deposition of orebody. Article in Journal/Newspaper Kiruna Directory of Open Access Journals: DOAJ Articles Kiruna Bala ENVELOPE(132.817,132.817,67.178,67.178) |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
Persian |
topic |
Tekieh Bala Kordestan province Schist Magnetite Kiruna-type Petrology QE420-499 |
spellingShingle |
Tekieh Bala Kordestan province Schist Magnetite Kiruna-type Petrology QE420-499 Mehrdad Barati Zahra Ghilzar Khojasteh meisam Gholipoor Study of iron mineralization in Tekieh Bala iron index, based on mineralogical and geochemical evidence |
topic_facet |
Tekieh Bala Kordestan province Schist Magnetite Kiruna-type Petrology QE420-499 |
description |
Abstract The Tekieh Bala iron index is located in the south east of Kordestan province in Sanandaj- Sirjan geotectonic zone. Exposed rocks at the study area are including granite, gabbro, diorite, quartzmonzonite, quartzmonzodiorite and actinolite schist to chlorite schist.Orebody is located in the fault-beratited zone. Magnetite, hematite, goethite, limonite and pyrite included iron minerals in this index. Epidotization, chloritization, sericitization, actinolitization and silicification are the main alteration around the orebody. Geochemical studies of major and trace elements from the magnetite ore and use of diagrams provided by the various researchers shows that this index placed in group of iron oxide deposits, IOA sub-type and IOCG-type. REE Studies have shown, patterns of these elements, and calculated differential parameters emphasize the similarity of this deposit and IOA-type. Ore forming fluids were formed in differentiation and crystalization of intermediate intrusions rocks as a iron-rich hydrothermal fluids, mixing with the meteoric waters has been led to change in the environmental conditions and deposition of orebody. |
format |
Article in Journal/Newspaper |
author |
Mehrdad Barati Zahra Ghilzar Khojasteh meisam Gholipoor |
author_facet |
Mehrdad Barati Zahra Ghilzar Khojasteh meisam Gholipoor |
author_sort |
Mehrdad Barati |
title |
Study of iron mineralization in Tekieh Bala iron index, based on mineralogical and geochemical evidence |
title_short |
Study of iron mineralization in Tekieh Bala iron index, based on mineralogical and geochemical evidence |
title_full |
Study of iron mineralization in Tekieh Bala iron index, based on mineralogical and geochemical evidence |
title_fullStr |
Study of iron mineralization in Tekieh Bala iron index, based on mineralogical and geochemical evidence |
title_full_unstemmed |
Study of iron mineralization in Tekieh Bala iron index, based on mineralogical and geochemical evidence |
title_sort |
study of iron mineralization in tekieh bala iron index, based on mineralogical and geochemical evidence |
publisher |
University of Isfahan |
publishDate |
2018 |
url |
https://doi.org/10.22108/ijp.2017.81995.0 https://doaj.org/article/7895352b50be4805a2e6a3d239234dca |
long_lat |
ENVELOPE(132.817,132.817,67.178,67.178) |
geographic |
Kiruna Bala |
geographic_facet |
Kiruna Bala |
genre |
Kiruna |
genre_facet |
Kiruna |
op_source |
پترولوژی, Vol 8, Iss 32, Pp 167-196 (2018) |
op_relation |
http://ijp.ui.ac.ir/article_22468_a8f17d867753d2fd42481c615c2871c1.pdf https://doaj.org/toc/2228-5210 https://doaj.org/toc/2322-2182 2228-5210 2322-2182 doi:10.22108/ijp.2017.81995.0 https://doaj.org/article/7895352b50be4805a2e6a3d239234dca |
op_doi |
https://doi.org/10.22108/ijp.2017.81995.0 |
_version_ |
1778528223117705216 |