Zircon U–Pb geochronology, Hf isotopes and geochemistry of intrusive rocks in the Gazu copper deposit, Iran: Petrogenesis and geological implications Article Swipe
Amir Mahdavi
,
Mohammad Hassan Karimpour
,
Jingwen Mao
,
Mohammad Reza Haidarian Shahri
,
Azadeh Malekzadeh Shafaroudi
,
Hongying Li
·
YOU?
·
· 2015
· Open Access
·
· DOI: https://doi.org/10.1016/j.oregeorev.2015.09.011
YOU?
·
· 2015
· Open Access
·
· DOI: https://doi.org/10.1016/j.oregeorev.2015.09.011
The Gazu Cu deposit is located at the boundary between the Lut and Tabas Blocks in Central Iranian Microcontinent. The intrusions in the Gazu area are characterized by SiO2 contents ranging from 52.6 to 66.4 wt.%, K2O from 1.98 to 3.64 wt.%, and Na2O from 2.5 to 5.2 wt.%. The intrusions have features typical of high-K calc-alkaline rocks, are metaluminous to weakly peraluminous, and formed in a volcanic arc setting. Zircon U–Pb age data for hornblende monzonite porphyry, hornblende monzodiorite porphyry, pyroxene monzonite, hornblende granite, hornblende quartz monzonite porphyry, and hornblende diorite porphyry are 68.1 ± 1.7 Ma, 67.74 ± 0.72 Ma, 67.41 ± 0.94 Ma, 65.9 ± 3.7 Ma, 65.1 ± 1.2 Ma, and 60.2 ± 1.2 Ma, respectively. Copper mineralization is related to the hornblende granite and hornblende quartz monzonite porphyry. Field observations and the U–Pb dating indicated three stages for intrusive rock emplacement: pre-mineralization intrusions (hornblende monzonite porphyry, hornblende monzodiorite porphyry, and pyroxene monzonite), syn-mineralization intrusions (hornblende granite and hornblende quartz monzonite porphyry), and post-mineralization intrusions (hornblende diorite porphyry). Mantle-normalized, trace-element spider diagrams display enrichment in large ion lithophile elements, such as Rb, Ba, K, and Cs, and depletion in high field strength elements, e.g., Nb, Ti, Zr, Y, and heavy rare earth elements, with light rare earth element enrichment ((La/Yb)N = 6.4–13.4) and a weak negative Eu anomaly (Eu/Eu* = 0.87–1.01). Zircon Hf isotope data indicate that the Gazu intrusive rocks are characterized by low positive εHf(t) values, with an average of 4.23, and show young Hf model ages (789–188 Ma), indicating derivation from juvenile crust. Relatively low positive εHf(t) values, the wide range for εHf(t), and the presence of zircon xenocrysts can be explained by involvement of a mantle component that mixed with older continental crust (Cadomian).
Related Topics
Concepts
Quartz monzonite
Hornblende
Geology
Geochemistry
Diorite
Zircon
Geochronology
Petrogenesis
Porphyry copper deposit
Petrology
Pluton
Mantle (geology)
Quartz
Fluid inclusions
Biotite
Tectonics
Paleontology
Metadata
- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.1016/j.oregeorev.2015.09.011
- OA Status
- hybrid
- Cited By
- 13
- References
- 113
- Related Works
- 10
- OpenAlex ID
- https://openalex.org/W2103623054
All OpenAlex metadata
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- OpenAlex ID
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https://openalex.org/W2103623054Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.1016/j.oregeorev.2015.09.011Digital Object Identifier
- Title
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Zircon U–Pb geochronology, Hf isotopes and geochemistry of intrusive rocks in the Gazu copper deposit, Iran: Petrogenesis and geological implicationsWork title
- Type
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articleOpenAlex work type
- Language
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enPrimary language
- Publication year
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2015Year of publication
- Publication date
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2015-09-16Full publication date if available
- Authors
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Amir Mahdavi, Mohammad Hassan Karimpour, Jingwen Mao, Mohammad Reza Haidarian Shahri, Azadeh Malekzadeh Shafaroudi, Hongying LiList of authors in order
- Landing page
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https://doi.org/10.1016/j.oregeorev.2015.09.011Publisher landing page
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YesWhether a free full text is available
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hybridOpen access status per OpenAlex
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https://doi.org/10.1016/j.oregeorev.2015.09.011Direct OA link when available
- Concepts
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Quartz monzonite, Hornblende, Geology, Geochemistry, Diorite, Zircon, Geochronology, Petrogenesis, Porphyry copper deposit, Petrology, Pluton, Mantle (geology), Quartz, Fluid inclusions, Biotite, Tectonics, PaleontologyTop concepts (fields/topics) attached by OpenAlex
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13Total citation count in OpenAlex
- Citations by year (recent)
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2025: 1, 2023: 1, 2022: 2, 2021: 1, 2020: 1Per-year citation counts (last 5 years)
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113Number of works referenced by this work
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10Other works algorithmically related by OpenAlex
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