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The study area is located in Jabal-Barez Ranges, southeastern part of Kerman Copper Belt (KCB), where the porphyry copper mineralization such as Kerver occurs. This article deals with the enhancement of hydrothermal alteration minerals for
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Download scientific diagram | Field photographs showing characteristics of Jebale Barez Plutonic complex (a) Outline of lithological units in the study area, (b) Porphyritic granite in the...
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The Jebal-e-Barez Plutonic Complex (JBPC) is located southeast of the UDMA and composed of quartz diorite, granodiorite, granite, and alkali granite. Magmatic enclaves, …
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The Jabal-Barez granitoid batholith is the major geological unit in Jabal-Barez Ranges (Fig. 2) that intruded the Eocene volcano-sedimentary rocks and is extensively exposed and covers an area of about 750 km2. According to previous studies such as [15], the Jabal-Barez batholith is related to the Late Eocene- ...
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The Darreh-Zereshk and Ali-Abad deposits are hosted by a series of Oligo-Miocene subvolcanic granitoid rocks and quartz monzodiorite (Zarasvandi et al., 2013) which have intruded into Mesozoic...
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Unlike the NKMA where the parent shallow intrusions and associated AC C porphyry-style mineralization are mainly hosted in Paleogene mafic-intermediate volcanic rocks, in the Jabal-Barez Ranges, the granitoid bodies are the main host to the porphyry systems.
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Unlike the NKMA where the parent shallow intrusions and associated AC C porphyry-style mineralization are mainly hosted in Paleogene mafic-intermediate volcanic rocks, in the Jabal …
WhatsApp: +86 18221755073
The Jabal-Barez granitoid batholith is the major geological unit in Jabal-Barez Ranges (Fig. 2) that intruded the Eocene volcano-sedimentary rocks and is extensively exposed and covers an area of about 750 km2. According to previous studies such as [15], the Jabal-Barez batholith is related to the Late Eocene-
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Jebal-e-Barez granitoids host the economic porphyry ores. Kuh-e-Panj granitoids link to weakly mineralized porphyry ores. Whole geochemical data are used to assess the petrogeochemical evolution and ore potentiality of different magmatic phases in the Kerman Cenozoic copper arc.
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In present study, we used new geochemical and Sr and Nd isotope data of both granitoid episodes (Kuh Panj and Jebal Barez) to identify their geochemical characteristics, and discus …
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Download scientific diagram | Field photographs showing characteristics of Jebale Barez Plutonic complex (a) Outline of lithological units in the study area, (b) Porphyritic granite in the...
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Magma has been percolated through Mijan caldera and emplacement Forms of Sill along the shear zone during various periods and the structural setting of granitoid complex in the Jebale-Barez is extensional-shear fractures which are the product of transpression tectonic regime.
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The quartz-rich phyllic alteration was derived from the effect of hydrothermal fluids on Jabal–Barez granite, and sericite phyllic alteration occurred in the quartz–monzonite and …
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The results indicate that silicarich rocks are found in the Jabal–Barez granitoid batholith and quartz- rich phyllic alteration zones, b results of Boolean logic integration for PCA results of sericite and silica-rich quartz that enhanced the quartzrich phyllic alteration zone in the SJBR. The results were draped on the ASTER band 4 image As ...
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Jebal-e-Barez granitoids host the economic porphyry ores. Kuh-e-Panj granitoids link to weakly mineralized porphyry ores. Whole geochemical data are used to assess the …
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In present study, we used new geochemical and Sr and Nd isotope data of both granitoid episodes (Kuh Panj and Jebal Barez) to identify their geochemical characteristics, and discus their possible magma sources.
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Introduction The Jebale-Barez Plutonic Complex (JBPC) is composed of many intrusive bodies and is located in the southeastern province of Kerman on the longitude of the 57 45 ' east to 58 00' and Northern latitudes 28 30' to 29 00'. The petrologic composition is composed of granodiorite, quartzdiorite, granite, alkali-granite, and trace amounts of tonalite with …
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Unlike the NKMA where the parent shallow intrusions and associated porphyry-style mineralization are mainly hosted in Paleogene mafic-intermediate volcanic rocks, in the Jabal-Barez Ranges, the granitoid bodies are the main host to the porphyry systems.
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Also a massive granitoid intrusion in NW of the studied area is detected by SAM method and color composite of 4,6,8 band of aster as a completely altered area ( SF area) which strongly recommend for more detailed exploration and field inspection. ... The study area is located in Jabal-Barez Ranges, southeastern part of Kerman Copper Belt (KCB ...
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The Jebal-e-Barez Plutonic Complex (JBPC) is located southeast of the UDMA and composed of quartz diorite, granodiorite, granite, and alkali granite. Magmatic enclaves, ranging in composition from felsic to mafic, are abundant in the studied rocks.
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According to global, regional and economic importance of Jabal Barez Red goat from the cashmir production aspect and role of Rheb gene on growth, cell cycle and cancer, expression of this gene was ...
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As comparison, barren intrusions (Jebal Barez granitoids) are characterized by Sr and Nd Isotopic Compositions The Kuh Panj granitoids show narrow range of relatively nonradiogenic 87Sr/86Sr ratio (0.7042530.704800) when compared with Jebal Barez granitoids (87Sr/86Sr=0. 705336-0.706810). 143Nd/144Ndratios of both granitoid types range from 0. ...
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The quartz-rich phyllic alteration was derived from the effect of hydrothermal fluids on Jabal–Barez granite, and sericite phyllic alteration occurred in the quartz–monzonite and granodiorite. Epidote occurred only along the Jabal–Barez faults, where Eocene volcanic rocks are outcropped.
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Abstract Jebale-Barez granitoid complex is composed of intrusive bodyes included Mijan, Dareh hamzeh, Kerver and Hishin and is located In the southeastern province of Kerman on the lengths of the ...
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The study area is located in Jabal-Barez Ranges, southeastern part of Kerman Copper Belt (KCB), where the porphyry copper mineralization such as Kerver occurs.
WhatsApp: +86 18221755073
Most of the volcanic arc granites (VAG) are of "pre-collision" and "syn- collision" types. Three magmatic phases occurred in oligomiocene in this area. The first phase of magmatism in this area...
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The Jabal-Barez ranges are distinguished by widespread Oligocene granitoid bodies, EP some of batholith sizes. Unlike the NKMA where the parent shallow intrusions and associated AC C porphyry-style mineralization are mainly hosted in Paleogene mafic-intermediate volcanic rocks, in the Jabal-Barez Ranges, the granitoid bodies are the main host ...
WhatsApp: +86 18221755073
Magma has been percolated through Mijan caldera and emplacement Forms of Sill along the shear zone during various periods and the structural setting of granitoid complex in the Jebale …
WhatsApp: +86 18221755073
The Darreh-Zereshk and Ali-Abad deposits are hosted by a series of Oligo-Miocene subvolcanic granitoid rocks and quartz monzodiorite (Zarasvandi et al., 2013) which have intruded into Mesozoic...
WhatsApp: +86 18221755073
Most of the volcanic arc granites (VAG) are of "pre-collision" and "syn- collision" types. Three magmatic phases occurred in oligomiocene in this area. The first phase of magmatism in this area...
WhatsApp: +86 18221755073
Geochemical studies, magmatic evolution, microstructures and replacement mechanisms in Jebale-Barez granitoid Complex,East and Southeast Jiroft (Persian with English abstract) August 2017 DOI: 10 ...
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Unlike the NKMA where the parent shallow intrusions and associated porphyry-style mineralization are mainly hosted in Paleogene mafic-intermediate volcanic rocks, in the Jabal …
WhatsApp: +86 18221755073
The study area is located in Jabal-Barez Ranges, southeastern part of Kerman Copper Belt (KCB), where the porphyry copper mineralization such as Kerver occurs. ... The Upper Triassic Siah-Kuh ...
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