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 ...
Introduction The Jebale-Barez Plutonic Complex (JBPC) is composed of many intrusive bodies and is located in the southeastern province of Kerman on the lo... Geochemical studies, magmatic evolution, microstructures and replacement mechanisms in Jebale-Barez granitoid Complex (East and Southeast Jiroft)
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 ...
jamal.rasouli1362@gmail :تﺎﺒﺗﺎﮑﻣ لوﺆﺴﻣ* DOI: 10.22067/econg.v9i1.47949 يدﺎﺼﺘﻗا ﯽﺳﺎﻨﺷﻦﯿﻣز ﻪﻠﺠﻣ (1396 لﺎﺳ) 1 هرﺎﻤﺷ ،9 ...
Comparison of hydrothermal alteration patterns associated with porphyry Cu deposits hosted by granitoids and intermediate-mafic volcanic rocks, Kerman Magmatic Arc, Iran: Application of geological, mineralogical and remote sensing data - ScienceDirect.
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
PDF | Abstract Jebale-Barez granitoid complex is composed of intrusive bodyes included Mijan, Dareh hamzeh, Kerver and Hishin and is located In... | Find, read …
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. ... Andesite – basalt, granitoid ...
Geochemical studies, magmatic evolution, microstructures and replacement mechanisms in Jebale-Barez granitoid Complex,East and Southeast Jiroft (Persian …
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.
Introduction The Jebale-Barez Plutonic Complex (JBPC) is composed of many intrusive bodies and is located in the southeastern province of Kerman on the lo...
The southern part of this belt, in the Jebal-Barez area, has been less investigated due to the mountainous and rough topography as well as some security. The Urumieh-Dokhtar Magmatic Belt (UDMB) is the host of …
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 … See more
The Jabal-Barez ranges are distinguished by widespread Oligocene granitoid bodies, some of batholith sizes. 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 …
granitoid jabal barez - nailsbykaty.ch. 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 … read more
granitoid jabal barez. Jebal Barez type granitoid The younger Jabal Barez and Kuh Panj type granitoids are added dotted areas after Shafiei et al 2009 to show compositional variations through time Normalization values from McDonough and Sun 1995 and Sun and McDonough 1989 respectively . #
The Jebal-e-Barez type granitoids mark the first phase of economic porphyry copper deposits (Sarcheshmeh and Meiduk). These granitoids and the Eocene volcanic …
The younger Jabal Barez and Kuh Panj-type granitoids are added (dotted areas, after Shafiei et al., 2009) to show compositional variations through time. …
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 exploration of porphyry Cu mineralization, and differentiates intense hydrothermal alteration zones ...
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 … read more. Read More
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Both adakitic and A-type granitoid have been recently identified in the southern ANS. The Emba-Derho and Koka granitoids yielded the same zircon U–Pb ages of 851 ± 14 Ma and 851 ± 2 Ma, respectively. The Emba-Derho granitoids show high and a narrow range of SiO2 (71.3–73.6 wt.%) and Al2O3 (14.9–15.9 wt.%) contents, but …
کمپلکس گرانیتوئیدی جبال بارز در جنوبشرق استان کرمان، بین طولهای شرقی ′45 57 تا ′00 58 و عرضهای شمالی ′30 28 تا ′00 29 واقع شده است. در این کمپلکس، پیکره اصلی سنگ شناسی شامل گرانودیوریت بوده؛ ولی سنگهایی با ترکیب ...
The Arabian-Nubian Shield (ANS) is an accretionary orogen at the northern part (present-day coordinates) of the East African Orogen (EAO) (Fig. 23.1) which formed in Tonian (1000–850 Ma) and Cryogenian (850–650 Ma) times accompanying terrane accretion around the Mozambique Ocean (Stern 1994, 2002).Taking in consideration …
Petrochemistry of the Siah-Kuh granitoid stock southwest of Kerman, Iran: Implications for initiation of Neotethys subduction. M Arvin, Y Pan, S Dargahi, A Malekizadeh, A Babaei ... of mixture tuned matched filtering on ASTER data for hydrothermal alteration mapping related to porphyry cu deposits in Jabal-Barez Ranges, Kerman Copper Belt, Iran.
granitoid jabal barezThe Pennefather vibrating Equipment european region brochure english 445 kb. granitoid jabal barez. Mineralogy petrology and geochemistry of mafic dikes in Abstract In the southeastern part of the Jebal-E-Barez Oligocene granitoids (Kerman province Iran) there are numerous mafic dikes and this work attempts to …
granitoid complex in the Jebale-Barez is extensional-shear fractures which are the product of transpression tectonic regime. Discussion The JBPC is calc-alkaline, high-K, subalkaline, and mostly metaluminous except granite and alkali-granite units which are slightly peraluminous and I type in character. ...
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 Eu/Eu* of granitoids from the Kerman belt are greater than 1.2, representing the oxidizing conditions for the crystallization of the granitoid magma, whereas Jebal Barez granitoids were formed ...
Geochemical studies, magmatic evolution, microstructures and replacement mechanisms in Jebale-Barez granitoid Complex (East and Southeast Jiroft) Jamal Rasouli, Mansour Ghorbani, Vahid Ahadnejad; Affiliations Jamal Rasouli Department of Geology, Faculty of Earth Sciences, Shahid Beheshti University, Tehran, Iran ...
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 …
Download scientific diagram | Close-up view of outcrop, hand-specimens and Photomicrograph displaying the occurrence of hydrothermal alteration at the study area; a. Slab of porphyry intrusion ...
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 ... Geochemical studies, magmatic evolution, microstructures and replacement mechanisms in Jebale-Barez granitoid ...
jebale barez plutonic complex is composed of granitoid intrusive bodyes and is located in the east - north east jiroft and southeastern province of kerman on the lengths of the 57° 45' east to 58° 00' and northern latitudes 28° 30' to 29° 00'. plutonic complex composed of granodiorite, quartzdiorite, monzogranite and porphyritic …
The studied area (Mardehak) is located in the east of Jiroft, in the south of Kerman, in the Jabal Barez mountain range, which is a part of the magmatic belt of Urmia-Dokhtar.
Whereas the granitoid rocks from Jebal Barez granitoids have a ratio of Eu/Eu* < 1 suggesting the magma was generated under reducing conditions. 5. Granitoid rocks of KPCB have a high ratio of Sr/Y, therefore they are adakitic, while the Jebal-Barez granitoids have low ratio Sr/Y and cannot be adakitic. 5.