PRESSURE-TEMPERATURE CONDITION AND HYDROTHERMAL-MAGMATIC FLUID EVOLUTION OF THE CU-MO SENJ DEPOSIT, CENTRAL ALBORZ: FLUID INCLUSION EVIDENCE

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

TALE FAZEL EBRAHIM; MEHRABI BEHZAD; ZAMANIAN HASSAN; HAYATALGHEYBI MASOUMEH

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: JOURNAL OF ECONOMIC GEOLOGY Year:2017 | Volume:8 | Issue:2 Page(s): 431-455

Download Full-Text

Persian Verion

View:

921

Download:

Cites:

Information Journal Paper

Title

PRESSURE-TEMPERATURE CONDITION AND HYDROTHERMAL-MAGMATIC FLUID EVOLUTION OF THE CU-MO SENJ DEPOSIT, CENTRAL ALBORZ: FLUID INCLUSION EVIDENCE

Author(s)

TALE FAZEL EBRAHIM | MEHRABI BEHZAD | ZAMANIAN HASSAN | HAYATALGHEYBI MASOUMEH | Issue Writer Certificate

Keywords

CU-MO MINERALIZATIONQ1

FLUID INCLUSIONSQ1

ORE-FORMING FLUID EVOLUTIONQ1

SENJ DEPOSITQ1

CENTRAL ALBORZQ2

Abstract

IntroductionThe SENJ DEPOSIT has significant potential for different types of mineralization, particularly porphyry-like Cu deposits, associated with subduction-related Eocene–Oligocene calc-alkaline porphyritic volcano-plutonic rocks. The study of FLUID INCLUSIONS in hydrothermal ore deposits aims to identify and characterize the pressure, temperature, volume and fluid composition, (PTX) conditions of fluids under which they were trapped (Heinrich et al., 1999; Ulrich and Heinrich, 2001; Redmond et al., 2004). Different characteristics of the deposit such as porphyrtic nature, alteration assemblage and the quartz-sulfide veins of the stockwork were poorly known. In this approach on the basis of alterations, vein cutting relationship and field distribution of FLUID INCLUSIONS, the physical and chemical evolution of the hydrothermal system forming the porphyry Cu-Mo (±Au-Ag) deposit in Senj is reconstructed.

Cites

No record.

References

No record.

Cite

APA: Copy

TALE FAZEL, EBRAHIM, MEHRABI, BEHZAD, ZAMANIAN, HASSAN, & HAYATALGHEYBI, MASOUMEH. (2017). PRESSURE-TEMPERATURE CONDITION AND HYDROTHERMAL-MAGMATIC FLUID EVOLUTION OF THE CU-MO SENJ DEPOSIT, CENTRAL ALBORZ: FLUID INCLUSION EVIDENCE. JOURNAL OF ECONOMIC GEOLOGY, 8(2), 431-455. SID. https://sid.ir/paper/180449/en

Vancouver: Copy

TALE FAZEL EBRAHIM, MEHRABI BEHZAD, ZAMANIAN HASSAN, HAYATALGHEYBI MASOUMEH. PRESSURE-TEMPERATURE CONDITION AND HYDROTHERMAL-MAGMATIC FLUID EVOLUTION OF THE CU-MO SENJ DEPOSIT, CENTRAL ALBORZ: FLUID INCLUSION EVIDENCE. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2017;8(2):431-455. Available from: https://sid.ir/paper/180449/en

IEEE: Copy

EBRAHIM TALE FAZEL, BEHZAD MEHRABI, HASSAN ZAMANIAN, and MASOUMEH HAYATALGHEYBI, “PRESSURE-TEMPERATURE CONDITION AND HYDROTHERMAL-MAGMATIC FLUID EVOLUTION OF THE CU-MO SENJ DEPOSIT, CENTRAL ALBORZ: FLUID INCLUSION EVIDENCE,” JOURNAL OF ECONOMIC GEOLOGY, vol. 8, no. 2, pp. 431–455, 2017, [Online]. Available: https://sid.ir/paper/180449/en

Related Journal Papers