PETRO GENESIS OF SKARN RELATED CU-PORPHYRY INTRUSION DEPOSIT, ALI-ABAD- DARREH ZERESHK, YAZD

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.

TAGHIPOUR BATOUL; MACKIZADEH MOHAMMAD ALI

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

Journal Paper

Paper Information

Journal: JOURNAL OF ECONOMIC GEOLOGY Year:2011 | Volume:3 | Issue:1 Page(s): 79-92

Download Full-Text

Persian Verion

View:

1,085

Download:

Cites:

Information Journal Paper

Title

PETRO GENESIS OF SKARN RELATED CU-PORPHYRY INTRUSION DEPOSIT, ALI-ABAD- DARREH ZERESHK, YAZD

Author(s)

TAGHIPOUR BATOUL | MACKIZADEH MOHAMMAD ALI | Issue Writer Certificate

Keywords

SKARNQ2

GARNETQ2

ANDRADITEQ2

CU-PORPHYRYQ2

HYDROTHERMALQ2

Abstract

The study area is a part of Cenozoic magmatic belt of Central Iran, which is located in the West of Yazd porovince. Contact metamorphism and SKARN occurred in conglomerate part of Sngestan Formation. The Oligocene intrusion bodies of Ali-Abad-Darreh Zereshk are leucocerate and have the chemical composition of granite to granodiorite with calc-alkaline affinity from volcanic arc geological setting. The main mineral assemblage of SKARN in order of imprtance is as follow: GARNET+epidote+quartz+calcite + pyrite+iron oxides. Brown GARNETs are the SKARN characteristic mineral. EPMA analysis has shown that the chemical composition with GARNET belong to ANDRADITE-grossular solid-solution (And 65, Gross 30) with more ANDRADITE component. The high permeability and presence of carbonate pebbles in conglomerate are two important factors for fluid flow and genesis of GARNETs. Distinct oscillatory zoning in GARNETs is resulted from the change of fO2 in fluids. The evolution of Ali-Abad SKARN is took place in the range of 380 to 530 oC, 0.5 Kbar pressure and high fO2. Also close association of this SKARN with Ali-Abad intrusive with CU-PORPHYRY mineralization shows that this SKARN is a CU-PORPHYRY type SKARN.

Cites

No record.

References

Cite

APA: Copy

TAGHIPOUR, BATOUL, & MACKIZADEH, MOHAMMAD ALI. (2011). PETRO GENESIS OF SKARN RELATED CU-PORPHYRY INTRUSION DEPOSIT, ALI-ABAD- DARREH ZERESHK, YAZD. JOURNAL OF ECONOMIC GEOLOGY, 3(1), 79-92. SID. https://sid.ir/paper/180422/en

Vancouver: Copy

TAGHIPOUR BATOUL, MACKIZADEH MOHAMMAD ALI. PETRO GENESIS OF SKARN RELATED CU-PORPHYRY INTRUSION DEPOSIT, ALI-ABAD- DARREH ZERESHK, YAZD. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2011;3(1):79-92. Available from: https://sid.ir/paper/180422/en

IEEE: Copy

BATOUL TAGHIPOUR, and MOHAMMAD ALI MACKIZADEH, “PETRO GENESIS OF SKARN RELATED CU-PORPHYRY INTRUSION DEPOSIT, ALI-ABAD- DARREH ZERESHK, YAZD,” JOURNAL OF ECONOMIC GEOLOGY, vol. 3, no. 1, pp. 79–92, 2011, [Online]. Available: https://sid.ir/paper/180422/en

Related Journal Papers