INVESTIGATION OF MINERALOGY AND GEOLOGY OF ZEOLITIC TUFFS IN ARDAKAN AREA

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GHANEEI J.; TAGHIPOUR B.; TAGHIPOUR S.

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Paper Information

Journal: RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE" Year:2006 | Volume:25 | Issue:3 Page(s): 117-129

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Information Journal Paper

Title

INVESTIGATION OF MINERALOGY AND GEOLOGY OF ZEOLITIC TUFFS IN ARDAKAN AREA

Author(s)

GHANEEI J. | TAGHIPOUR B. | TAGHIPOUR S. | Issue Writer Certificate

Keywords

MAGMATISMQ3

CENTRAL IRANQ3

ARDAKANQ3

ZEOLITEQ3

CLINOPTILOLITEQ3

Abstract

The studied area is located in Cenozoic Magmatic Belt of CENTRAL IRAN. The main constituents rocks are Eocene volcanic including: andesite, trachite, dacite and related pyroclastics. Field studies, mineralogy and result of analytical data (DTG, TG, XRD and XRF) have shown that the CLINOPTILOLITE is the main ZEOLITE component of acid altered tuffs. Quartz, muscovite, biotite are minor minerals in the zeolitic tuffs. A closed hydrologic system is probably has formed this sedimentary type ZEOLITE deposit, because the chemical composition of fresh tuffs are similar to zeolitic tuffs. On the base of geochemical data absorption behavior of ZEOLITEs in zeolitic tuffs are responsible to anomaly of Ba and Sr in the rocks. Volcanic rocks are originated from calc-alkaline type magma.

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APA: Copy

GHANEEI, J., TAGHIPOUR, B., & TAGHIPOUR, S.. (2006). INVESTIGATION OF MINERALOGY AND GEOLOGY OF ZEOLITIC TUFFS IN ARDAKAN AREA. RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 25(3), 117-129. SID. https://sid.ir/paper/55888/en

Vancouver: Copy

GHANEEI J., TAGHIPOUR B., TAGHIPOUR S.. INVESTIGATION OF MINERALOGY AND GEOLOGY OF ZEOLITIC TUFFS IN ARDAKAN AREA. RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2006;25(3):117-129. Available from: https://sid.ir/paper/55888/en

IEEE: Copy

J. GHANEEI, B. TAGHIPOUR, and S. TAGHIPOUR, “INVESTIGATION OF MINERALOGY AND GEOLOGY OF ZEOLITIC TUFFS IN ARDAKAN AREA,” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 25, no. 3, pp. 117–129, 2006, [Online]. Available: https://sid.ir/paper/55888/en

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