THE MINERALOGY, STRUCTURE, TEXTURE AND GENESIS OF THE REDBED-TYPE SEDIMENTARY-DIAGENETIC MARKASHEH CU OCCURRENCE IN THE JURASSIC GARADU RED FORMATION, SOUTH CENTRAL IRAN

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MAHDAVI A.; RASTAD E.; HOSSEINI BARZI M.

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Journal: GEOSCIENCES Year:2011 | Volume:21 | Issue:81 Page(s): 81-92

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Title

THE MINERALOGY, STRUCTURE, TEXTURE AND GENESIS OF THE REDBED-TYPE SEDIMENTARY-DIAGENETIC MARKASHEH CU OCCURRENCE IN THE JURASSIC GARADU RED FORMATION, SOUTH CENTRAL IRAN

Author(s)

MAHDAVI A. | RASTAD E. | HOSSEINI BARZI M. | Issue Writer Certificate

Keywords

SEDIMENTARY DIAGENETIC COPPERQ2

PALEOCHANNELQ2

OXIDIZEDQ2

REDUCED AND MINERALIZED ZONESQ2

MARKASHEHQ2

RAVARQ3

Abstract

Markasheh occurrence includes redbed sediments (Garadu Redbeds) of Jurassic-Cretaceous age that extend in a large area for over 400 km in an area. Garadu Redbeds include alternate of red OXIDIZED sandstone, conglomerate and siltstone that is partly reduced. Mineralization occurred in reduced horizons and is related with PALEOCHANNELs. In the MARKASHEH area two obvious main reduced horizons and four subhorizons occur. Each of these horizons includes three zones: Red OXIDIZED zone, bleached zone and Reduced mineralized zone. Based on characteristics of MARKASHEH Cu occurrence such as lithology, lens like and layered shape) in geometry, (regional extent, replacement and disseminated textures, simple mineralogy, presence of plant fossils and concentration of copper mineralization in relation to fossils, MARKASHEH Cu occurrence is considered as a Red bed sediment-hosted copper deposit type. The mineralization has been occured after early diagenesis before burial of the host roks.

Cites

STUDY OF MINERALIZATION AND ORIGIN OF PLIOCENE CONGLOMERATE HOSTED STRATA BOUND SEDIMENTARY CU MINERALIZATION IN THE GHAREH-AGHAJ, MAKU

References

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APA: Copy

MAHDAVI, A., RASTAD, E., & HOSSEINI BARZI, M.. (2011). THE MINERALOGY, STRUCTURE, TEXTURE AND GENESIS OF THE REDBED-TYPE SEDIMENTARY-DIAGENETIC MARKASHEH CU OCCURRENCE IN THE JURASSIC GARADU RED FORMATION, SOUTH CENTRAL IRAN. GEOSCIENCES, 21(81), 81-92. SID. https://sid.ir/paper/32029/en

Vancouver: Copy

MAHDAVI A., RASTAD E., HOSSEINI BARZI M.. THE MINERALOGY, STRUCTURE, TEXTURE AND GENESIS OF THE REDBED-TYPE SEDIMENTARY-DIAGENETIC MARKASHEH CU OCCURRENCE IN THE JURASSIC GARADU RED FORMATION, SOUTH CENTRAL IRAN. GEOSCIENCES[Internet]. 2011;21(81):81-92. Available from: https://sid.ir/paper/32029/en

IEEE: Copy

A. MAHDAVI, E. RASTAD, and M. HOSSEINI BARZI, “THE MINERALOGY, STRUCTURE, TEXTURE AND GENESIS OF THE REDBED-TYPE SEDIMENTARY-DIAGENETIC MARKASHEH CU OCCURRENCE IN THE JURASSIC GARADU RED FORMATION, SOUTH CENTRAL IRAN,” GEOSCIENCES, vol. 21, no. 81, pp. 81–92, 2011, [Online]. Available: https://sid.ir/paper/32029/en

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