DOLOMITIZATION AND EVAPORATE MINERALIZATION OF SACHUN FORMATION AT TYPE LOCALITY (SE SHIRAZ)

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SHABAFROOZ R.; MAHBOUBI A.; MOUSSAVI HARAMI R.

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Journal: Iranian Journal of Crystallography and Mineralogy Year:2010 | Volume:17 | Issue:4 Page(s): 609-620

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Information Journal Paper

Title

DOLOMITIZATION AND EVAPORATE MINERALIZATION OF SACHUN FORMATION AT TYPE LOCALITY (SE SHIRAZ)

Author(s)

SHABAFROOZ R. | MAHBOUBI A. | MOUSSAVI HARAMI R. | Issue Writer Certificate

Keywords

GYPSUMQ3

ANHYDRITEQ2

ALABASTRINEQ3

PORPHYROBLASTICQ3

DOLOMITEQ2

SACHUN FORMATIONQ2

Abstract

The SACHUN FORMATION (Paleocene-Lower Eocene) is mainly composed of carbonates and evaporates that were deposited in shallow-marine evaporitic mudflat environments. The SACHUN FORMATION in the study area has been divided into three units including: lower evaporate, middle bioclastic limestone and upper evaporate. It is mainly composed of diagenetic GYPSUM, which originated from dehydration of ANHYDRITE precursor. This GYPSUM in the SACHUN FORMATION generally displays ALABASTRINE and PORPHYROBLASTIC textures with corroded ANHYDRITE relics. Petro logical studies reveal that the most important diagenetic processes affected the middle Part of the SACHUN FORMATION are dolomitization and evaporate mineralization. Four types of DOLOMITE, ranging from early to burial diagenetic environments, were identified. These are including very fine-to-fine crystalline (D1), neomorphic DOLOMITE (D2), fine-to-medium crystalline euhedral to subhedral DOLOMITE (D3) and pore-and fracture-filling DOLOMITE (D4).

Cites

EVAPORITE (ANHYDRITE AND CELESTITE) MINERALIZATION AND ITS EFFECT ON RESERVOIR QUALITY OF THE DOLOSTONE INTERVALS OF THE ASMARI FORMATION, NORTHERN PART OF DEZFUL EMBAYMENT, SOUTHWEST OF IRAN

References

بازنگری مرز بین سازندهای تاربور و ساچون درکوه ساچون، جنوب داراب فارس ( محل برش نمونه سازند ساچون)

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APA: Copy

SHABAFROOZ, R., MAHBOUBI, A., & MOUSSAVI HARAMI, R.. (2010). DOLOMITIZATION AND EVAPORATE MINERALIZATION OF SACHUN FORMATION AT TYPE LOCALITY (SE SHIRAZ). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 17(4), 609-620. SID. https://sid.ir/paper/4202/en

Vancouver: Copy

SHABAFROOZ R., MAHBOUBI A., MOUSSAVI HARAMI R.. DOLOMITIZATION AND EVAPORATE MINERALIZATION OF SACHUN FORMATION AT TYPE LOCALITY (SE SHIRAZ). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2010;17(4):609-620. Available from: https://sid.ir/paper/4202/en

IEEE: Copy

R. SHABAFROOZ, A. MAHBOUBI, and R. MOUSSAVI HARAMI, “DOLOMITIZATION AND EVAPORATE MINERALIZATION OF SACHUN FORMATION AT TYPE LOCALITY (SE SHIRAZ),” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 17, no. 4, pp. 609–620, 2010, [Online]. Available: https://sid.ir/paper/4202/en

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