CLAY CEMENT DEVELOPMENT IN FARAGHAN FORMATION, GAHKUM MOUNTAIN

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ZAMANZADEH S.M.; AMINI A.A.H.; SARDAR H.

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Journal: Iranian Journal of Geology Year:2009 | Volume:2 | Issue:8 Page(s): 103-111

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Information Journal Paper

Title

CLAY CEMENT DEVELOPMENT IN FARAGHAN FORMATION, GAHKUM MOUNTAIN

Author(s)

ZAMANZADEH S.M. | AMINI A.A.H. | SARDAR H. | Issue Writer Certificate

Keywords

CHLORITEQ2

CLAY CEMENTSQ2

DIAGENESISQ3

DICKITEQ3

FARAGHAN FORMATIONQ3

ILLITEQ2

KAOLINITEQ3

SMECTITEQ2

Abstract

Study of the FARAGHAN FORMATION sandstone illustrates the development of CLAY CEMENTS in them. KAOLINITE is by far the most abundant clay cement in sandstones and SMECTITE, ILLITE and CHLORITE are the next frequent cements respectively. DICKITE also occurs as the deep burial diagenetic product from KAOLINITE. Formation of KAOLINITE is attributed to shallow diagenetic environments mainly due to feldspar alteration. Formation of CHLORITE and ILLITE is attributed to deep burial diagenetic environments due to transformation of bertierine and KAOLINITE precursors respectively. SMECTITE is suggested to form in either eogenetic or telogenetic environments. The maximum burial depth estimated for this formation, mainly based on the development of mesogenetic clays (i.e. CHLORITE, ILLITE and DICKITE), is closely corresponding with the generation of gas.

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APA: Copy

ZAMANZADEH, S.M., AMINI, A.A.H., & SARDAR, H.. (2009). CLAY CEMENT DEVELOPMENT IN FARAGHAN FORMATION, GAHKUM MOUNTAIN. IRANIAN JOURNAL OF GEOLOGY, 2(8), 103-111. SID. https://sid.ir/paper/129345/en

Vancouver: Copy

ZAMANZADEH S.M., AMINI A.A.H., SARDAR H.. CLAY CEMENT DEVELOPMENT IN FARAGHAN FORMATION, GAHKUM MOUNTAIN. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2009;2(8):103-111. Available from: https://sid.ir/paper/129345/en

IEEE: Copy

S.M. ZAMANZADEH, A.A.H. AMINI, and H. SARDAR, “CLAY CEMENT DEVELOPMENT IN FARAGHAN FORMATION, GAHKUM MOUNTAIN,” IRANIAN JOURNAL OF GEOLOGY, vol. 2, no. 8, pp. 103–111, 2009, [Online]. Available: https://sid.ir/paper/129345/en

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