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Information Journal Paper

Title

New hypothesis on time and thermal gradient of subducted slab with emphasis on dolomitic and shale host rocks in formation of Pb-Zn deposits of Irankuh-Ahangaran belt

Pages

  677-706

Abstract

 Mississippi Valley-Type (MVT) deposits are epigenetic zinc and lead deposits with minor copper hosted by dolostone, limestone, and locally sandstone in platform carbonate sequences inboard of major orogenic belts (Leach and Sangster, 1993; Leach et al., 2010). . . .

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  • Cite

    APA: Copy

    KARIMPOUR, MOHAMMAD HASSAN, MALEKZADEH SHAFAROUDI, AZADEH, ALAMINIA, ZAHRA, ESMAEILI SEVIERI, ABBAS, & STERN, CHARLES R.. (2019). New hypothesis on time and thermal gradient of subducted slab with emphasis on dolomitic and shale host rocks in formation of Pb-Zn deposits of Irankuh-Ahangaran belt. JOURNAL OF ECONOMIC GEOLOGY, 10(2 ), 677-706. SID. https://sid.ir/paper/180493/en

    Vancouver: Copy

    KARIMPOUR MOHAMMAD HASSAN, MALEKZADEH SHAFAROUDI AZADEH, ALAMINIA ZAHRA, ESMAEILI SEVIERI ABBAS, STERN CHARLES R.. New hypothesis on time and thermal gradient of subducted slab with emphasis on dolomitic and shale host rocks in formation of Pb-Zn deposits of Irankuh-Ahangaran belt. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2019;10(2 ):677-706. Available from: https://sid.ir/paper/180493/en

    IEEE: Copy

    MOHAMMAD HASSAN KARIMPOUR, AZADEH MALEKZADEH SHAFAROUDI, ZAHRA ALAMINIA, ABBAS ESMAEILI SEVIERI, and CHARLES R. STERN, “New hypothesis on time and thermal gradient of subducted slab with emphasis on dolomitic and shale host rocks in formation of Pb-Zn deposits of Irankuh-Ahangaran belt,” JOURNAL OF ECONOMIC GEOLOGY, vol. 10, no. 2 , pp. 677–706, 2019, [Online]. Available: https://sid.ir/paper/180493/en

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