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Information Journal Paper

Title

SULFIDE MINERALIZATION IN ULTRAMAFIC ROCKS OF THE FARYAB OPHIOLITE COMPLEX, SOUTHERN KERMAN

Pages

  259-276

Abstract

 IntroductionWorldwide, Ni-Cu and PGE magmatic SULFIDE deposits are confined to the lower parts of stratiform mafic and ultramafic complexes. However, OPHIOLITE mafic and ultramafic complexes have been rarely explored for SULFIDE deposits despite the fact that they have been extensively explored and exploited for chromite. SULFIDE saturation during magmatic evolution is necessary for SULFIDE MINERALIZATION, in which SULFIDE melts scavenge chalcophile metals from the parent magma and concentrate them in specific lithological zones. The lack of exploration for SULFIDEs in this environment suggests that SULFIDE saturation is rarely attained in OPHIOLITE-related magmas. Some OPHIOLITEs, however, contain SULFIDE deposits, such as at Acoje in Philippines, and Cliffs in Shetland, U.K. (Evans, 2000; Naldrett, 2004).

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    APA: Copy

    RAJABZADEH, MOHAMMAD ALI, & AL SADI, FATEMEH. (2016). SULFIDE MINERALIZATION IN ULTRAMAFIC ROCKS OF THE FARYAB OPHIOLITE COMPLEX, SOUTHERN KERMAN. JOURNAL OF ECONOMIC GEOLOGY, 7(2), 259-276. SID. https://sid.ir/paper/180543/en

    Vancouver: Copy

    RAJABZADEH MOHAMMAD ALI, AL SADI FATEMEH. SULFIDE MINERALIZATION IN ULTRAMAFIC ROCKS OF THE FARYAB OPHIOLITE COMPLEX, SOUTHERN KERMAN. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2016;7(2):259-276. Available from: https://sid.ir/paper/180543/en

    IEEE: Copy

    MOHAMMAD ALI RAJABZADEH, and FATEMEH AL SADI, “SULFIDE MINERALIZATION IN ULTRAMAFIC ROCKS OF THE FARYAB OPHIOLITE COMPLEX, SOUTHERN KERMAN,” JOURNAL OF ECONOMIC GEOLOGY, vol. 7, no. 2, pp. 259–276, 2016, [Online]. Available: https://sid.ir/paper/180543/en

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