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Information Journal Paper

Title

GENESIS OF MG-BEARING INDUSTRIAL MINERALS (BRUCITE-HYDROMAGNESITE) IN POLYGENETIC MARBLE, BAGHI ABAD, YAZD

Pages

  61-71

Abstract

 The study area is located about 40 km southwest of Yazd in eastern SHIR-KUH range.Intrusive bodies occur as dike and small stocks. Chemical composition of intrusive bodies is in the range of granodiorite, diorite, and gabbro. The nature of magmatism is clac-alkaline, generated in orogenic setting. Cretaceous carbonate rocks in vicinity of those intrusions are transformed into various MARBLEs and skarns. The following mineral assemblages include: Forsterite +serpentine+talc+brucite+hydromagnesite+calcite+dolomite.Brucite porphyroblasts are only the most widespread mineral in MARBLEs. The peak of metamorphism is begun with periclase and forsterite (>700 oC) formation.Then low temperature paragenesis like carbonate and hydrous minerals form at 25oC. There are several stages in the MARBLE evolution which imply the polygenic genesis of the MARBLEs.

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    APA: Copy

    TAGHIPOUR, B.. (2011). GENESIS OF MG-BEARING INDUSTRIAL MINERALS (BRUCITE-HYDROMAGNESITE) IN POLYGENETIC MARBLE, BAGHI ABAD, YAZD. IRANIAN JOURNAL OF GEOLOGY, 5(17), 61-71. SID. https://sid.ir/paper/129380/en

    Vancouver: Copy

    TAGHIPOUR B.. GENESIS OF MG-BEARING INDUSTRIAL MINERALS (BRUCITE-HYDROMAGNESITE) IN POLYGENETIC MARBLE, BAGHI ABAD, YAZD. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2011;5(17):61-71. Available from: https://sid.ir/paper/129380/en

    IEEE: Copy

    B. TAGHIPOUR, “GENESIS OF MG-BEARING INDUSTRIAL MINERALS (BRUCITE-HYDROMAGNESITE) IN POLYGENETIC MARBLE, BAGHI ABAD, YAZD,” IRANIAN JOURNAL OF GEOLOGY, vol. 5, no. 17, pp. 61–71, 2011, [Online]. Available: https://sid.ir/paper/129380/en

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