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Information Journal Paper

Title

THE ORIGIN OF HALITE AND GYPSUM WITH INTRODUCTION OF GLAUBERITE AND SASSOLITE MINERALS IN LARESTAN SALT DOME, (SOUTH OF IRAN)

Pages

  11-21

Abstract

 Salt domes are one of the most notable features of Zagros fold belt in the south of Iran. In this study the salt of Dehkoyeh, Paskhand and Karmostaj domes located in Larestan were analyzed based on salt colors. In mineralogical studies for the first time two minerals, SASSOLITE B(OH)3 and GLAUBERITE Na2Ca (SO4)2 which are of today 's FUMAROLEs indexes in different parts of the world, were identified in Dehkoyeh dome as well as Hormuz salt formation. Generally, compared to other existing elements iron has the greatest impact on the changes of salt color. In salts accompanying SASSOLITE and GLAUBERITE certain minerals with temperature range between 50oC to 60oC were identified. Sea floor FUMAROLEs has probably played important roles in formation of Hormuz salt in infra-Cambrian era. In all probability this FUMAROLE was the main supply of ions needed for salt formation and this fact justifies the emergence of large volumes of Hormuz salt in a relatively short time.

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    APA: Copy

    NOKHBATOLFOGHAHAIE, ALI, NEZAFATI, NIMA, & GHORBANI, MANSOUR. (2017). THE ORIGIN OF HALITE AND GYPSUM WITH INTRODUCTION OF GLAUBERITE AND SASSOLITE MINERALS IN LARESTAN SALT DOME, (SOUTH OF IRAN). APPLIED SEDIMENTOLOGY, 4(8), 11-21. SID. https://sid.ir/paper/260565/en

    Vancouver: Copy

    NOKHBATOLFOGHAHAIE ALI, NEZAFATI NIMA, GHORBANI MANSOUR. THE ORIGIN OF HALITE AND GYPSUM WITH INTRODUCTION OF GLAUBERITE AND SASSOLITE MINERALS IN LARESTAN SALT DOME, (SOUTH OF IRAN). APPLIED SEDIMENTOLOGY[Internet]. 2017;4(8):11-21. Available from: https://sid.ir/paper/260565/en

    IEEE: Copy

    ALI NOKHBATOLFOGHAHAIE, NIMA NEZAFATI, and MANSOUR GHORBANI, “THE ORIGIN OF HALITE AND GYPSUM WITH INTRODUCTION OF GLAUBERITE AND SASSOLITE MINERALS IN LARESTAN SALT DOME, (SOUTH OF IRAN),” APPLIED SEDIMENTOLOGY, vol. 4, no. 8, pp. 11–21, 2017, [Online]. Available: https://sid.ir/paper/260565/en

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