SEDIMENTOLOGY AND MINERALOGY OF HOLOCENE SEDIMENTS OF HOZ-E-SOLTAN LAKE

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REZAEIAN LANGEROUDI SAEED; LAK RAZYEH

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ISSN: 2588-4824

Journal Paper

Paper Information

Journal: QUATERNARY JOURNAL OF IRAN Year:2015 | Volume:1 | Issue:2 Page(s): 7-8

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Title

SEDIMENTOLOGY AND MINERALOGY OF HOLOCENE SEDIMENTS OF HOZ-E-SOLTAN LAKE

Author(s)

REZAEIAN LANGEROUDI SAEED | LAK RAZYEH | Issue Writer Certificate

Keywords

CORE

EVAPORITE

HOZ-E-SOLTAN LAKE

QOM

SEDIMENT

Abstract

Extended Abstract: Introduction: Geological time has been EVAPORITEd SEDIMENTs form by solar-driven concentration of a surface or nearsurface brine. Large, thick and extensive deposits were dominated by rock-salt (mega-halite) or anhydrite (mega-sulfate) deposits tend to be marine EVAPORITEs and can be associated with extensive deposits of potash salts (mega-potash). Examinations of SEDIMENTologic and mineralogic characteristics of the closed-basin COREs due to the very high susceptibility to precipitation and evaporation balance are beneficial for determination and evolution of late Quaternary SEDIMENTary specification. Playa defined as an intra-continental arid zone basin with a negative water balance for over half of each year, dry for over 75% of the time, with a capillary fringe close enough to the surface such that evaporation will cause water to discharge, usually resulting in EVAPORITEs.

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APA: Copy

REZAEIAN LANGEROUDI, SAEED, & LAK, RAZYEH. (2015). SEDIMENTOLOGY AND MINERALOGY OF HOLOCENE SEDIMENTS OF HOZ-E-SOLTAN LAKE. QUATERNARY JOURNAL OF IRAN, 1(2), 7-8. SID. https://sid.ir/paper/676704/en

Vancouver: Copy

REZAEIAN LANGEROUDI SAEED, LAK RAZYEH. SEDIMENTOLOGY AND MINERALOGY OF HOLOCENE SEDIMENTS OF HOZ-E-SOLTAN LAKE. QUATERNARY JOURNAL OF IRAN[Internet]. 2015;1(2):7-8. Available from: https://sid.ir/paper/676704/en

IEEE: Copy

SAEED REZAEIAN LANGEROUDI, and RAZYEH LAK, “SEDIMENTOLOGY AND MINERALOGY OF HOLOCENE SEDIMENTS OF HOZ-E-SOLTAN LAKE,” QUATERNARY JOURNAL OF IRAN, vol. 1, no. 2, pp. 7–8, 2015, [Online]. Available: https://sid.ir/paper/676704/en

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