HOLOCENE SEDIMENTARY ENVIRONMENT OF MAHARLOU LAKE BY SEDIMENTOLOGICAL AND MINERALOGICAL EVIDENCES

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LAK RAZYEH; REZAEIAN LANGEROUDI SAEED

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Journal Paper

Paper Information

Journal: QUATERNARY JOURNAL OF IRAN Year:2015 | Volume:1 | Issue:1 Page(s): 13-14

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Information Journal Paper

Title

HOLOCENE SEDIMENTARY ENVIRONMENT OF MAHARLOU LAKE BY SEDIMENTOLOGICAL AND MINERALOGICAL EVIDENCES

Author(s)

LAK RAZYEH | REZAEIAN LANGEROUDI SAEED | Issue Writer Certificate

Keywords

CORE

ENVIRONMENT RECONSTRUCTION

EVAPORITE

HOLOCENE

LAKE

Abstract

Extended Abstract: Introduction: Playa is considered as a dry inland with dry negative water balance which is dry in more than 3/4 of a year. Its capillary margins are so close to the surface that evaporation resulting from these margins leads to water discharge and evaporates formation. Paleophysical and paleochemical changes of a playa make significant changes in type of sediments which can be applied to determine paleosedimentary environments and their effective sedimentary processes. Sediments and minerals of salty LAKEs are changed by seasonal and temporal variations of sea level, so by studying sediments and minerals especially evaporate minerals in the past, sedimentary environments can be reconstructed. The present study is aimed to reconstruct and determine HOLOCENE sub-environments in Maharlou LAKE as a playa sedimentary environment which is exactly related to input– output balance of water. Maharlou is a salty ephemeral LAKE. It is located between 29o17’00 and 29o23’30’’ northern latitudes and 52o41’00’’ and 52o49’00’’ eastern longitude. The LAKE has maximum area equals to 28 km2 situated in 18 km from southeastern of Shiraz town. The greatest length of the LAKE is nearly 35 km, maximum width about 15 km and average width 7 km. The LAKE's height from sea level is 1455m. There is no permanent river in catchment basin of Maharlou LAKE and basin's flooding is entered in the LAKE by several flood plains and seasonal (monsoon) rivers.

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APA: Copy

LAK, RAZYEH, & REZAEIAN LANGEROUDI, SAEED. (2015). HOLOCENE SEDIMENTARY ENVIRONMENT OF MAHARLOU LAKE BY SEDIMENTOLOGICAL AND MINERALOGICAL EVIDENCES. QUATERNARY JOURNAL OF IRAN, 1(1), 13-14. SID. https://sid.ir/paper/680931/en

Vancouver: Copy

LAK RAZYEH, REZAEIAN LANGEROUDI SAEED. HOLOCENE SEDIMENTARY ENVIRONMENT OF MAHARLOU LAKE BY SEDIMENTOLOGICAL AND MINERALOGICAL EVIDENCES. QUATERNARY JOURNAL OF IRAN[Internet]. 2015;1(1):13-14. Available from: https://sid.ir/paper/680931/en

IEEE: Copy

RAZYEH LAK, and SAEED REZAEIAN LANGEROUDI, “HOLOCENE SEDIMENTARY ENVIRONMENT OF MAHARLOU LAKE BY SEDIMENTOLOGICAL AND MINERALOGICAL EVIDENCES,” QUATERNARY JOURNAL OF IRAN, vol. 1, no. 1, pp. 13–14, 2015, [Online]. Available: https://sid.ir/paper/680931/en

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