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The magnetic susceptibility behavior along two cores in Hassangholi Bay, eastern flank of the Caspian Sea and their interpretation for the sea level changes

نویسنده:
عبدالمجید نادری بنی
,
سیدرضا موسوی حرمی
,
Lahijani, H
,
اسداله محبوبی
,
ABDOLMAJID NADERI BENI
,
Sayyed Reza Moussavi Harami
,
Asadollah Mahboubi
سال
: 2013
چکیده: Magnetic susceptibility is largely depending to mineralogy of

materials particularly to Fe- bearing minerals. However, some other

inherent and non-inherent properties of sediments such as grain size

and shape can impact the measures. This property enables us to

classify different types of sediments based on their magnetic

behavior.

The Hassangholi Bay lies in the eastern flank of the Caspian Sea

where the region has been influenced by the level changes. The area

receives sediments from different sources with different magnetic

properties. Copet Dagh in the east is the main source for detrital

carbonate while Alborz Mountain in south could be the main source

for Fe bearing minerals. However, the Caspian Sea could bring

sediments during sea level rise. This last source could change the

magnetic susceptibility behavior of the sediments and could be a

potential proxy for tracing the Caspian Sea level fluctuations.

This paper tries to make a correlation between the magnetic

susceptibility and sea level curves in the eastern flank of the

Caspian Sea
یو آر آی: http://libsearch.um.ac.ir:80/fum/handle/fum/3388118
کلیدواژه(گان): Hassangholi Bay- Caspian Sea- magnetic susceptibility-
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    The magnetic susceptibility behavior along two cores in Hassangholi Bay, eastern flank of the Caspian Sea and their interpretation for the sea level changes

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contributor authorعبدالمجید نادری بنیen
contributor authorسیدرضا موسوی حرمیen
contributor authorLahijani, Hen
contributor authorاسداله محبوبیen
contributor authorABDOLMAJID NADERI BENIfa
contributor authorSayyed Reza Moussavi Haramifa
contributor authorAsadollah Mahboubifa
date accessioned2020-06-06T14:14:10Z
date available2020-06-06T14:14:10Z
date copyright1/5/2013
date issued2013
identifier urihttp://libsearch.um.ac.ir:80/fum/handle/fum/3388118
description abstractMagnetic susceptibility is largely depending to mineralogy of

materials particularly to Fe- bearing minerals. However, some other

inherent and non-inherent properties of sediments such as grain size

and shape can impact the measures. This property enables us to

classify different types of sediments based on their magnetic

behavior.

The Hassangholi Bay lies in the eastern flank of the Caspian Sea

where the region has been influenced by the level changes. The area

receives sediments from different sources with different magnetic

properties. Copet Dagh in the east is the main source for detrital

carbonate while Alborz Mountain in south could be the main source

for Fe bearing minerals. However, the Caspian Sea could bring

sediments during sea level rise. This last source could change the

magnetic susceptibility behavior of the sediments and could be a

potential proxy for tracing the Caspian Sea level fluctuations.

This paper tries to make a correlation between the magnetic

susceptibility and sea level curves in the eastern flank of the

Caspian Sea
en
languageEnglish
titleThe magnetic susceptibility behavior along two cores in Hassangholi Bay, eastern flank of the Caspian Sea and their interpretation for the sea level changesen
typeConference Paper
contenttypeExternal Fulltext
subject keywordsHassangholi Bay- Caspian Sea- magnetic susceptibility-en
identifier linkhttps://profdoc.um.ac.ir/paper-abstract-1041168.html
conference titleRapidly Changing Large Lakes and Human Responseen
conference locationتهرانfa
identifier articleid1041168
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