The magnetic susceptibility behavior along two cores in Hassangholi Bay, eastern flank of the Caspian Sea and their interpretation for the sea level changes
Author:
, , , , , ,Year
: 2013
Abstract: 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
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
Keyword(s): 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 author | عبدالمجید نادری بنی | en |
| contributor author | سیدرضا موسوی حرمی | en |
| contributor author | Lahijani, H | en |
| contributor author | اسداله محبوبی | en |
| contributor author | ABDOLMAJID NADERI BENI | fa |
| contributor author | Sayyed Reza Moussavi Harami | fa |
| contributor author | Asadollah Mahboubi | fa |
| date accessioned | 2020-06-06T14:14:10Z | |
| date available | 2020-06-06T14:14:10Z | |
| date copyright | 1/5/2013 | |
| date issued | 2013 | |
| identifier uri | https://libsearch.um.ac.ir:443/fum/handle/fum/3388118?locale-attribute=en | |
| description abstract | 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 | en |
| language | English | |
| title | The magnetic susceptibility behavior along two cores in Hassangholi Bay, eastern flank of the Caspian Sea and their interpretation for the sea level changes | en |
| type | Conference Paper | |
| contenttype | External Fulltext | |
| subject keywords | Hassangholi Bay- Caspian Sea- magnetic susceptibility- | en |
| identifier link | https://profdoc.um.ac.ir/paper-abstract-1041168.html | |
| conference title | Rapidly Changing Large Lakes and Human Response | en |
| conference location | تهران | fa |
| identifier articleid | 1041168 |