INVESTIGATION OF KHOROSLODAGH GEOMORPHOLOGY EMPHASIZING AGREEMENT AND ADVERSE STREAM NETWORKS (NORTHERN ARDABIL PROVINCE)

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

MADADI A.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: GEOGRAPHICAL RESEARCH Year:2010 | Volume:25 | Issue:3 (98) Page(s): 103-124

Download Full-Text

Persian Verion

View:

952

Download:

Cites:

Information Journal Paper

Title

INVESTIGATION OF KHOROSLODAGH GEOMORPHOLOGY EMPHASIZING AGREEMENT AND ADVERSE STREAM NETWORKS (NORTHERN ARDABIL PROVINCE)

Author(s)

MADADI A. | Issue Writer Certificate

Keywords

KHOROSLODAGHQ3

ANTECEDENCEQ3

INVERTED RELIEFQ3

DRAINAGE NETWORKQ3

EARTH STRUCTUREQ3

Abstract

KHOROSLODAGHlocated in northwestern of Iran and south of Moghan plain in Ardabil province. These mountainsare from Azarbyjan mountains unit and are separated from Caucasus and Talesh Mountains in Azarbyjan republic. Study area was folded by upper Pliocene and Quaternary orogeny. Pliocene orogeny was severe but Quaternary folded was calm. Afterward orogeny movements and folding, invertedrelief (specially hanging synclinals) has been formed by erosion. Apart of hydrographic network are adjustment with construction but some of drainage are not agreement with structure geology. This disagreeing is interpret by ANTECEDENCE theory, because this area has been a subsidence area, before Khoroslo Mountain forming, has been deposited from Eocene until Pliocene. In south of this area existence Meshghen- Ahar uplifted zone and rivers stream from this uplifted area toward north (Moghan and Araxs river). Study area in Pliocene and Quaternary orogeny (KHOROSLODAGH) has been uplifted and rivers continue to drilling activity, this activity has been the cause of cutting previous direction and created narrow valleys in the area.

Cites

No record.

References

پدیده برگشت ارتفاعی در لوت از پالئوزوئیک تا سنوزوئیک

Cite

APA: Copy

MADADI, A.. (2010). INVESTIGATION OF KHOROSLODAGH GEOMORPHOLOGY EMPHASIZING AGREEMENT AND ADVERSE STREAM NETWORKS (NORTHERN ARDABIL PROVINCE). GEOGRAPHICAL RESEARCH, 25(3 (98)), 103-124. SID. https://sid.ir/paper/30068/en

Vancouver: Copy

MADADI A.. INVESTIGATION OF KHOROSLODAGH GEOMORPHOLOGY EMPHASIZING AGREEMENT AND ADVERSE STREAM NETWORKS (NORTHERN ARDABIL PROVINCE). GEOGRAPHICAL RESEARCH[Internet]. 2010;25(3 (98)):103-124. Available from: https://sid.ir/paper/30068/en

IEEE: Copy

A. MADADI, “INVESTIGATION OF KHOROSLODAGH GEOMORPHOLOGY EMPHASIZING AGREEMENT AND ADVERSE STREAM NETWORKS (NORTHERN ARDABIL PROVINCE),” GEOGRAPHICAL RESEARCH, vol. 25, no. 3 (98), pp. 103–124, 2010, [Online]. Available: https://sid.ir/paper/30068/en

Related Journal Papers