الخصائص الهيدرولوجية لمنخفض الصليبات (جنوب العراق)

The low Alsalibat important depressions which are located in southern Iraq, specifically in the provinces of Muthanna, DhiQar, and within walking distance of the course of the Euphrates River, a distance, though construction Tectonic for low falls within the scope of the seam between the sidewalk st...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Ādāb al-kūfat 2017, Vol.1 (30), p.117-174
Hauptverfasser: الخفاجي، سرحان نعيم طشطوش, جبر، علي محسن كامل هاشم محسن
Format: Artikel
Sprache:ara ; eng
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 174
container_issue 30
container_start_page 117
container_title Ādāb al-kūfat
container_volume 1
creator الخفاجي، سرحان نعيم طشطوش
جبر، علي محسن كامل هاشم محسن
description The low Alsalibat important depressions which are located in southern Iraq, specifically in the provinces of Muthanna, DhiQar, and within walking distance of the course of the Euphrates River, a distance, though construction Tectonic for low falls within the scope of the seam between the sidewalk stable (sedimentary easy) others and sidewalk Mstqralamtmthel b (Western plateau). The region has been affected by tectonic movements that stretched from the eras third time until the Holocene of time four-wheel, and had the effect of these movements played a major role in the low configuration, in addition to contrast the influence of other factors of the geological structure and topography and the climate and soil in its composition, low and is considered one of the natural reservoirs the task of water in the region, it shall take the tank to the Euphrates River excess during the flood period, as well as water valleys, as it ends a series of valleys that varies from the discharged water per class between the valley and the last. Of these valleys it starts flowing from inside Saudi territory, and denounced it as a drainage starts from inside Iraqi territory, as well as so that the center of this low represents Lake Hoare Itbainun in terms of depth on the one hand to the other.
format Article
fullrecord <record><control><sourceid>emarefa</sourceid><recordid>TN_cdi_emarefa_primary_770668</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>770668</sourcerecordid><originalsourceid>FETCH-emarefa_primary_7706683</originalsourceid><addsrcrecordid>eNpjYuA0MjMz0TUxs4xgYeA0tLQ00bWwtLTkYOAtLs5MMjA0MrCwNLE05GSIvbH8ZsuNdTe23lh-Y9mNrQog7s32m1031t_YeLMDyO64sQbIW6kAZLbebLux7mbjjW1gVTe2AoW6bqwAalyloAFU1QZUuwIitfPGRiDdpMnDwJqWmFOcyguluRlk3VxDnD10U3MTi1LTEuMLijKBrMp4c3MDMzMLY0LyAE-MXyU</addsrcrecordid><sourcetype>Publisher</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>الخصائص الهيدرولوجية لمنخفض الصليبات (جنوب العراق)</title><source>DOAJ Directory of Open Access Journals</source><source>Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals</source><creator>الخفاجي، سرحان نعيم طشطوش ; جبر، علي محسن كامل هاشم محسن</creator><creatorcontrib>الخفاجي، سرحان نعيم طشطوش ; جبر، علي محسن كامل هاشم محسن</creatorcontrib><description>The low Alsalibat important depressions which are located in southern Iraq, specifically in the provinces of Muthanna, DhiQar, and within walking distance of the course of the Euphrates River, a distance, though construction Tectonic for low falls within the scope of the seam between the sidewalk stable (sedimentary easy) others and sidewalk Mstqralamtmthel b (Western plateau). The region has been affected by tectonic movements that stretched from the eras third time until the Holocene of time four-wheel, and had the effect of these movements played a major role in the low configuration, in addition to contrast the influence of other factors of the geological structure and topography and the climate and soil in its composition, low and is considered one of the natural reservoirs the task of water in the region, it shall take the tank to the Euphrates River excess during the flood period, as well as water valleys, as it ends a series of valleys that varies from the discharged water per class between the valley and the last. Of these valleys it starts flowing from inside Saudi territory, and denounced it as a drainage starts from inside Iraqi territory, as well as so that the center of this low represents Lake Hoare Itbainun in terms of depth on the one hand to the other.</description><identifier>ISSN: 1994-8999</identifier><identifier>EISSN: 2664-469X</identifier><language>ara ; eng</language><publisher>النجف، العراق: جامعة الكوفة، كلية الآداب</publisher><ispartof>Ādāb al-kūfat, 2017, Vol.1 (30), p.117-174</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780</link.rule.ids></links><search><creatorcontrib>الخفاجي، سرحان نعيم طشطوش</creatorcontrib><creatorcontrib>جبر، علي محسن كامل هاشم محسن</creatorcontrib><title>الخصائص الهيدرولوجية لمنخفض الصليبات (جنوب العراق)</title><title>Ādāb al-kūfat</title><description>The low Alsalibat important depressions which are located in southern Iraq, specifically in the provinces of Muthanna, DhiQar, and within walking distance of the course of the Euphrates River, a distance, though construction Tectonic for low falls within the scope of the seam between the sidewalk stable (sedimentary easy) others and sidewalk Mstqralamtmthel b (Western plateau). The region has been affected by tectonic movements that stretched from the eras third time until the Holocene of time four-wheel, and had the effect of these movements played a major role in the low configuration, in addition to contrast the influence of other factors of the geological structure and topography and the climate and soil in its composition, low and is considered one of the natural reservoirs the task of water in the region, it shall take the tank to the Euphrates River excess during the flood period, as well as water valleys, as it ends a series of valleys that varies from the discharged water per class between the valley and the last. Of these valleys it starts flowing from inside Saudi territory, and denounced it as a drainage starts from inside Iraqi territory, as well as so that the center of this low represents Lake Hoare Itbainun in terms of depth on the one hand to the other.</description><issn>1994-8999</issn><issn>2664-469X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNpjYuA0MjMz0TUxs4xgYeA0tLQ00bWwtLTkYOAtLs5MMjA0MrCwNLE05GSIvbH8ZsuNdTe23lh-Y9mNrQog7s32m1031t_YeLMDyO64sQbIW6kAZLbebLux7mbjjW1gVTe2AoW6bqwAalyloAFU1QZUuwIitfPGRiDdpMnDwJqWmFOcyguluRlk3VxDnD10U3MTi1LTEuMLijKBrMp4c3MDMzMLY0LyAE-MXyU</recordid><startdate>2017</startdate><enddate>2017</enddate><creator>الخفاجي، سرحان نعيم طشطوش</creator><creator>جبر، علي محسن كامل هاشم محسن</creator><general>جامعة الكوفة، كلية الآداب</general><scope>ADJCN</scope><scope>AGBXD</scope><scope>AHFXO</scope><scope>AHMDM</scope></search><sort><creationdate>2017</creationdate><title>الخصائص الهيدرولوجية لمنخفض الصليبات (جنوب العراق)</title><author>الخفاجي، سرحان نعيم طشطوش ; جبر، علي محسن كامل هاشم محسن</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-emarefa_primary_7706683</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>ara ; eng</language><creationdate>2017</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>الخفاجي، سرحان نعيم طشطوش</creatorcontrib><creatorcontrib>جبر، علي محسن كامل هاشم محسن</creatorcontrib><collection>الدوريات العلمية والإحصائية - e-Marefa Academic and Statistical Periodicals</collection><collection>قاعدة البيئة والطاقة والمياه - e-Marefa Water, Energy &amp; Environment Issues</collection><collection>معرفة - المحتوى العربي الأكاديمي المتكامل - e-Marefa Academic Complete</collection><collection>قاعدة العلوم الإنسانية - e-Marefa Humanities</collection><jtitle>Ādāb al-kūfat</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>الخفاجي، سرحان نعيم طشطوش</au><au>جبر، علي محسن كامل هاشم محسن</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>الخصائص الهيدرولوجية لمنخفض الصليبات (جنوب العراق)</atitle><jtitle>Ādāb al-kūfat</jtitle><date>2017</date><risdate>2017</risdate><volume>1</volume><issue>30</issue><spage>117</spage><epage>174</epage><pages>117-174</pages><issn>1994-8999</issn><eissn>2664-469X</eissn><abstract>The low Alsalibat important depressions which are located in southern Iraq, specifically in the provinces of Muthanna, DhiQar, and within walking distance of the course of the Euphrates River, a distance, though construction Tectonic for low falls within the scope of the seam between the sidewalk stable (sedimentary easy) others and sidewalk Mstqralamtmthel b (Western plateau). The region has been affected by tectonic movements that stretched from the eras third time until the Holocene of time four-wheel, and had the effect of these movements played a major role in the low configuration, in addition to contrast the influence of other factors of the geological structure and topography and the climate and soil in its composition, low and is considered one of the natural reservoirs the task of water in the region, it shall take the tank to the Euphrates River excess during the flood period, as well as water valleys, as it ends a series of valleys that varies from the discharged water per class between the valley and the last. Of these valleys it starts flowing from inside Saudi territory, and denounced it as a drainage starts from inside Iraqi territory, as well as so that the center of this low represents Lake Hoare Itbainun in terms of depth on the one hand to the other.</abstract><cop>النجف، العراق</cop><pub>جامعة الكوفة، كلية الآداب</pub><tpages>58 ص.</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1994-8999
ispartof Ādāb al-kūfat, 2017, Vol.1 (30), p.117-174
issn 1994-8999
2664-469X
language ara ; eng
recordid cdi_emarefa_primary_770668
source DOAJ Directory of Open Access Journals; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals
title الخصائص الهيدرولوجية لمنخفض الصليبات (جنوب العراق)
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-19T12%3A40%3A01IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-emarefa&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=%D8%A7%D9%84%D8%AE%D8%B5%D8%A7%D8%A6%D8%B5%20%D8%A7%D9%84%D9%87%D9%8A%D8%AF%D8%B1%D9%88%D9%84%D9%88%D8%AC%D9%8A%D8%A9%20%D9%84%D9%85%D9%86%D8%AE%D9%81%D8%B6%20%D8%A7%D9%84%D8%B5%D9%84%D9%8A%D8%A8%D8%A7%D8%AA%20(%D8%AC%D9%86%D9%88%D8%A8%20%D8%A7%D9%84%D8%B9%D8%B1%D8%A7%D9%82)&rft.jtitle=%C4%80d%C4%81b%20al-k%C5%ABfat&rft.au=%D8%A7%D9%84%D8%AE%D9%81%D8%A7%D8%AC%D9%8A%D8%8C%20%D8%B3%D8%B1%D8%AD%D8%A7%D9%86%20%D9%86%D8%B9%D9%8A%D9%85%20%D8%B7%D8%B4%D8%B7%D9%88%D8%B4&rft.date=2017&rft.volume=1&rft.issue=30&rft.spage=117&rft.epage=174&rft.pages=117-174&rft.issn=1994-8999&rft.eissn=2664-469X&rft_id=info:doi/&rft_dat=%3Cemarefa%3E770668%3C/emarefa%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true