Environments of Mukadiya and Bai Hassan formations depending on lithofacies and sedimentary structures in Zurbatiya area East of Iraq

Environments of Mukadiya and Bai Hassan formations depending on lithofacies and sedimentary structures in Zurbatiya area East of Iraq

The present study has carried out for Mukdadiya and Bai Hassan formations (Pliocene) at Zurbatiya area east of Iraq. Thickness of Mukdadiya Formation ranging between 1 to 70m in the study area. Mukdadiya Formation was divided into five finning-upward cycles depending on detailed field observations....

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Hauptverfasser: Ahmed, Hussein Z., Al-Tarif, Abdulsalam M., Kadhim, Lafta S.
Format: Tagungsbericht
Sprache:eng
Schlagworte:
Alluvial fans
Fossils
Metamorphic rocks
Mudstone
Rivers
Sandstone
Thickness
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page
container_issue 1
container_start_page
container_title
container_volume 2839
creator Ahmed, Hussein Z.
Al-Tarif, Abdulsalam M.
Kadhim, Lafta S.
description The present study has carried out for Mukdadiya and Bai Hassan formations (Pliocene) at Zurbatiya area east of Iraq. Thickness of Mukdadiya Formation ranging between 1 to 70m in the study area. Mukdadiya Formation was divided into five finning-upward cycles depending on detailed field observations. Mukdadiya Formation consisting of sedimentary structures like imbrication and trace fossils. The lithofacies were observed in Mukdadiya Formation are mudstone, sandstone and conglomerate lithofacies. The environment of the lower part of the Mukdadiya Formation considers as Meandering rivers environments while the lower part of the Mukdadiya Formation represents a braided rivers environment. Thickness of Bai Hassan Formation about 20m in the study area Bai Hassan Formation composed from one coarsening-upward cycle. The lithofacies were observed in Bai Hassan Formation are mudstone and conglomerate lithofacies. Bai Hassan Formation without sedimentary structures in this section because of rapid deposition. The environment of lower part of Bai Hassan Formation is meandering rivers while the upper part is alluvial fan. As well as determine the origin and ratio of the sedimentary, igneous, and metamorphic rocks.
doi_str_mv 10.1063/5.0171966
format Conference Proceeding
fullrecord <record><control><sourceid>proquest_scita</sourceid><recordid>TN_cdi_proquest_journals_2870158788</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2870158788</sourcerecordid><originalsourceid>FETCH-LOGICAL-p133t-5335ff09070a3914b3887bcd7e231955e31035566d696dc55d9b96a082e8f1733</originalsourceid><addsrcrecordid>eNotkM9KAzEYxIMoWKsH3yDgTdiabJp_Ry3VFipeFMRLyG6ymtom2yQr9AF8b3drT9_hm_kNMwBcYzTBiJE7OkGYY8nYCRhhSnHBGWanYISQnBbllLyfg4uU1giVknMxAr9z_-Ni8Fvrc4Khgc_dtzZur6H2Bj5oBxc6Je1hE-JWZxd8gsa21hvnP2HwcOPyV2h07Ww6WJI1boDpuIcpx67OXexfzsOPLlY9YUBHq-FcpzwELqPeXYKzRm-SvTreMXh7nL_OFsXq5Wk5u18VLSYkF5QQ2jRIIo40kXhaESF4VRtuS4IlpZZgRChlzDDJTE2pkZVkGonSigZzQsbg5p_bxrDrbMpqHbro-0hVCo4wFVyIXnX7r0q1y4fOqo1u2zdSGKlhZkXVcWbyB-vwb-4</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>conference_proceeding</recordtype><pqid>2870158788</pqid></control><display><type>conference_proceeding</type><title>Environments of Mukadiya and Bai Hassan formations depending on lithofacies and sedimentary structures in Zurbatiya area East of Iraq</title><source>AIP Journals Complete</source><creator>Ahmed, Hussein Z. ; Al-Tarif, Abdulsalam M. ; Kadhim, Lafta S.</creator><contributor>Kumbhalkar, Manoj A. ; Kene, Jagdish D. ; Gajghat, Radheshyam ; Rambhad, Kishor S.</contributor><creatorcontrib>Ahmed, Hussein Z. ; Al-Tarif, Abdulsalam M. ; Kadhim, Lafta S. ; Kumbhalkar, Manoj A. ; Kene, Jagdish D. ; Gajghat, Radheshyam ; Rambhad, Kishor S.</creatorcontrib><description>The present study has carried out for Mukdadiya and Bai Hassan formations (Pliocene) at Zurbatiya area east of Iraq. Thickness of Mukdadiya Formation ranging between 1 to 70m in the study area. Mukdadiya Formation was divided into five finning-upward cycles depending on detailed field observations. Mukdadiya Formation consisting of sedimentary structures like imbrication and trace fossils. The lithofacies were observed in Mukdadiya Formation are mudstone, sandstone and conglomerate lithofacies. The environment of the lower part of the Mukdadiya Formation considers as Meandering rivers environments while the lower part of the Mukdadiya Formation represents a braided rivers environment. Thickness of Bai Hassan Formation about 20m in the study area Bai Hassan Formation composed from one coarsening-upward cycle. The lithofacies were observed in Bai Hassan Formation are mudstone and conglomerate lithofacies. Bai Hassan Formation without sedimentary structures in this section because of rapid deposition. The environment of lower part of Bai Hassan Formation is meandering rivers while the upper part is alluvial fan. As well as determine the origin and ratio of the sedimentary, igneous, and metamorphic rocks.</description><identifier>ISSN: 0094-243X</identifier><identifier>EISSN: 1551-7616</identifier><identifier>DOI: 10.1063/5.0171966</identifier><identifier>CODEN: APCPCS</identifier><language>eng</language><publisher>Melville: American Institute of Physics</publisher><subject>Alluvial fans ; Fossils ; Metamorphic rocks ; Mudstone ; Rivers ; Sandstone ; Thickness</subject><ispartof>AIP conference proceedings, 2023, Vol.2839 (1)</ispartof><rights>Author(s)</rights><rights>2023 Author(s). Published by AIP Publishing.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://pubs.aip.org/acp/article-lookup/doi/10.1063/5.0171966$$EHTML$$P50$$Gscitation$$H</linktohtml><link.rule.ids>309,310,314,776,780,785,786,790,4498,23909,23910,25118,27901,27902,76126</link.rule.ids></links><search><contributor>Kumbhalkar, Manoj A.</contributor><contributor>Kene, Jagdish D.</contributor><contributor>Gajghat, Radheshyam</contributor><contributor>Rambhad, Kishor S.</contributor><creatorcontrib>Ahmed, Hussein Z.</creatorcontrib><creatorcontrib>Al-Tarif, Abdulsalam M.</creatorcontrib><creatorcontrib>Kadhim, Lafta S.</creatorcontrib><title>Environments of Mukadiya and Bai Hassan formations depending on lithofacies and sedimentary structures in Zurbatiya area East of Iraq</title><title>AIP conference proceedings</title><description>The present study has carried out for Mukdadiya and Bai Hassan formations (Pliocene) at Zurbatiya area east of Iraq. Thickness of Mukdadiya Formation ranging between 1 to 70m in the study area. Mukdadiya Formation was divided into five finning-upward cycles depending on detailed field observations. Mukdadiya Formation consisting of sedimentary structures like imbrication and trace fossils. The lithofacies were observed in Mukdadiya Formation are mudstone, sandstone and conglomerate lithofacies. The environment of the lower part of the Mukdadiya Formation considers as Meandering rivers environments while the lower part of the Mukdadiya Formation represents a braided rivers environment. Thickness of Bai Hassan Formation about 20m in the study area Bai Hassan Formation composed from one coarsening-upward cycle. The lithofacies were observed in Bai Hassan Formation are mudstone and conglomerate lithofacies. Bai Hassan Formation without sedimentary structures in this section because of rapid deposition. The environment of lower part of Bai Hassan Formation is meandering rivers while the upper part is alluvial fan. As well as determine the origin and ratio of the sedimentary, igneous, and metamorphic rocks.</description><subject>Alluvial fans</subject><subject>Fossils</subject><subject>Metamorphic rocks</subject><subject>Mudstone</subject><subject>Rivers</subject><subject>Sandstone</subject><subject>Thickness</subject><issn>0094-243X</issn><issn>1551-7616</issn><fulltext>true</fulltext><rsrctype>conference_proceeding</rsrctype><creationdate>2023</creationdate><recordtype>conference_proceeding</recordtype><recordid>eNotkM9KAzEYxIMoWKsH3yDgTdiabJp_Ry3VFipeFMRLyG6ymtom2yQr9AF8b3drT9_hm_kNMwBcYzTBiJE7OkGYY8nYCRhhSnHBGWanYISQnBbllLyfg4uU1giVknMxAr9z_-Ni8Fvrc4Khgc_dtzZur6H2Bj5oBxc6Je1hE-JWZxd8gsa21hvnP2HwcOPyV2h07Ww6WJI1boDpuIcpx67OXexfzsOPLlY9YUBHq-FcpzwELqPeXYKzRm-SvTreMXh7nL_OFsXq5Wk5u18VLSYkF5QQ2jRIIo40kXhaESF4VRtuS4IlpZZgRChlzDDJTE2pkZVkGonSigZzQsbg5p_bxrDrbMpqHbro-0hVCo4wFVyIXnX7r0q1y4fOqo1u2zdSGKlhZkXVcWbyB-vwb-4</recordid><startdate>20230929</startdate><enddate>20230929</enddate><creator>Ahmed, Hussein Z.</creator><creator>Al-Tarif, Abdulsalam M.</creator><creator>Kadhim, Lafta S.</creator><general>American Institute of Physics</general><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>20230929</creationdate><title>Environments of Mukadiya and Bai Hassan formations depending on lithofacies and sedimentary structures in Zurbatiya area East of Iraq</title><author>Ahmed, Hussein Z. ; Al-Tarif, Abdulsalam M. ; Kadhim, Lafta S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p133t-5335ff09070a3914b3887bcd7e231955e31035566d696dc55d9b96a082e8f1733</frbrgroupid><rsrctype>conference_proceedings</rsrctype><prefilter>conference_proceedings</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Alluvial fans</topic><topic>Fossils</topic><topic>Metamorphic rocks</topic><topic>Mudstone</topic><topic>Rivers</topic><topic>Sandstone</topic><topic>Thickness</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ahmed, Hussein Z.</creatorcontrib><creatorcontrib>Al-Tarif, Abdulsalam M.</creatorcontrib><creatorcontrib>Kadhim, Lafta S.</creatorcontrib><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ahmed, Hussein Z.</au><au>Al-Tarif, Abdulsalam M.</au><au>Kadhim, Lafta S.</au><au>Kumbhalkar, Manoj A.</au><au>Kene, Jagdish D.</au><au>Gajghat, Radheshyam</au><au>Rambhad, Kishor S.</au><format>book</format><genre>proceeding</genre><ristype>CONF</ristype><atitle>Environments of Mukadiya and Bai Hassan formations depending on lithofacies and sedimentary structures in Zurbatiya area East of Iraq</atitle><btitle>AIP conference proceedings</btitle><date>2023-09-29</date><risdate>2023</risdate><volume>2839</volume><issue>1</issue><issn>0094-243X</issn><eissn>1551-7616</eissn><coden>APCPCS</coden><abstract>The present study has carried out for Mukdadiya and Bai Hassan formations (Pliocene) at Zurbatiya area east of Iraq. Thickness of Mukdadiya Formation ranging between 1 to 70m in the study area. Mukdadiya Formation was divided into five finning-upward cycles depending on detailed field observations. Mukdadiya Formation consisting of sedimentary structures like imbrication and trace fossils. The lithofacies were observed in Mukdadiya Formation are mudstone, sandstone and conglomerate lithofacies. The environment of the lower part of the Mukdadiya Formation considers as Meandering rivers environments while the lower part of the Mukdadiya Formation represents a braided rivers environment. Thickness of Bai Hassan Formation about 20m in the study area Bai Hassan Formation composed from one coarsening-upward cycle. The lithofacies were observed in Bai Hassan Formation are mudstone and conglomerate lithofacies. Bai Hassan Formation without sedimentary structures in this section because of rapid deposition. The environment of lower part of Bai Hassan Formation is meandering rivers while the upper part is alluvial fan. As well as determine the origin and ratio of the sedimentary, igneous, and metamorphic rocks.</abstract><cop>Melville</cop><pub>American Institute of Physics</pub><doi>10.1063/5.0171966</doi><tpages>9</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0094-243X
ispartof AIP conference proceedings, 2023, Vol.2839 (1)
issn 0094-243X
1551-7616
language eng
recordid cdi_proquest_journals_2870158788
source AIP Journals Complete
subjects Alluvial fans
Fossils
Metamorphic rocks
Mudstone
Rivers
Sandstone
Thickness
title Environments of Mukadiya and Bai Hassan formations depending on lithofacies and sedimentary structures in Zurbatiya area East of Iraq
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-08T20%3A15%3A58IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_scita&rft_val_fmt=info:ofi/fmt:kev:mtx:book&rft.genre=proceeding&rft.atitle=Environments%20of%20Mukadiya%20and%20Bai%20Hassan%20formations%20depending%20on%20lithofacies%20and%20sedimentary%20structures%20in%20Zurbatiya%20area%20East%20of%20Iraq&rft.btitle=AIP%20conference%20proceedings&rft.au=Ahmed,%20Hussein%20Z.&rft.date=2023-09-29&rft.volume=2839&rft.issue=1&rft.issn=0094-243X&rft.eissn=1551-7616&rft.coden=APCPCS&rft_id=info:doi/10.1063/5.0171966&rft_dat=%3Cproquest_scita%3E2870158788%3C/proquest_scita%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2870158788&rft_id=info:pmid/&rfr_iscdi=true