Biostratigraphy of early cretaceous sediments (Fahliyan Formation, Berriasian–Barremian) in Aghar19 (Zagros Basin, SW Iran)
The Fahliyan Formation, which is part of the Khami Group is one of the important oil resources in the lower cretaceous strata in the Zagros area. Index Foraminifera, continuity, and discontinuities have been used to identify the boundaries of this formation. To study biostratigraphy on Fahliyan Form...
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| Veröffentlicht in: | Carbonates and evaporites 2021-06, Vol.36 (2), Article 26 |
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| description | The Fahliyan Formation, which is part of the Khami Group is one of the important oil resources in the lower cretaceous strata in the Zagros area. Index Foraminifera, continuity, and discontinuities have been used to identify the boundaries of this formation. To study biostratigraphy on Fahliyan Formation, the subsurface stratigraphic section of Aghar19 was selected in the southwest province of Iran. The thickness of this formation in this section is measured 215 m, including thin-to-medium-bedded limestone and dolomitic limestone. Fahliyan Formation continuously overlies Surmeh and Hith Formation and underlies Gadvan Formation. Vertical study of this formation has led to the identification of calcareous algae and foraminifera, which include 48 genera, 32 species, and three biozones in the sediments of the Fahliyan Formation. These biozones include: (1)
Dukhania
zone; (2)
Pseudocyclammina lituus
,
Trocholina
zone; and (3)
Orbitolina
,
Choffatella
,
Salpingoporella
Assemblage zone. Based on the established biozones, the age of the Fahliyan Formation in the Aghar19 section was determined from Berriasian to Early Barremian. |
| doi_str_mv | 10.1007/s13146-021-00696-8 |
| format | Article |
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Dukhania
zone; (2)
Pseudocyclammina lituus
,
Trocholina
zone; and (3)
Orbitolina
,
Choffatella
,
Salpingoporella
Assemblage zone. Based on the established biozones, the age of the Fahliyan Formation in the Aghar19 section was determined from Berriasian to Early Barremian.</description><identifier>ISSN: 0891-2556</identifier><identifier>EISSN: 1878-5212</identifier><identifier>DOI: 10.1007/s13146-021-00696-8</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Algae ; Biostratigraphy ; Cretaceous ; Dolomitic limestone ; Earth and Environmental Science ; Earth Sciences ; Foraminifera ; Fossils ; Geology ; Limestone ; Mineral Resources ; Mineralogy ; Original Article ; Sediment ; Sediments ; Stratigraphy</subject><ispartof>Carbonates and evaporites, 2021-06, Vol.36 (2), Article 26</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2021</rights><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2021.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a342t-4d68d0f6606ec65e3845218d4f347f108cab87f234d18c044796f29907c9f4663</citedby><cites>FETCH-LOGICAL-a342t-4d68d0f6606ec65e3845218d4f347f108cab87f234d18c044796f29907c9f4663</cites><orcidid>0000-0001-7315-3137</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s13146-021-00696-8$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s13146-021-00696-8$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Abedpour, Masoud</creatorcontrib><creatorcontrib>Afghah, Massih</creatorcontrib><creatorcontrib>Dehghanian, Mohammadsadegh</creatorcontrib><title>Biostratigraphy of early cretaceous sediments (Fahliyan Formation, Berriasian–Barremian) in Aghar19 (Zagros Basin, SW Iran)</title><title>Carbonates and evaporites</title><addtitle>Carbonates Evaporites</addtitle><description>The Fahliyan Formation, which is part of the Khami Group is one of the important oil resources in the lower cretaceous strata in the Zagros area. Index Foraminifera, continuity, and discontinuities have been used to identify the boundaries of this formation. To study biostratigraphy on Fahliyan Formation, the subsurface stratigraphic section of Aghar19 was selected in the southwest province of Iran. The thickness of this formation in this section is measured 215 m, including thin-to-medium-bedded limestone and dolomitic limestone. Fahliyan Formation continuously overlies Surmeh and Hith Formation and underlies Gadvan Formation. Vertical study of this formation has led to the identification of calcareous algae and foraminifera, which include 48 genera, 32 species, and three biozones in the sediments of the Fahliyan Formation. These biozones include: (1)
Dukhania
zone; (2)
Pseudocyclammina lituus
,
Trocholina
zone; and (3)
Orbitolina
,
Choffatella
,
Salpingoporella
Assemblage zone. Based on the established biozones, the age of the Fahliyan Formation in the Aghar19 section was determined from Berriasian to Early Barremian.</description><subject>Algae</subject><subject>Biostratigraphy</subject><subject>Cretaceous</subject><subject>Dolomitic limestone</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Foraminifera</subject><subject>Fossils</subject><subject>Geology</subject><subject>Limestone</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Original Article</subject><subject>Sediment</subject><subject>Sediments</subject><subject>Stratigraphy</subject><issn>0891-2556</issn><issn>1878-5212</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kLFOwzAURS0EEqXwA0yWWIpEwHYcxx6bikIlJAZASCyWSew0VZOU53TIgMQ_8Id8CS5BYmPyG865z-8idErJJSUkvfI0plxEhNGIEKFEJPfQiMpURgmjbB-NiFQ0YkkiDtGR96sdxJUaofesan0HpqtKMJtlj1uHrYF1j3Owncltu_XY26KqbdN5PJmb5brqTYPnLdTBapsLnFmAyvjKNF8fn5kBsHWYz3HV4Gm5NEAVnryYElqPs4AF4-EZLyAgx-jAmbW3J7_vGD3Nrx9nt9Hd_c1iNr2LTMxZF_FCyII4IYiwuUhsLHk4SxbcxTx1lMjcvMrUsZgXVOaE81QJx5Qiaa4cFyIeo7MhdwPt29b6Tq_aLTRhpWa7JJrGJAkUG6g8fNWDdXoDVW2g15ToXc16qFmHmvVPzVoGKR4kH-CmtPAX_Y_1DVcagA8</recordid><startdate>20210601</startdate><enddate>20210601</enddate><creator>Abedpour, Masoud</creator><creator>Afghah, Massih</creator><creator>Dehghanian, Mohammadsadegh</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><orcidid>https://orcid.org/0000-0001-7315-3137</orcidid></search><sort><creationdate>20210601</creationdate><title>Biostratigraphy of early cretaceous sediments (Fahliyan Formation, Berriasian–Barremian) in Aghar19 (Zagros Basin, SW Iran)</title><author>Abedpour, Masoud ; Afghah, Massih ; Dehghanian, Mohammadsadegh</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a342t-4d68d0f6606ec65e3845218d4f347f108cab87f234d18c044796f29907c9f4663</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Algae</topic><topic>Biostratigraphy</topic><topic>Cretaceous</topic><topic>Dolomitic limestone</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Foraminifera</topic><topic>Fossils</topic><topic>Geology</topic><topic>Limestone</topic><topic>Mineral Resources</topic><topic>Mineralogy</topic><topic>Original Article</topic><topic>Sediment</topic><topic>Sediments</topic><topic>Stratigraphy</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Abedpour, Masoud</creatorcontrib><creatorcontrib>Afghah, Massih</creatorcontrib><creatorcontrib>Dehghanian, Mohammadsadegh</creatorcontrib><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection (Proquest) (PQ_SDU_P3)</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><jtitle>Carbonates and evaporites</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Abedpour, Masoud</au><au>Afghah, Massih</au><au>Dehghanian, Mohammadsadegh</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Biostratigraphy of early cretaceous sediments (Fahliyan Formation, Berriasian–Barremian) in Aghar19 (Zagros Basin, SW Iran)</atitle><jtitle>Carbonates and evaporites</jtitle><stitle>Carbonates Evaporites</stitle><date>2021-06-01</date><risdate>2021</risdate><volume>36</volume><issue>2</issue><artnum>26</artnum><issn>0891-2556</issn><eissn>1878-5212</eissn><abstract>The Fahliyan Formation, which is part of the Khami Group is one of the important oil resources in the lower cretaceous strata in the Zagros area. Index Foraminifera, continuity, and discontinuities have been used to identify the boundaries of this formation. To study biostratigraphy on Fahliyan Formation, the subsurface stratigraphic section of Aghar19 was selected in the southwest province of Iran. The thickness of this formation in this section is measured 215 m, including thin-to-medium-bedded limestone and dolomitic limestone. Fahliyan Formation continuously overlies Surmeh and Hith Formation and underlies Gadvan Formation. Vertical study of this formation has led to the identification of calcareous algae and foraminifera, which include 48 genera, 32 species, and three biozones in the sediments of the Fahliyan Formation. These biozones include: (1)
Dukhania
zone; (2)
Pseudocyclammina lituus
,
Trocholina
zone; and (3)
Orbitolina
,
Choffatella
,
Salpingoporella
Assemblage zone. Based on the established biozones, the age of the Fahliyan Formation in the Aghar19 section was determined from Berriasian to Early Barremian.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s13146-021-00696-8</doi><orcidid>https://orcid.org/0000-0001-7315-3137</orcidid></addata></record> |
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| subjects | Algae Biostratigraphy Cretaceous Dolomitic limestone Earth and Environmental Science Earth Sciences Foraminifera Fossils Geology Limestone Mineral Resources Mineralogy Original Article Sediment Sediments Stratigraphy |
| title | Biostratigraphy of early cretaceous sediments (Fahliyan Formation, Berriasian–Barremian) in Aghar19 (Zagros Basin, SW Iran) |
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