Diagenesis and Genetic Model of Calcareous Interbeds in Marine Strata

Calcareous interbeds control the migration of oil and water in marine strata. However, in China, the origins of such calcareous interbeds have not been investigated in detail. In this paper, we present a study of calcareous interbeds in marine strata of the Zhujiang Formation in the Wenchang Oil Fie...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Chemistry and technology of fuels and oils 2024-05, Vol.60 (2), p.374-381
Hauptverfasser: Lin, Dan, Liao, Jijia, Liao, Mingguang, Hu, Yu
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 381
container_issue 2
container_start_page 374
container_title Chemistry and technology of fuels and oils
container_volume 60
creator Lin, Dan
Liao, Jijia
Liao, Mingguang
Hu, Yu
description Calcareous interbeds control the migration of oil and water in marine strata. However, in China, the origins of such calcareous interbeds have not been investigated in detail. In this paper, we present a study of calcareous interbeds in marine strata of the Zhujiang Formation in the Wenchang Oil Field, which is located in the southeast of Hainan Province, China. The lithological characteristics, types and features of diagenesis, and formation of the calcareous interbeds were investigated using core, thin-section, scanning electron microscopy, and cathodoluminescence observations, and stable carbon and oxygen isotope data. The calcareous interbeds consist of mixed sediments, which are dominated by bioclastic limestones containing terrigenous clasts, along with subordinate calcareous sandstone. The interbeds are densely cemented. The bioclasts are dominantly brachiopods, pleopods, and foraminifera, with minor amounts of echinodermata, bivalves, red algae, ostracods, and bryozoa. Diagenesis involved calcitic cementation, associated with relatively weak compaction. Carbon and oxygen isotopic data indicate the pore water that formed the carbonate cement was mostly sourced from seawater and minor amounts of meteoric water. The degree of carbonate cementation was significantly related to the bioclast content. On the basis of our study, a genetic model for the macroscopic and microscopic formation of calcareous interbeds is proposed.
doi_str_mv 10.1007/s10553-024-01691-0
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_3059397252</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>3059397252</sourcerecordid><originalsourceid>FETCH-LOGICAL-c270t-ab38dec24d2ea210b7c4b8a5b871841a651ebda29bc6336a57b2f38a93854ed43</originalsourceid><addsrcrecordid>eNp9kDFPwzAQhS0EEqXwB5gsMRvOdpw4IyqlVGrFAMzW2blUqUpS7HTg35M2SGxMdye9907vY-xWwr0EKB6SBGO0AJUJkHkpBZyxiTSFFlZLOGcTACiFhlJdsquUtsezUHrC5k8Nbqil1CSObcUXw943ga-7ina8q_kMdwEjdYfEl21P0VOVeNPyNcamJf7WR-zxml3UuEt08zun7ON5_j57EavXxXL2uBJBFdAL9NpWFFRWKUIlwRch8xaNt4W0mcTcSPIVqtKHXOscTeFVrS2W2pqMqkxP2d2Yu4_d14FS77bdIbbDS6fBlHroZNSgUqMqxC6lSLXbx-YT47eT4I643IjLDbjcCZeDwaRHUxrE7YbiX_Q_rh-PuWwq</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>3059397252</pqid></control><display><type>article</type><title>Diagenesis and Genetic Model of Calcareous Interbeds in Marine Strata</title><source>SpringerLink Journals</source><creator>Lin, Dan ; Liao, Jijia ; Liao, Mingguang ; Hu, Yu</creator><creatorcontrib>Lin, Dan ; Liao, Jijia ; Liao, Mingguang ; Hu, Yu</creatorcontrib><description>Calcareous interbeds control the migration of oil and water in marine strata. However, in China, the origins of such calcareous interbeds have not been investigated in detail. In this paper, we present a study of calcareous interbeds in marine strata of the Zhujiang Formation in the Wenchang Oil Field, which is located in the southeast of Hainan Province, China. The lithological characteristics, types and features of diagenesis, and formation of the calcareous interbeds were investigated using core, thin-section, scanning electron microscopy, and cathodoluminescence observations, and stable carbon and oxygen isotope data. The calcareous interbeds consist of mixed sediments, which are dominated by bioclastic limestones containing terrigenous clasts, along with subordinate calcareous sandstone. The interbeds are densely cemented. The bioclasts are dominantly brachiopods, pleopods, and foraminifera, with minor amounts of echinodermata, bivalves, red algae, ostracods, and bryozoa. Diagenesis involved calcitic cementation, associated with relatively weak compaction. Carbon and oxygen isotopic data indicate the pore water that formed the carbonate cement was mostly sourced from seawater and minor amounts of meteoric water. The degree of carbonate cementation was significantly related to the bioclast content. On the basis of our study, a genetic model for the macroscopic and microscopic formation of calcareous interbeds is proposed.</description><identifier>ISSN: 0009-3092</identifier><identifier>EISSN: 1573-8310</identifier><identifier>DOI: 10.1007/s10553-024-01691-0</identifier><language>eng</language><publisher>New York: Springer US</publisher><subject>Carbon ; Cathodoluminescence ; Cementation ; Chemistry ; Chemistry and Materials Science ; Geotechnical Engineering &amp; Applied Earth Sciences ; Industrial Chemistry/Chemical Engineering ; Innovative Technologies of Oil and Gas ; Meteoric water ; Mineral Resources ; Mollusks ; Oil fields ; Oxygen isotopes ; Pore water ; Sandstone ; Seawater ; Sediments ; Strata</subject><ispartof>Chemistry and technology of fuels and oils, 2024-05, Vol.60 (2), p.374-381</ispartof><rights>Springer Science+Business Media, LLC, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c270t-ab38dec24d2ea210b7c4b8a5b871841a651ebda29bc6336a57b2f38a93854ed43</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10553-024-01691-0$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10553-024-01691-0$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>Lin, Dan</creatorcontrib><creatorcontrib>Liao, Jijia</creatorcontrib><creatorcontrib>Liao, Mingguang</creatorcontrib><creatorcontrib>Hu, Yu</creatorcontrib><title>Diagenesis and Genetic Model of Calcareous Interbeds in Marine Strata</title><title>Chemistry and technology of fuels and oils</title><addtitle>Chem Technol Fuels Oils</addtitle><description>Calcareous interbeds control the migration of oil and water in marine strata. However, in China, the origins of such calcareous interbeds have not been investigated in detail. In this paper, we present a study of calcareous interbeds in marine strata of the Zhujiang Formation in the Wenchang Oil Field, which is located in the southeast of Hainan Province, China. The lithological characteristics, types and features of diagenesis, and formation of the calcareous interbeds were investigated using core, thin-section, scanning electron microscopy, and cathodoluminescence observations, and stable carbon and oxygen isotope data. The calcareous interbeds consist of mixed sediments, which are dominated by bioclastic limestones containing terrigenous clasts, along with subordinate calcareous sandstone. The interbeds are densely cemented. The bioclasts are dominantly brachiopods, pleopods, and foraminifera, with minor amounts of echinodermata, bivalves, red algae, ostracods, and bryozoa. Diagenesis involved calcitic cementation, associated with relatively weak compaction. Carbon and oxygen isotopic data indicate the pore water that formed the carbonate cement was mostly sourced from seawater and minor amounts of meteoric water. The degree of carbonate cementation was significantly related to the bioclast content. On the basis of our study, a genetic model for the macroscopic and microscopic formation of calcareous interbeds is proposed.</description><subject>Carbon</subject><subject>Cathodoluminescence</subject><subject>Cementation</subject><subject>Chemistry</subject><subject>Chemistry and Materials Science</subject><subject>Geotechnical Engineering &amp; Applied Earth Sciences</subject><subject>Industrial Chemistry/Chemical Engineering</subject><subject>Innovative Technologies of Oil and Gas</subject><subject>Meteoric water</subject><subject>Mineral Resources</subject><subject>Mollusks</subject><subject>Oil fields</subject><subject>Oxygen isotopes</subject><subject>Pore water</subject><subject>Sandstone</subject><subject>Seawater</subject><subject>Sediments</subject><subject>Strata</subject><issn>0009-3092</issn><issn>1573-8310</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNp9kDFPwzAQhS0EEqXwB5gsMRvOdpw4IyqlVGrFAMzW2blUqUpS7HTg35M2SGxMdye9907vY-xWwr0EKB6SBGO0AJUJkHkpBZyxiTSFFlZLOGcTACiFhlJdsquUtsezUHrC5k8Nbqil1CSObcUXw943ga-7ina8q_kMdwEjdYfEl21P0VOVeNPyNcamJf7WR-zxml3UuEt08zun7ON5_j57EavXxXL2uBJBFdAL9NpWFFRWKUIlwRch8xaNt4W0mcTcSPIVqtKHXOscTeFVrS2W2pqMqkxP2d2Yu4_d14FS77bdIbbDS6fBlHroZNSgUqMqxC6lSLXbx-YT47eT4I643IjLDbjcCZeDwaRHUxrE7YbiX_Q_rh-PuWwq</recordid><startdate>20240501</startdate><enddate>20240501</enddate><creator>Lin, Dan</creator><creator>Liao, Jijia</creator><creator>Liao, Mingguang</creator><creator>Hu, Yu</creator><general>Springer US</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>20240501</creationdate><title>Diagenesis and Genetic Model of Calcareous Interbeds in Marine Strata</title><author>Lin, Dan ; Liao, Jijia ; Liao, Mingguang ; Hu, Yu</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c270t-ab38dec24d2ea210b7c4b8a5b871841a651ebda29bc6336a57b2f38a93854ed43</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Carbon</topic><topic>Cathodoluminescence</topic><topic>Cementation</topic><topic>Chemistry</topic><topic>Chemistry and Materials Science</topic><topic>Geotechnical Engineering &amp; Applied Earth Sciences</topic><topic>Industrial Chemistry/Chemical Engineering</topic><topic>Innovative Technologies of Oil and Gas</topic><topic>Meteoric water</topic><topic>Mineral Resources</topic><topic>Mollusks</topic><topic>Oil fields</topic><topic>Oxygen isotopes</topic><topic>Pore water</topic><topic>Sandstone</topic><topic>Seawater</topic><topic>Sediments</topic><topic>Strata</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lin, Dan</creatorcontrib><creatorcontrib>Liao, Jijia</creatorcontrib><creatorcontrib>Liao, Mingguang</creatorcontrib><creatorcontrib>Hu, Yu</creatorcontrib><collection>CrossRef</collection><jtitle>Chemistry and technology of fuels and oils</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lin, Dan</au><au>Liao, Jijia</au><au>Liao, Mingguang</au><au>Hu, Yu</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Diagenesis and Genetic Model of Calcareous Interbeds in Marine Strata</atitle><jtitle>Chemistry and technology of fuels and oils</jtitle><stitle>Chem Technol Fuels Oils</stitle><date>2024-05-01</date><risdate>2024</risdate><volume>60</volume><issue>2</issue><spage>374</spage><epage>381</epage><pages>374-381</pages><issn>0009-3092</issn><eissn>1573-8310</eissn><abstract>Calcareous interbeds control the migration of oil and water in marine strata. However, in China, the origins of such calcareous interbeds have not been investigated in detail. In this paper, we present a study of calcareous interbeds in marine strata of the Zhujiang Formation in the Wenchang Oil Field, which is located in the southeast of Hainan Province, China. The lithological characteristics, types and features of diagenesis, and formation of the calcareous interbeds were investigated using core, thin-section, scanning electron microscopy, and cathodoluminescence observations, and stable carbon and oxygen isotope data. The calcareous interbeds consist of mixed sediments, which are dominated by bioclastic limestones containing terrigenous clasts, along with subordinate calcareous sandstone. The interbeds are densely cemented. The bioclasts are dominantly brachiopods, pleopods, and foraminifera, with minor amounts of echinodermata, bivalves, red algae, ostracods, and bryozoa. Diagenesis involved calcitic cementation, associated with relatively weak compaction. Carbon and oxygen isotopic data indicate the pore water that formed the carbonate cement was mostly sourced from seawater and minor amounts of meteoric water. The degree of carbonate cementation was significantly related to the bioclast content. On the basis of our study, a genetic model for the macroscopic and microscopic formation of calcareous interbeds is proposed.</abstract><cop>New York</cop><pub>Springer US</pub><doi>10.1007/s10553-024-01691-0</doi><tpages>8</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0009-3092
ispartof Chemistry and technology of fuels and oils, 2024-05, Vol.60 (2), p.374-381
issn 0009-3092
1573-8310
language eng
recordid cdi_proquest_journals_3059397252
source SpringerLink Journals
subjects Carbon
Cathodoluminescence
Cementation
Chemistry
Chemistry and Materials Science
Geotechnical Engineering & Applied Earth Sciences
Industrial Chemistry/Chemical Engineering
Innovative Technologies of Oil and Gas
Meteoric water
Mineral Resources
Mollusks
Oil fields
Oxygen isotopes
Pore water
Sandstone
Seawater
Sediments
Strata
title Diagenesis and Genetic Model of Calcareous Interbeds in Marine Strata
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-14T01%3A44%3A41IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Diagenesis%20and%20Genetic%20Model%20of%20Calcareous%20Interbeds%20in%20Marine%20Strata&rft.jtitle=Chemistry%20and%20technology%20of%20fuels%20and%20oils&rft.au=Lin,%20Dan&rft.date=2024-05-01&rft.volume=60&rft.issue=2&rft.spage=374&rft.epage=381&rft.pages=374-381&rft.issn=0009-3092&rft.eissn=1573-8310&rft_id=info:doi/10.1007/s10553-024-01691-0&rft_dat=%3Cproquest_cross%3E3059397252%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=3059397252&rft_id=info:pmid/&rfr_iscdi=true