Distribution and controlling factors of the oolitic shoal deposits in the sequence stratigraphic framework: a case study of the Lower Triassic Feixianguan Formation, eastern Sichuan Basin, China
As one of the main reservoirs types in the Sichuan Basin, the granular shoal reservoirs of the Feixianguan Formation have great potential for oil and gas exploration. Therefore, it is very important to study the sedimentary evolution characteristics and the distribution of shoal deposits of the Feix...
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| description | As one of the main reservoirs types in the Sichuan Basin, the granular shoal reservoirs of the Feixianguan Formation have great potential for oil and gas exploration. Therefore, it is very important to study the sedimentary evolution characteristics and the distribution of shoal deposits of the Feixianguan Formation. In this paper, the sequence stratigraphy, sedimentary characteristics and distribution characteristics of the granular shoal deposits of the southwestern section of the Kaijiang–Liangping Trough in the Sichuan Basin were investigated, through core observations, thin section analysis, and field profiles measurement and sampling, combined with well-logging data and interpretations of two and three-dimensional seismic data of the local area. According to the identification marks, three sequence boundaries (SB1, SB2, and SB3) and two third-order sequences (SQ1 and SQ2) were identified, and a transgressive systems tract (TST) and highstand systems tract (HST) were distinguished in each third-order sequence. The analysis of the Feixianguan Formation sedimentary facies indicated that this formation developed in a carbonate platform setting. In the depositional period of SQ1, the study area inherited the sedimentary pattern of the Changxing Formation and developed carbonate platform depositions. During the SQ1-HST stage, the platform margin shoals and the intra-platform shoals in the study area were relatively well developed. During the SQ2-TST period, oolitic shoals were developed in the region, but their thicknesses were smaller than those of SQ1-HST. In addition, the distribution pattern of sedimentary facies was similar to that of SQ1-HST. The platform marginal zone was relatively narrow at that time, whereas the open platform was more widely distributed, and the distribution areas of platform margin shoals and intra-platform oolitic shoals were relatively limited. During the depositional period of SQ2-TST, the sea level dropped to the lowest level of the studied interval, and limited and evaporation platform facies developed in the study area. Based on previous studies, the influence of different factors on the deposition of the shoals in the Feixianguan Formation were evaluated. The results showed that under the influence of sea level, basement faults, and hydrodynamic conditions, the platform margin area in the study area was more favorable to the development of granular shoals, and the growth model of the granular shoals was “accretion before |
| doi_str_mv | 10.1007/s13146-021-00680-2 |
| format | Article |
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Therefore, it is very important to study the sedimentary evolution characteristics and the distribution of shoal deposits of the Feixianguan Formation. In this paper, the sequence stratigraphy, sedimentary characteristics and distribution characteristics of the granular shoal deposits of the southwestern section of the Kaijiang–Liangping Trough in the Sichuan Basin were investigated, through core observations, thin section analysis, and field profiles measurement and sampling, combined with well-logging data and interpretations of two and three-dimensional seismic data of the local area. According to the identification marks, three sequence boundaries (SB1, SB2, and SB3) and two third-order sequences (SQ1 and SQ2) were identified, and a transgressive systems tract (TST) and highstand systems tract (HST) were distinguished in each third-order sequence. The analysis of the Feixianguan Formation sedimentary facies indicated that this formation developed in a carbonate platform setting. In the depositional period of SQ1, the study area inherited the sedimentary pattern of the Changxing Formation and developed carbonate platform depositions. During the SQ1-HST stage, the platform margin shoals and the intra-platform shoals in the study area were relatively well developed. During the SQ2-TST period, oolitic shoals were developed in the region, but their thicknesses were smaller than those of SQ1-HST. In addition, the distribution pattern of sedimentary facies was similar to that of SQ1-HST. The platform marginal zone was relatively narrow at that time, whereas the open platform was more widely distributed, and the distribution areas of platform margin shoals and intra-platform oolitic shoals were relatively limited. During the depositional period of SQ2-TST, the sea level dropped to the lowest level of the studied interval, and limited and evaporation platform facies developed in the study area. Based on previous studies, the influence of different factors on the deposition of the shoals in the Feixianguan Formation were evaluated. The results showed that under the influence of sea level, basement faults, and hydrodynamic conditions, the platform margin area in the study area was more favorable to the development of granular shoals, and the growth model of the granular shoals was “accretion before migration”.</description><identifier>ISSN: 0891-2556</identifier><identifier>EISSN: 1878-5212</identifier><identifier>DOI: 10.1007/s13146-021-00680-2</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Accretion ; Carbonates ; Data logging ; Deposition ; Deposits ; Distribution ; Distribution patterns ; Earth and Environmental Science ; Earth Sciences ; Evaporation ; Geology ; Growth models ; Hydrodynamics ; Logging ; Mineral Resources ; Mineralogy ; Natural gas exploration ; Oil and gas exploration ; Oil exploration ; Original Article ; Platforms (geology) ; Reservoirs ; Sea level ; Sedimentary facies ; Seismic data ; Sequence stratigraphy ; Sequences ; Sequencing ; Shoals ; Stratigraphy ; Triassic</subject><ispartof>Carbonates and evaporites, 2021-03, Vol.36 (1), Article 17</ispartof><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH, DE part of Springer Nature 2021</rights><rights>The Author(s), under exclusive licence to Springer-Verlag GmbH, DE part of Springer Nature 2021.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a342t-5f659cfacf2cca3315367346be9d87e9f91d4dde447acee2300f8c3ea6b6e3243</citedby><cites>FETCH-LOGICAL-a342t-5f659cfacf2cca3315367346be9d87e9f91d4dde447acee2300f8c3ea6b6e3243</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/s13146-021-00680-2$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s13146-021-00680-2$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,41487,42556,51318</link.rule.ids></links><search><creatorcontrib>Zuo, Mingtao</creatorcontrib><creatorcontrib>Hu, Zhonggui</creatorcontrib><creatorcontrib>Hu, Mingyi</creatorcontrib><creatorcontrib>Niu, Xing</creatorcontrib><creatorcontrib>Dong, Qingmin</creatorcontrib><title>Distribution and controlling factors of the oolitic shoal deposits in the sequence stratigraphic framework: a case study of the Lower Triassic Feixianguan Formation, eastern Sichuan Basin, China</title><title>Carbonates and evaporites</title><addtitle>Carbonates Evaporites</addtitle><description>As one of the main reservoirs types in the Sichuan Basin, the granular shoal reservoirs of the Feixianguan Formation have great potential for oil and gas exploration. Therefore, it is very important to study the sedimentary evolution characteristics and the distribution of shoal deposits of the Feixianguan Formation. In this paper, the sequence stratigraphy, sedimentary characteristics and distribution characteristics of the granular shoal deposits of the southwestern section of the Kaijiang–Liangping Trough in the Sichuan Basin were investigated, through core observations, thin section analysis, and field profiles measurement and sampling, combined with well-logging data and interpretations of two and three-dimensional seismic data of the local area. According to the identification marks, three sequence boundaries (SB1, SB2, and SB3) and two third-order sequences (SQ1 and SQ2) were identified, and a transgressive systems tract (TST) and highstand systems tract (HST) were distinguished in each third-order sequence. The analysis of the Feixianguan Formation sedimentary facies indicated that this formation developed in a carbonate platform setting. In the depositional period of SQ1, the study area inherited the sedimentary pattern of the Changxing Formation and developed carbonate platform depositions. During the SQ1-HST stage, the platform margin shoals and the intra-platform shoals in the study area were relatively well developed. During the SQ2-TST period, oolitic shoals were developed in the region, but their thicknesses were smaller than those of SQ1-HST. In addition, the distribution pattern of sedimentary facies was similar to that of SQ1-HST. The platform marginal zone was relatively narrow at that time, whereas the open platform was more widely distributed, and the distribution areas of platform margin shoals and intra-platform oolitic shoals were relatively limited. During the depositional period of SQ2-TST, the sea level dropped to the lowest level of the studied interval, and limited and evaporation platform facies developed in the study area. Based on previous studies, the influence of different factors on the deposition of the shoals in the Feixianguan Formation were evaluated. The results showed that under the influence of sea level, basement faults, and hydrodynamic conditions, the platform margin area in the study area was more favorable to the development of granular shoals, and the growth model of the granular shoals was “accretion before migration”.</description><subject>Accretion</subject><subject>Carbonates</subject><subject>Data logging</subject><subject>Deposition</subject><subject>Deposits</subject><subject>Distribution</subject><subject>Distribution patterns</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Evaporation</subject><subject>Geology</subject><subject>Growth models</subject><subject>Hydrodynamics</subject><subject>Logging</subject><subject>Mineral Resources</subject><subject>Mineralogy</subject><subject>Natural gas exploration</subject><subject>Oil and gas exploration</subject><subject>Oil exploration</subject><subject>Original Article</subject><subject>Platforms (geology)</subject><subject>Reservoirs</subject><subject>Sea level</subject><subject>Sedimentary facies</subject><subject>Seismic data</subject><subject>Sequence stratigraphy</subject><subject>Sequences</subject><subject>Sequencing</subject><subject>Shoals</subject><subject>Stratigraphy</subject><subject>Triassic</subject><issn>0891-2556</issn><issn>1878-5212</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>AFKRA</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><recordid>eNp9kc1u1DAUhSNEJYbCC7CyxJaA_5I47GBgAGmkLlrW1h3nZuKSsQdfR6Wvx5Ph6YDYdWXL5zvn-upU1SvB3wrOu3cklNBtzaWoOW8Nr-WTaiVMZ-pGCvm0WnHTi1o2Tfusek50W6Be9_2q-v3JU05-t2QfA4MwMBdDTnGefdizEVyOiVgcWZ6QxTj77B2jKcLMBjxG8pmYDw8q4c8FgyuXnCD7fYLjVOAxwQHvYvrxngFzQCd9Ge7_ZW7jHSZ2kzwQFXqD_peHsF8gsE1MBzj96w1DoIwpsGvvppP0EciX5_XkA7yoLkaYCV_-PS-r75vPN-uv9fbqy7f1h20NSstcN2Pb9K5sNErnQCnRqLZTut1hP5gO-7EXgx4G1LoDhygV56NxCqHdtaikVpfV63PuMcWyKWV7G5cUykgrda-MUaoxhZJnyqVIlHC0x-QPkO6t4PbUlT13ZUtX9qErK4tJnU1U4LDH9D_6EdcfEWWcTg</recordid><startdate>20210301</startdate><enddate>20210301</enddate><creator>Zuo, Mingtao</creator><creator>Hu, Zhonggui</creator><creator>Hu, Mingyi</creator><creator>Niu, Xing</creator><creator>Dong, Qingmin</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><scope>PRINS</scope></search><sort><creationdate>20210301</creationdate><title>Distribution and controlling factors of the oolitic shoal deposits in the sequence stratigraphic framework: a case study of the Lower Triassic Feixianguan Formation, eastern Sichuan Basin, China</title><author>Zuo, Mingtao ; Hu, Zhonggui ; Hu, Mingyi ; Niu, Xing ; Dong, Qingmin</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a342t-5f659cfacf2cca3315367346be9d87e9f91d4dde447acee2300f8c3ea6b6e3243</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Accretion</topic><topic>Carbonates</topic><topic>Data logging</topic><topic>Deposition</topic><topic>Deposits</topic><topic>Distribution</topic><topic>Distribution patterns</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Evaporation</topic><topic>Geology</topic><topic>Growth models</topic><topic>Hydrodynamics</topic><topic>Logging</topic><topic>Mineral Resources</topic><topic>Mineralogy</topic><topic>Natural gas exploration</topic><topic>Oil and gas exploration</topic><topic>Oil exploration</topic><topic>Original Article</topic><topic>Platforms (geology)</topic><topic>Reservoirs</topic><topic>Sea level</topic><topic>Sedimentary facies</topic><topic>Seismic data</topic><topic>Sequence stratigraphy</topic><topic>Sequences</topic><topic>Sequencing</topic><topic>Shoals</topic><topic>Stratigraphy</topic><topic>Triassic</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zuo, Mingtao</creatorcontrib><creatorcontrib>Hu, Zhonggui</creatorcontrib><creatorcontrib>Hu, Mingyi</creatorcontrib><creatorcontrib>Niu, Xing</creatorcontrib><creatorcontrib>Dong, Qingmin</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>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</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</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><collection>ProQuest Central China</collection><jtitle>Carbonates and evaporites</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zuo, Mingtao</au><au>Hu, Zhonggui</au><au>Hu, Mingyi</au><au>Niu, Xing</au><au>Dong, Qingmin</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Distribution and controlling factors of the oolitic shoal deposits in the sequence stratigraphic framework: a case study of the Lower Triassic Feixianguan Formation, eastern Sichuan Basin, China</atitle><jtitle>Carbonates and evaporites</jtitle><stitle>Carbonates Evaporites</stitle><date>2021-03-01</date><risdate>2021</risdate><volume>36</volume><issue>1</issue><artnum>17</artnum><issn>0891-2556</issn><eissn>1878-5212</eissn><abstract>As one of the main reservoirs types in the Sichuan Basin, the granular shoal reservoirs of the Feixianguan Formation have great potential for oil and gas exploration. Therefore, it is very important to study the sedimentary evolution characteristics and the distribution of shoal deposits of the Feixianguan Formation. In this paper, the sequence stratigraphy, sedimentary characteristics and distribution characteristics of the granular shoal deposits of the southwestern section of the Kaijiang–Liangping Trough in the Sichuan Basin were investigated, through core observations, thin section analysis, and field profiles measurement and sampling, combined with well-logging data and interpretations of two and three-dimensional seismic data of the local area. According to the identification marks, three sequence boundaries (SB1, SB2, and SB3) and two third-order sequences (SQ1 and SQ2) were identified, and a transgressive systems tract (TST) and highstand systems tract (HST) were distinguished in each third-order sequence. The analysis of the Feixianguan Formation sedimentary facies indicated that this formation developed in a carbonate platform setting. In the depositional period of SQ1, the study area inherited the sedimentary pattern of the Changxing Formation and developed carbonate platform depositions. During the SQ1-HST stage, the platform margin shoals and the intra-platform shoals in the study area were relatively well developed. During the SQ2-TST period, oolitic shoals were developed in the region, but their thicknesses were smaller than those of SQ1-HST. In addition, the distribution pattern of sedimentary facies was similar to that of SQ1-HST. The platform marginal zone was relatively narrow at that time, whereas the open platform was more widely distributed, and the distribution areas of platform margin shoals and intra-platform oolitic shoals were relatively limited. During the depositional period of SQ2-TST, the sea level dropped to the lowest level of the studied interval, and limited and evaporation platform facies developed in the study area. Based on previous studies, the influence of different factors on the deposition of the shoals in the Feixianguan Formation were evaluated. The results showed that under the influence of sea level, basement faults, and hydrodynamic conditions, the platform margin area in the study area was more favorable to the development of granular shoals, and the growth model of the granular shoals was “accretion before migration”.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s13146-021-00680-2</doi></addata></record> |
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| subjects | Accretion Carbonates Data logging Deposition Deposits Distribution Distribution patterns Earth and Environmental Science Earth Sciences Evaporation Geology Growth models Hydrodynamics Logging Mineral Resources Mineralogy Natural gas exploration Oil and gas exploration Oil exploration Original Article Platforms (geology) Reservoirs Sea level Sedimentary facies Seismic data Sequence stratigraphy Sequences Sequencing Shoals Stratigraphy Triassic |
| title | Distribution and controlling factors of the oolitic shoal deposits in the sequence stratigraphic framework: a case study of the Lower Triassic Feixianguan Formation, eastern Sichuan Basin, China |
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