Latest Neogene-Quaternary seismic stratigraphy and post-opening tectonic history on the southwest margin of the Ulleung Basin, East Sea
Sequence analysis of 2D seismic profiles and sediment data from the southwestern margin of Ulleung Basin reveals that the latest Neogene-Quaternary deposits comprise five depositional sequences (DS1–DS5), separated by erosional unconformities (H1–H5). The lower two sequences (DS1 and DS2), correlate...
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| Veröffentlicht in: | Marine geophysical researches 2022-09, Vol.43 (3), Article 36 |
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| description | Sequence analysis of 2D seismic profiles and sediment data from the southwestern margin of Ulleung Basin reveals that the latest Neogene-Quaternary deposits comprise five depositional sequences (DS1–DS5), separated by erosional unconformities (H1–H5). The lower two sequences (DS1 and DS2), correlated with the Miocene strata, are acoustically characterized by hummocky and chaotic seismic facies, and were significantly deformed with several faults and folds. During the late Miocene, distinct geologic structures, including the Ulsan Structure (US), Dolgorae Thrust Belt (DTB), and Gorae Structure (GS) were also developed sequentially, which were closely related to formation of lower two sequences. However, the upper three sequences (DS3–DS5), belonging to the Plio-Quaternary strata, is acoustically characterized by well-stratified and prograding reflection configurations, and remained relatively undeformed. The tectonic movement related to the regional structures (US, DTB, and GS) was almost stopped since the Pliocene, whereas the part of the GS has been uplifted until the present. These results indicated that sedimentation for the upper three sequence since the Pliocene was mainly influenced by periodically repeated sea-level changes rather than tectonic activity. |
| doi_str_mv | 10.1007/s11001-022-09496-8 |
| format | Article |
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The lower two sequences (DS1 and DS2), correlated with the Miocene strata, are acoustically characterized by hummocky and chaotic seismic facies, and were significantly deformed with several faults and folds. During the late Miocene, distinct geologic structures, including the Ulsan Structure (US), Dolgorae Thrust Belt (DTB), and Gorae Structure (GS) were also developed sequentially, which were closely related to formation of lower two sequences. However, the upper three sequences (DS3–DS5), belonging to the Plio-Quaternary strata, is acoustically characterized by well-stratified and prograding reflection configurations, and remained relatively undeformed. The tectonic movement related to the regional structures (US, DTB, and GS) was almost stopped since the Pliocene, whereas the part of the GS has been uplifted until the present. 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The lower two sequences (DS1 and DS2), correlated with the Miocene strata, are acoustically characterized by hummocky and chaotic seismic facies, and were significantly deformed with several faults and folds. During the late Miocene, distinct geologic structures, including the Ulsan Structure (US), Dolgorae Thrust Belt (DTB), and Gorae Structure (GS) were also developed sequentially, which were closely related to formation of lower two sequences. However, the upper three sequences (DS3–DS5), belonging to the Plio-Quaternary strata, is acoustically characterized by well-stratified and prograding reflection configurations, and remained relatively undeformed. The tectonic movement related to the regional structures (US, DTB, and GS) was almost stopped since the Pliocene, whereas the part of the GS has been uplifted until the present. 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Yoo, Dong-Geun ; Lee, Gwang-Soo ; Hong, Seok-Hwi ; Kong, Gee-Soo ; Kim, Byoung-Yeop</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c319t-82c2eed6d2b98557b375fa3ccf2ef32c36e0831b6a574249280ab5c45ad255833</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>East Sea</topic><topic>Geological structures</topic><topic>Geophysics/Geodesy</topic><topic>Miocene</topic><topic>Neogene</topic><topic>Oceanography</topic><topic>Offshore Engineering</topic><topic>Original Research Paper</topic><topic>Pliocene</topic><topic>Quaternary</topic><topic>Quaternary deposits</topic><topic>Sea level changes</topic><topic>Sedimentary facies</topic><topic>Sediments</topic><topic>Seismic profiles</topic><topic>Seismic stratigraphy</topic><topic>Sequencing</topic><topic>Special Issue: Geological implications for submarine geohazards</topic><topic>Stratigraphy</topic><topic>Stress state</topic><topic>Tectonics</topic><topic>Ulleung Basin</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Lee, Bo-Ram</creatorcontrib><creatorcontrib>Yoo, Dong-Geun</creatorcontrib><creatorcontrib>Lee, Gwang-Soo</creatorcontrib><creatorcontrib>Hong, Seok-Hwi</creatorcontrib><creatorcontrib>Kong, Gee-Soo</creatorcontrib><creatorcontrib>Kim, Byoung-Yeop</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</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 Basic</collection><jtitle>Marine geophysical researches</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Lee, Bo-Ram</au><au>Yoo, Dong-Geun</au><au>Lee, Gwang-Soo</au><au>Hong, Seok-Hwi</au><au>Kong, Gee-Soo</au><au>Kim, Byoung-Yeop</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Latest Neogene-Quaternary seismic stratigraphy and post-opening tectonic history on the southwest margin of the Ulleung Basin, East Sea</atitle><jtitle>Marine geophysical researches</jtitle><stitle>Mar Geophys Res</stitle><date>2022-09-01</date><risdate>2022</risdate><volume>43</volume><issue>3</issue><artnum>36</artnum><issn>0025-3235</issn><eissn>1573-0581</eissn><abstract>Sequence analysis of 2D seismic profiles and sediment data from the southwestern margin of Ulleung Basin reveals that the latest Neogene-Quaternary deposits comprise five depositional sequences (DS1–DS5), separated by erosional unconformities (H1–H5). The lower two sequences (DS1 and DS2), correlated with the Miocene strata, are acoustically characterized by hummocky and chaotic seismic facies, and were significantly deformed with several faults and folds. During the late Miocene, distinct geologic structures, including the Ulsan Structure (US), Dolgorae Thrust Belt (DTB), and Gorae Structure (GS) were also developed sequentially, which were closely related to formation of lower two sequences. However, the upper three sequences (DS3–DS5), belonging to the Plio-Quaternary strata, is acoustically characterized by well-stratified and prograding reflection configurations, and remained relatively undeformed. The tectonic movement related to the regional structures (US, DTB, and GS) was almost stopped since the Pliocene, whereas the part of the GS has been uplifted until the present. These results indicated that sedimentation for the upper three sequence since the Pliocene was mainly influenced by periodically repeated sea-level changes rather than tectonic activity.</abstract><cop>Dordrecht</cop><pub>Springer Netherlands</pub><doi>10.1007/s11001-022-09496-8</doi></addata></record> |
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| subjects | Earth and Environmental Science Earth Sciences East Sea Geological structures Geophysics/Geodesy Miocene Neogene Oceanography Offshore Engineering Original Research Paper Pliocene Quaternary Quaternary deposits Sea level changes Sedimentary facies Sediments Seismic profiles Seismic stratigraphy Sequencing Special Issue: Geological implications for submarine geohazards Stratigraphy Stress state Tectonics Ulleung Basin |
| title | Latest Neogene-Quaternary seismic stratigraphy and post-opening tectonic history on the southwest margin of the Ulleung Basin, East Sea |
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