Palaeoseismicity in relation to basin tectonics as revealed from soft-sediment deformation structures of the Lower Triassic Panchet formation, Raniganj basin (Damodar valley), eastern India
The Raniganj basin in the Damodar valley of eastern India is located within the riftogenic Gondwana Master-Basin. The fluvio-lacustrine deposits of the Lower Triassic Panchet formation of the Damodar valley in the study area preserve various soft-sediment deformation structures such as slump folds,...
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| Veröffentlicht in: | Journal of Earth System Science 2011-02, Vol.120 (1), p.167-181 |
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| creator | KUNDU, ABHIK GOSWAMI, BAPI ERIKSSON, PATRICK G CHAKRABORTY, ABHIJIT |
| description | The Raniganj basin in the Damodar valley of eastern India is located within the riftogenic Gondwana Master-Basin. The fluvio-lacustrine deposits of the Lower Triassic Panchet formation of the Damodar valley in the study area preserve various soft-sediment deformation structures such as slump folds, convolute laminae, flame structures, dish-and-pillar structures, sandstone dykes, pseudonodules and syn-sedimentary faults. Although such soft-sediment deformation structures maybe formed by various processes, in the present area the association of these structures, their relation to the adjacent sedimentary rocks and the tectonic and depositional setting of the formation suggest that these structures are seismogenic. Movements along the basin margin and the intra-basinal faults and resultant seismicity with moderate magnitude (2–5 on Richter scale) are thought to have been responsible for the soft-sediment deformations. |
| doi_str_mv | 10.1007/s12040-011-0071-8 |
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The fluvio-lacustrine deposits of the Lower Triassic Panchet formation of the Damodar valley in the study area preserve various soft-sediment deformation structures such as slump folds, convolute laminae, flame structures, dish-and-pillar structures, sandstone dykes, pseudonodules and syn-sedimentary faults. Although such soft-sediment deformation structures maybe formed by various processes, in the present area the association of these structures, their relation to the adjacent sedimentary rocks and the tectonic and depositional setting of the formation suggest that these structures are seismogenic. Movements along the basin margin and the intra-basinal faults and resultant seismicity with moderate magnitude (2–5 on Richter scale) are thought to have been responsible for the soft-sediment deformations.</description><identifier>ISSN: 0253-4126</identifier><identifier>ISSN: 2347-4327</identifier><identifier>EISSN: 0973-774X</identifier><identifier>DOI: 10.1007/s12040-011-0071-8</identifier><language>eng</language><publisher>India: Springer-Verlag</publisher><subject>Deformation ; Earth and Environmental Science ; Earth Sciences ; Earth, ocean, space ; Earthquake magnitude scale ; Exact sciences and technology ; Gondwana ; Lake deposits ; Laminates ; Paleoclimates ; Plate tectonics ; River basins ; Sandstone ; Sediment ; Sedimentary rocks ; Sediments ; Seismicity ; Seismology ; Space Exploration and Astronautics ; Space Sciences (including Extraterrestrial Physics ; Structures ; Tectonics ; Triassic ; Valleys</subject><ispartof>Journal of Earth System Science, 2011-02, Vol.120 (1), p.167-181</ispartof><rights>Indian Academy of Sciences 2011</rights><rights>2015 INIST-CNRS</rights><rights>Indian Academy of Sciences 2011.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a444t-91e6919393d78cf1e8d16fb4993a18719a1a76a9550ec495ae6542c13f1b3b553</citedby><cites>FETCH-LOGICAL-a444t-91e6919393d78cf1e8d16fb4993a18719a1a76a9550ec495ae6542c13f1b3b553</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/s12040-011-0071-8$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12040-011-0071-8$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51297</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=24096601$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>KUNDU, ABHIK</creatorcontrib><creatorcontrib>GOSWAMI, BAPI</creatorcontrib><creatorcontrib>ERIKSSON, PATRICK G</creatorcontrib><creatorcontrib>CHAKRABORTY, ABHIJIT</creatorcontrib><title>Palaeoseismicity in relation to basin tectonics as revealed from soft-sediment deformation structures of the Lower Triassic Panchet formation, Raniganj basin (Damodar valley), eastern India</title><title>Journal of Earth System Science</title><addtitle>J Earth Syst Sci</addtitle><description>The Raniganj basin in the Damodar valley of eastern India is located within the riftogenic Gondwana Master-Basin. 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GOSWAMI, BAPI ; ERIKSSON, PATRICK G ; CHAKRABORTY, ABHIJIT</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a444t-91e6919393d78cf1e8d16fb4993a18719a1a76a9550ec495ae6542c13f1b3b553</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>Deformation</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Earth, ocean, space</topic><topic>Earthquake magnitude scale</topic><topic>Exact sciences and technology</topic><topic>Gondwana</topic><topic>Lake deposits</topic><topic>Laminates</topic><topic>Paleoclimates</topic><topic>Plate tectonics</topic><topic>River basins</topic><topic>Sandstone</topic><topic>Sediment</topic><topic>Sedimentary rocks</topic><topic>Sediments</topic><topic>Seismicity</topic><topic>Seismology</topic><topic>Space Exploration and Astronautics</topic><topic>Space Sciences (including Extraterrestrial Physics</topic><topic>Structures</topic><topic>Tectonics</topic><topic>Triassic</topic><topic>Valleys</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>KUNDU, ABHIK</creatorcontrib><creatorcontrib>GOSWAMI, BAPI</creatorcontrib><creatorcontrib>ERIKSSON, PATRICK G</creatorcontrib><creatorcontrib>CHAKRABORTY, ABHIJIT</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources 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 One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</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>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>Environmental 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>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Journal of Earth System Science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>KUNDU, ABHIK</au><au>GOSWAMI, BAPI</au><au>ERIKSSON, PATRICK G</au><au>CHAKRABORTY, ABHIJIT</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Palaeoseismicity in relation to basin tectonics as revealed from soft-sediment deformation structures of the Lower Triassic Panchet formation, Raniganj basin (Damodar valley), eastern India</atitle><jtitle>Journal of Earth System Science</jtitle><stitle>J Earth Syst Sci</stitle><date>2011-02-01</date><risdate>2011</risdate><volume>120</volume><issue>1</issue><spage>167</spage><epage>181</epage><pages>167-181</pages><issn>0253-4126</issn><issn>2347-4327</issn><eissn>0973-774X</eissn><abstract>The Raniganj basin in the Damodar valley of eastern India is located within the riftogenic Gondwana Master-Basin. The fluvio-lacustrine deposits of the Lower Triassic Panchet formation of the Damodar valley in the study area preserve various soft-sediment deformation structures such as slump folds, convolute laminae, flame structures, dish-and-pillar structures, sandstone dykes, pseudonodules and syn-sedimentary faults. Although such soft-sediment deformation structures maybe formed by various processes, in the present area the association of these structures, their relation to the adjacent sedimentary rocks and the tectonic and depositional setting of the formation suggest that these structures are seismogenic. Movements along the basin margin and the intra-basinal faults and resultant seismicity with moderate magnitude (2–5 on Richter scale) are thought to have been responsible for the soft-sediment deformations.</abstract><cop>India</cop><pub>Springer-Verlag</pub><doi>10.1007/s12040-011-0071-8</doi><tpages>15</tpages><oa>free_for_read</oa></addata></record> |
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| source | Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Indian Academy of Sciences; Springer Nature - Complete Springer Journals |
| subjects | Deformation Earth and Environmental Science Earth Sciences Earth, ocean, space Earthquake magnitude scale Exact sciences and technology Gondwana Lake deposits Laminates Paleoclimates Plate tectonics River basins Sandstone Sediment Sedimentary rocks Sediments Seismicity Seismology Space Exploration and Astronautics Space Sciences (including Extraterrestrial Physics Structures Tectonics Triassic Valleys |
| title | Palaeoseismicity in relation to basin tectonics as revealed from soft-sediment deformation structures of the Lower Triassic Panchet formation, Raniganj basin (Damodar valley), eastern India |
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