Rapid spatiotemporal variations in rift structure during development of the Corinth Rift, central Greece
The Corinth Rift, central Greece, enables analysis of early rift development as it is young (
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| Veröffentlicht in: | Tectonics (Washington, D.C.) D.C.), 2016-05, Vol.35 (5), p.1225-1248 |
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| creator | Nixon, Casey W. McNeill, Lisa C. Bull, Jonathan M. Bell, Rebecca E. Gawthorpe, Robert L. Henstock, Timothy J. Christodoulou, Dimitris Ford, Mary Taylor, Brian Sakellariou, Dimitris Ferentinos, George Papatheodorou, George Leeder, Mike R. Collier, Richard E.LI Goodliffe, Andrew M. Sachpazi, Maria Kranis, Haralambos |
| description | The Corinth Rift, central Greece, enables analysis of early rift development as it is young ( |
| doi_str_mv | 10.1002/2015TC004026 |
| format | Article |
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Key Points
Offshore Corinth Rift evolution is investigated at high spatial and temporal resolution
Rift migration and localization of deformation are significant within the Corinth Rift
Changes in rift geometry and linkage of major rift faults occur at rapid 100 kyr timescales</description><identifier>ISSN: 0278-7407</identifier><identifier>EISSN: 1944-9194</identifier><identifier>DOI: 10.1002/2015TC004026</identifier><identifier>CODEN: TCTNDM</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>border faults ; Corinth Rift ; Deformation ; Earth Sciences ; fault linkage ; Plate tectonics ; rift evolution ; rift symmetry ; Sciences of the Universe ; sedimentary basins ; Seismology ; Tectonics</subject><ispartof>Tectonics (Washington, D.C.), 2016-05, Vol.35 (5), p.1225-1248</ispartof><rights>2016. The Authors.</rights><rights>2016. American Geophysical Union. All Rights Reserved.</rights><rights>Attribution</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4550-8fcfd8bb67dc9ddc7ab23ea43b2a4ceaeed7340b6641a5a2ed182e0a9589b5d03</citedby><cites>FETCH-LOGICAL-c4550-8fcfd8bb67dc9ddc7ab23ea43b2a4ceaeed7340b6641a5a2ed182e0a9589b5d03</cites><orcidid>0000-0003-3732-1900 ; 0000-0002-4151-7909 ; 0000-0002-3012-6865</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2F2015TC004026$$EPDF$$P50$$Gwiley$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2F2015TC004026$$EHTML$$P50$$Gwiley$$Hfree_for_read</linktohtml><link.rule.ids>230,314,776,780,881,1411,1427,11493,27901,27902,45550,45551,46384,46443,46808,46867</link.rule.ids><backlink>$$Uhttps://hal.science/hal-01416610$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Nixon, Casey W.</creatorcontrib><creatorcontrib>McNeill, Lisa C.</creatorcontrib><creatorcontrib>Bull, Jonathan M.</creatorcontrib><creatorcontrib>Bell, Rebecca E.</creatorcontrib><creatorcontrib>Gawthorpe, Robert L.</creatorcontrib><creatorcontrib>Henstock, Timothy J.</creatorcontrib><creatorcontrib>Christodoulou, Dimitris</creatorcontrib><creatorcontrib>Ford, Mary</creatorcontrib><creatorcontrib>Taylor, Brian</creatorcontrib><creatorcontrib>Sakellariou, Dimitris</creatorcontrib><creatorcontrib>Ferentinos, George</creatorcontrib><creatorcontrib>Papatheodorou, George</creatorcontrib><creatorcontrib>Leeder, Mike R.</creatorcontrib><creatorcontrib>Collier, Richard E.LI</creatorcontrib><creatorcontrib>Goodliffe, Andrew M.</creatorcontrib><creatorcontrib>Sachpazi, Maria</creatorcontrib><creatorcontrib>Kranis, Haralambos</creatorcontrib><title>Rapid spatiotemporal variations in rift structure during development of the Corinth Rift, central Greece</title><title>Tectonics (Washington, D.C.)</title><description>The Corinth Rift, central Greece, enables analysis of early rift development as it is young (<5 Ma) and highly active and its full history is recorded at high resolution by sedimentary systems. A complete compilation of marine geophysical data, complemented by onshore data, is used to develop a high‐resolution chronostratigraphy and detailed fault history for the offshore Corinth Rift, integrating interpretations and reconciling previous discrepancies. Rift migration and localization of deformation have been significant within the rift since inception. Over the last circa 2 Myr the rift transitioned from a spatially complex rift to a uniform asymmetric rift, but this transition did not occur synchronously along strike. Isochore maps at circa 100 kyr intervals illustrate a change in fault polarity within the short interval circa 620–340 ka, characterized by progressive transfer of activity from major south dipping faults to north dipping faults and southward migration of discrete depocenters at ~30 m/kyr. Since circa 340 ka there has been localization and linkage of the dominant north dipping border fault system along the southern rift margin, demonstrated by lateral growth of discrete depocenters at ~40 m/kyr. A single central depocenter formed by circa 130 ka, indicating full fault linkage. These results indicate that rift localization is progressive (not instantaneous) and can be synchronous once a rift border fault system is established. This study illustrates that development processes within young rifts occur at 100 kyr timescales, including rapid changes in rift symmetry and growth and linkage of major rift faults.
Key Points
Offshore Corinth Rift evolution is investigated at high spatial and temporal resolution
Rift migration and localization of deformation are significant within the Corinth Rift
Changes in rift geometry and linkage of major rift faults occur at rapid 100 kyr timescales</description><subject>border faults</subject><subject>Corinth Rift</subject><subject>Deformation</subject><subject>Earth Sciences</subject><subject>fault linkage</subject><subject>Plate tectonics</subject><subject>rift evolution</subject><subject>rift symmetry</subject><subject>Sciences of the Universe</subject><subject>sedimentary basins</subject><subject>Seismology</subject><subject>Tectonics</subject><issn>0278-7407</issn><issn>1944-9194</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><recordid>eNp90VFrFDEQAOAgCp61b_6AgC8KXTvJJpvdx7LUVjgolOtzyCazXsreZk2yJ_335jgR8cGXCcx8M2QYQj4w-MIA-DUHJnc9gADevCIb1glRdSW-Jhvgqq2UAPWWvEvpGYAJ2TQbsn80i3c0LSb7kPGwhGgmejTRnxJzon6m0Y-ZphxXm9eI1K3Rz9-pwyNOYTngnGkYad4j7UOp5D19LA1X1JbKadhdRLT4nrwZzZTw8vd7QZ6-3u76-2r7cPetv9lWVkgJVTva0bXD0ChnO-esMgOv0Yh64EZYNIhO1QKGphHMSMPRsZYjmE623SAd1Bfk83nu3kx6if5g4osOxuv7m60-5crmrGkYHFmxn852ieHHiinrg08Wp8nMGNakWQutAiGhK_TjP_Q5rHEum2imOiVqoSQv6uqsbAwpRRz__ICBPp1I_32iwusz_-knfPmv1bvbfsdBMKh_AUGikso</recordid><startdate>201605</startdate><enddate>201605</enddate><creator>Nixon, Casey W.</creator><creator>McNeill, Lisa C.</creator><creator>Bull, Jonathan M.</creator><creator>Bell, Rebecca E.</creator><creator>Gawthorpe, Robert L.</creator><creator>Henstock, Timothy J.</creator><creator>Christodoulou, Dimitris</creator><creator>Ford, Mary</creator><creator>Taylor, Brian</creator><creator>Sakellariou, Dimitris</creator><creator>Ferentinos, George</creator><creator>Papatheodorou, George</creator><creator>Leeder, Mike R.</creator><creator>Collier, Richard E.LI</creator><creator>Goodliffe, Andrew M.</creator><creator>Sachpazi, Maria</creator><creator>Kranis, Haralambos</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union (AGU)</general><scope>24P</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0003-3732-1900</orcidid><orcidid>https://orcid.org/0000-0002-4151-7909</orcidid><orcidid>https://orcid.org/0000-0002-3012-6865</orcidid></search><sort><creationdate>201605</creationdate><title>Rapid spatiotemporal variations in rift structure during development of the Corinth Rift, central Greece</title><author>Nixon, Casey W. ; McNeill, Lisa C. ; Bull, Jonathan M. ; Bell, Rebecca E. ; Gawthorpe, Robert L. ; Henstock, Timothy J. ; Christodoulou, Dimitris ; Ford, Mary ; Taylor, Brian ; Sakellariou, Dimitris ; Ferentinos, George ; Papatheodorou, George ; Leeder, Mike R. ; Collier, Richard E.LI ; Goodliffe, Andrew M. ; Sachpazi, Maria ; Kranis, Haralambos</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4550-8fcfd8bb67dc9ddc7ab23ea43b2a4ceaeed7340b6641a5a2ed182e0a9589b5d03</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>border faults</topic><topic>Corinth Rift</topic><topic>Deformation</topic><topic>Earth Sciences</topic><topic>fault linkage</topic><topic>Plate tectonics</topic><topic>rift evolution</topic><topic>rift symmetry</topic><topic>Sciences of the Universe</topic><topic>sedimentary basins</topic><topic>Seismology</topic><topic>Tectonics</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Nixon, Casey W.</creatorcontrib><creatorcontrib>McNeill, Lisa C.</creatorcontrib><creatorcontrib>Bull, Jonathan M.</creatorcontrib><creatorcontrib>Bell, Rebecca E.</creatorcontrib><creatorcontrib>Gawthorpe, Robert L.</creatorcontrib><creatorcontrib>Henstock, Timothy J.</creatorcontrib><creatorcontrib>Christodoulou, Dimitris</creatorcontrib><creatorcontrib>Ford, Mary</creatorcontrib><creatorcontrib>Taylor, Brian</creatorcontrib><creatorcontrib>Sakellariou, Dimitris</creatorcontrib><creatorcontrib>Ferentinos, George</creatorcontrib><creatorcontrib>Papatheodorou, George</creatorcontrib><creatorcontrib>Leeder, Mike R.</creatorcontrib><creatorcontrib>Collier, Richard E.LI</creatorcontrib><creatorcontrib>Goodliffe, Andrew M.</creatorcontrib><creatorcontrib>Sachpazi, Maria</creatorcontrib><creatorcontrib>Kranis, Haralambos</creatorcontrib><collection>Wiley Online Library Open Access</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Hyper Article en Ligne (HAL)</collection><collection>Hyper Article en Ligne (HAL) (Open Access)</collection><jtitle>Tectonics (Washington, D.C.)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Nixon, Casey W.</au><au>McNeill, Lisa C.</au><au>Bull, Jonathan M.</au><au>Bell, Rebecca E.</au><au>Gawthorpe, Robert L.</au><au>Henstock, Timothy J.</au><au>Christodoulou, Dimitris</au><au>Ford, Mary</au><au>Taylor, Brian</au><au>Sakellariou, Dimitris</au><au>Ferentinos, George</au><au>Papatheodorou, George</au><au>Leeder, Mike R.</au><au>Collier, Richard E.LI</au><au>Goodliffe, Andrew M.</au><au>Sachpazi, Maria</au><au>Kranis, Haralambos</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Rapid spatiotemporal variations in rift structure during development of the Corinth Rift, central Greece</atitle><jtitle>Tectonics (Washington, D.C.)</jtitle><date>2016-05</date><risdate>2016</risdate><volume>35</volume><issue>5</issue><spage>1225</spage><epage>1248</epage><pages>1225-1248</pages><issn>0278-7407</issn><eissn>1944-9194</eissn><coden>TCTNDM</coden><abstract>The Corinth Rift, central Greece, enables analysis of early rift development as it is young (<5 Ma) and highly active and its full history is recorded at high resolution by sedimentary systems. A complete compilation of marine geophysical data, complemented by onshore data, is used to develop a high‐resolution chronostratigraphy and detailed fault history for the offshore Corinth Rift, integrating interpretations and reconciling previous discrepancies. Rift migration and localization of deformation have been significant within the rift since inception. Over the last circa 2 Myr the rift transitioned from a spatially complex rift to a uniform asymmetric rift, but this transition did not occur synchronously along strike. Isochore maps at circa 100 kyr intervals illustrate a change in fault polarity within the short interval circa 620–340 ka, characterized by progressive transfer of activity from major south dipping faults to north dipping faults and southward migration of discrete depocenters at ~30 m/kyr. Since circa 340 ka there has been localization and linkage of the dominant north dipping border fault system along the southern rift margin, demonstrated by lateral growth of discrete depocenters at ~40 m/kyr. A single central depocenter formed by circa 130 ka, indicating full fault linkage. These results indicate that rift localization is progressive (not instantaneous) and can be synchronous once a rift border fault system is established. This study illustrates that development processes within young rifts occur at 100 kyr timescales, including rapid changes in rift symmetry and growth and linkage of major rift faults.
Key Points
Offshore Corinth Rift evolution is investigated at high spatial and temporal resolution
Rift migration and localization of deformation are significant within the Corinth Rift
Changes in rift geometry and linkage of major rift faults occur at rapid 100 kyr timescales</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/2015TC004026</doi><tpages>24</tpages><orcidid>https://orcid.org/0000-0003-3732-1900</orcidid><orcidid>https://orcid.org/0000-0002-4151-7909</orcidid><orcidid>https://orcid.org/0000-0002-3012-6865</orcidid><oa>free_for_read</oa></addata></record> |
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| issn | 0278-7407 1944-9194 |
| language | eng |
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| source | Wiley Free Content; Wiley-Blackwell AGU Digital Library; Wiley Online Library Journals Frontfile Complete; EZB-FREE-00999 freely available EZB journals |
| subjects | border faults Corinth Rift Deformation Earth Sciences fault linkage Plate tectonics rift evolution rift symmetry Sciences of the Universe sedimentary basins Seismology Tectonics |
| title | Rapid spatiotemporal variations in rift structure during development of the Corinth Rift, central Greece |
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