FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3166804729> ?p ?o ?g. }

• W3166804729 abstract "&lt;p&gt;Transform continental margins known across the Earth represent 31% of passive margins. Resulting from first-order plate tectonic processes, transform margins record a diachronous evolution mainly defined by three successive stages, including intra-continental transform faulting, active and passive transform margin. Due to their high complexity and a lack of large hydrocarbon discoveries (i.e. not a target for oil industry), they have only been sparsely studied, especially when compared with other margin types (i.e. divergent or convergent).&lt;/p&gt;&lt;p&gt;&amp;#160;&amp;#160;&amp;#160;&amp;#160;&amp;#160;&amp;#160;&amp;#160;&amp;#160;&amp;#160;&amp;#160;&amp;#160;&amp;#160;&amp;#160;&amp;#160;&amp;#160;&amp;#160;&amp;#160; We present the structure and evolution of the NS-trending Limpopo Transform Fault Zone (LTFZ), corresponding to the main fracture zone from western part of the Africa-Antarctica Corridor (AAC). Here, we combine published and unpublished dataset (seismic reflection profiles, wells, multibeam bathymetry, gravity, magnetic data) in order to propose an interpretation of the LTFZ structure and adjoining segments and their evolution through time, from rifting to spreading.&lt;/p&gt;&lt;p&gt;The LTFZ is composed of two main segments: the East Limpopo segment and the Astrid conjugate one and the North and South Natal segment including the Dana-Galathea Plateau (Mozambique side) and the Maud rise/east of Grunehogna craton (Antarctica margin). The LTFZ offsets the segments of divergent conjugate margins (Southern Natal-off Grunehogna craton in the west and Beira High Angoche-Riiser Larsen Sea in the east) since&amp;#160;155 Ma (chron M25). We focus on the evolution of the transform fault zone from its initiation at chron M25 up to chron M0 (~126 Ma, Barremian). Oceanic spreading onset at chron M25 in the south of Beira High segment and Dana-Galathea Plateau triggered the uplift and erosion of the proximal parts of the margin and the formation of several seaward dipping reflectors wedges. Plate kinematic implies an NNW-SSE opening of the LTFZ. The oblique component of opening promotes the setting up of several volcanic wedges. These wedges rejuvenate southward trough time, which is consistent with the sliding of Antarctica with respect to Africa and thus confirm the diachronous evolution of the transform fault zone.&lt;/p&gt;" @default.
• W3166804729 created "2021-06-22" @default.
• W3166804729 creator A5001446945 @default.
• W3166804729 creator A5006281942 @default.
• W3166804729 creator A5012480923 @default.
• W3166804729 creator A5028328122 @default.
• W3166804729 creator A5044946648 @default.
• W3166804729 creator A5049799328 @default.
• W3166804729 creator A5072904044 @default.
• W3166804729 creator A5076445271 @default.
• W3166804729 creator A5087185234 @default.
• W3166804729 date "2020-03-23" @default.
• W3166804729 modified "2023-09-26" @default.
• W3166804729 title "Magma-rich transform margins: example from the Limpopo transform fault zone between Mozambique and Antarctica" @default.
• W3166804729 doi "https://doi.org/10.5194/egusphere-egu2020-10508" @default.
• W3166804729 hasPublicationYear "2020" @default.
• W3166804729 type Work @default.
• W3166804729 sameAs 3166804729 @default.
• W3166804729 citedByCount "1" @default.
• W3166804729 countsByYear W31668047292021 @default.
• W3166804729 crossrefType "posted-content" @default.
• W3166804729 hasAuthorship W3166804729A5001446945 @default.
• W3166804729 hasAuthorship W3166804729A5006281942 @default.
• W3166804729 hasAuthorship W3166804729A5012480923 @default.
• W3166804729 hasAuthorship W3166804729A5028328122 @default.
• W3166804729 hasAuthorship W3166804729A5044946648 @default.
• W3166804729 hasAuthorship W3166804729A5049799328 @default.
• W3166804729 hasAuthorship W3166804729A5072904044 @default.
• W3166804729 hasAuthorship W3166804729A5076445271 @default.
• W3166804729 hasAuthorship W3166804729A5087185234 @default.
• W3166804729 hasConcept C106973953 @default.
• W3166804729 hasConcept C127313418 @default.
• W3166804729 hasConcept C165205528 @default.
• W3166804729 hasConcept C175551986 @default.
• W3166804729 hasConcept C180526460 @default.
• W3166804729 hasConcept C181199279 @default.
• W3166804729 hasConcept C185592680 @default.
• W3166804729 hasConcept C55493867 @default.
• W3166804729 hasConceptScore W3166804729C106973953 @default.
• W3166804729 hasConceptScore W3166804729C127313418 @default.
• W3166804729 hasConceptScore W3166804729C165205528 @default.
• W3166804729 hasConceptScore W3166804729C175551986 @default.
• W3166804729 hasConceptScore W3166804729C180526460 @default.
• W3166804729 hasConceptScore W3166804729C181199279 @default.
• W3166804729 hasConceptScore W3166804729C185592680 @default.
• W3166804729 hasConceptScore W3166804729C55493867 @default.
• W3166804729 hasLocation W31668047291 @default.
• W3166804729 hasOpenAccess W3166804729 @default.
• W3166804729 hasPrimaryLocation W31668047291 @default.
• W3166804729 hasRelatedWork W45518673 @default.
• W3166804729 hasRelatedWork W51105697 @default.
• W3166804729 hasRelatedWork W53610893 @default.
• W3166804729 hasRelatedWork W60349875 @default.
• W3166804729 hasRelatedWork W63702898 @default.
• W3166804729 hasRelatedWork W69209786 @default.
• W3166804729 hasRelatedWork W76669141 @default.
• W3166804729 hasRelatedWork W90533467 @default.
• W3166804729 hasRelatedWork W90657174 @default.
• W3166804729 hasRelatedWork W94736417 @default.
• W3166804729 isParatext "false" @default.
• W3166804729 isRetracted "false" @default.
• W3166804729 magId "3166804729" @default.
• W3166804729 workType "article" @default.