FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2096967048> ?p ?o ?g. }

• W2096967048 endingPage "519" @default.
• W2096967048 startingPage "501" @default.
• W2096967048 abstract "Rifting between Arabia and Somalia started around 35 Ma followed by spreading at 17.6 Ma in the eastern part of the Gulf of Aden. The first-order segment between Alula-Fartak and Socotra-Hadbeen fracture zones is divided into three second-order segments with different structure and morphology. Seismic reflection data were collected during the Encens Cruise in 2006 on the northeastern margin. In this study, we present the results of Pre-Stack Depth Migration of the multichannel seismic data from the western segment, which allows us to propose a tectono-stratigraphic model of the evolution of this segment of the margin from rifting to the present day. The chronological interpretation of the sedimentary sequences is mapped out within relation to the onshore observations and existing dating. After a major development of syn-rift grabens and horsts, the deformation localized where the crust is the thinnest. This deformation occurred in the distal margin graben (DIM) at the northern boundary of the ocean–continent transition (OCT) represented by the OCT ridge. At the onset of the OCT formation differential uplift induced a submarine landslide on top of the deepest tilted block and the crustal deformation was restricted to the southern part of the DIM graben, where the continental break-up finally occurred. Initial seafloor spreading was followed by post-rift magmatic events (flows, sills and volcano-sedimentary wedge), whose timing is constrained by the analysis of the sedimentary cover of the OCT ridge, correlated with onshore stratigraphy. The OCT ridge may represent exhumed serpentinized mantle intruded by post-rift magmatic material, which modified the OCT after its emplacement." @default.
• W2096967048 created "2016-06-24" @default.
• W2096967048 creator A5003914466 @default.
• W2096967048 creator A5010844378 @default.
• W2096967048 creator A5015713527 @default.
• W2096967048 creator A5026325986 @default.
• W2096967048 creator A5034718981 @default.
• W2096967048 creator A5040684590 @default.
• W2096967048 creator A5063486929 @default.
• W2096967048 creator A5072904044 @default.
• W2096967048 creator A5087185234 @default.
• W2096967048 date "2010-02-01" @default.
• W2096967048 modified "2023-10-13" @default.
• W2096967048 title "Continental break-up history of a deep magma-poor margin based on seismic reflection data (northeastern Gulf of Aden margin, offshore Oman)" @default.
• W2096967048 cites W1579118674 @default.
• W2096967048 cites W1586873887 @default.
• W2096967048 cites W1597948644 @default.
• W2096967048 cites W1629102058 @default.
• W2096967048 cites W1660410253 @default.
• W2096967048 cites W1860912165 @default.
• W2096967048 cites W1963730357 @default.
• W2096967048 cites W1964421696 @default.
• W2096967048 cites W1966938295 @default.
• W2096967048 cites W1968534064 @default.
• W2096967048 cites W1969091811 @default.
• W2096967048 cites W1974850963 @default.
• W2096967048 cites W1975437244 @default.
• W2096967048 cites W1976870535 @default.
• W2096967048 cites W197699760 @default.
• W2096967048 cites W1981545340 @default.
• W2096967048 cites W1984028684 @default.
• W2096967048 cites W1987451771 @default.
• W2096967048 cites W1990127138 @default.
• W2096967048 cites W1993176067 @default.
• W2096967048 cites W1998523277 @default.
• W2096967048 cites W2000936634 @default.
• W2096967048 cites W2003207592 @default.
• W2096967048 cites W2006334200 @default.
• W2096967048 cites W2006957727 @default.
• W2096967048 cites W2009311382 @default.
• W2096967048 cites W2010391154 @default.
• W2096967048 cites W2015356066 @default.
• W2096967048 cites W2029810342 @default.
• W2096967048 cites W2030865624 @default.
• W2096967048 cites W2031690282 @default.
• W2096967048 cites W2034753142 @default.
• W2096967048 cites W2039554481 @default.
• W2096967048 cites W2040150643 @default.
• W2096967048 cites W2040686738 @default.
• W2096967048 cites W2049412643 @default.
• W2096967048 cites W2049885524 @default.
• W2096967048 cites W2055127223 @default.
• W2096967048 cites W2057186874 @default.
• W2096967048 cites W2057371440 @default.
• W2096967048 cites W2057698253 @default.
• W2096967048 cites W2074344573 @default.
• W2096967048 cites W2076588934 @default.
• W2096967048 cites W2077308142 @default.
• W2096967048 cites W2079423425 @default.
• W2096967048 cites W2089857088 @default.
• W2096967048 cites W2099395631 @default.
• W2096967048 cites W2102271623 @default.
• W2096967048 cites W2114562000 @default.
• W2096967048 cites W2114660893 @default.
• W2096967048 cites W2123170786 @default.
• W2096967048 cites W2124474119 @default.
• W2096967048 cites W2126669455 @default.
• W2096967048 cites W2127878314 @default.
• W2096967048 cites W2129225601 @default.
• W2096967048 cites W2135406745 @default.
• W2096967048 cites W2139226830 @default.
• W2096967048 cites W2146622027 @default.
• W2096967048 cites W2147994093 @default.
• W2096967048 cites W2148041619 @default.
• W2096967048 cites W2155339969 @default.
• W2096967048 cites W2159877291 @default.
• W2096967048 cites W2161724769 @default.
• W2096967048 cites W2163722736 @default.
• W2096967048 cites W2169567100 @default.
• W2096967048 cites W2241185619 @default.
• W2096967048 cites W2329283479 @default.
• W2096967048 cites W2436318394 @default.
• W2096967048 cites W2735774697 @default.
• W2096967048 cites W4252226173 @default.
• W2096967048 cites W4376099761 @default.
• W2096967048 cites W4376453751 @default.
• W2096967048 cites W56821118 @default.
• W2096967048 cites W2717917087 @default.
• W2096967048 doi "https://doi.org/10.1111/j.1365-246x.2009.04424.x" @default.
• W2096967048 hasPublicationYear "2010" @default.
• W2096967048 type Work @default.
• W2096967048 sameAs 2096967048 @default.
• W2096967048 citedByCount "83" @default.
• W2096967048 countsByYear W20969670482012 @default.
• W2096967048 countsByYear W20969670482013 @default.
• W2096967048 countsByYear W20969670482014 @default.
• W2096967048 countsByYear W20969670482015 @default.
• W2096967048 countsByYear W20969670482016 @default.

• next