FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4317726608> ?p ?o ?g. }

• W4317726608 endingPage "229728" @default.
• W4317726608 startingPage "229728" @default.
• W4317726608 abstract "The diversity and complexity of existing models on the structure of the Red Sea is the result of a mobile sedimentary cover that not only hides most of the basement and oceanic structures but also hamper the geophysical signals. In this study, we combined published with new unpublished geophysical data to propose a revised interpretation of the structure of the lithosphere between the Hanish Islands (ca. 13.5°N) and the Dead Sea Fracture Zone (ca. 27.5°N). The recognition of allochthonous salt and overburden allows to propose a structural model with simple geometries that are consistent with the present-day kinematic constraints (GPS velocities and Euler Poles) and with the rules of plate's motion on a sphere (Euler Theorem). We mapped a continuous Mid Ocean Ridge segment parallel to the main rift orientation in the southern Red Sea that becomes highly discontinuous and more oblique towards the north as it gets closer to the Euler Pole. These segments all point towards the Euler pole and are consistently offset to the right by transform faults in the central and northern Red Sea cumulating an offset of 400 km. The transform faults are accommodating seafloor spreading in the Red Sea and cluster in three main fracture zones: (1) the Ikwan Fracture Zone near the Ikwan (or Brother) Islands, (2) the Zabargad Fracture Zone in the vicinity of the Zabargad Island and (3) the Jeddah Fracture Zone offshore the Jeddah/Port Sudan area (central Red Sea). Based on a new seismic reflection dataset and published data we propose an interpretation of the Ocean Continent Transition (OCT) in the Red Sea. We bring new evidence (magnetic lineaments, distance of the OCT to the ridge, basin stratigraphy) to support a Middle Miocene (ca. 14 Ma) age for the initiation of seafloor spreading throughout the Red Sea, and we discuss this event with the initiation of strike-slip motion in the Aqaba-Dead Sea transform zone. Finally, compiling all available data and literature, we propose a regionally coherent geodynamic reconstruction using two different poles of rotation for the rifting and seafloor spreading phases." @default.
• W4317726608 created "2023-01-23" @default.
• W4317726608 creator A5053826418 @default.
• W4317726608 creator A5054072678 @default.
• W4317726608 creator A5060797133 @default.
• W4317726608 creator A5074794653 @default.
• W4317726608 creator A5079151229 @default.
• W4317726608 creator A5081512089 @default.
• W4317726608 date "2023-02-01" @default.
• W4317726608 modified "2023-10-05" @default.
• W4317726608 title "Structure and morphology of the Red Sea, from the mid-ocean ridge to the ocean-continent boundary" @default.
• W4317726608 cites W1519872695 @default.
• W4317726608 cites W1531273367 @default.
• W4317726608 cites W1577670450 @default.
• W4317726608 cites W1588980084 @default.
• W4317726608 cites W1660410253 @default.
• W4317726608 cites W1763460218 @default.
• W4317726608 cites W1968534064 @default.
• W4317726608 cites W1973242220 @default.
• W4317726608 cites W1978632315 @default.
• W4317726608 cites W1980703311 @default.
• W4317726608 cites W1983447647 @default.
• W4317726608 cites W1986824716 @default.
• W4317726608 cites W1992477749 @default.
• W4317726608 cites W1996399287 @default.
• W4317726608 cites W1997739005 @default.
• W4317726608 cites W2001636832 @default.
• W4317726608 cites W2003089534 @default.
• W4317726608 cites W2010749247 @default.
• W4317726608 cites W2012530126 @default.
• W4317726608 cites W2014144720 @default.
• W4317726608 cites W2022648729 @default.
• W4317726608 cites W2028672304 @default.
• W4317726608 cites W2030629162 @default.
• W4317726608 cites W2047018904 @default.
• W4317726608 cites W2053148752 @default.
• W4317726608 cites W2054927110 @default.
• W4317726608 cites W2057854684 @default.
• W4317726608 cites W2061255597 @default.
• W4317726608 cites W2063992088 @default.
• W4317726608 cites W2066447471 @default.
• W4317726608 cites W2077455611 @default.
• W4317726608 cites W2079035957 @default.
• W4317726608 cites W2087564946 @default.
• W4317726608 cites W2102234201 @default.
• W4317726608 cites W2111211903 @default.
• W4317726608 cites W2117737667 @default.
• W4317726608 cites W2119344498 @default.
• W4317726608 cites W2120909089 @default.
• W4317726608 cites W2121889129 @default.
• W4317726608 cites W2121915027 @default.
• W4317726608 cites W2122155423 @default.
• W4317726608 cites W2135715440 @default.
• W4317726608 cites W2136415225 @default.
• W4317726608 cites W2138058376 @default.
• W4317726608 cites W2139226830 @default.
• W4317726608 cites W2148123201 @default.
• W4317726608 cites W2148175431 @default.
• W4317726608 cites W2148917200 @default.
• W4317726608 cites W2148982479 @default.
• W4317726608 cites W2149576899 @default.
• W4317726608 cites W2165338724 @default.
• W4317726608 cites W2172894972 @default.
• W4317726608 cites W2202216454 @default.
• W4317726608 cites W2217301490 @default.
• W4317726608 cites W2494150380 @default.
• W4317726608 cites W2498047478 @default.
• W4317726608 cites W2605707177 @default.
• W4317726608 cites W2767174830 @default.
• W4317726608 cites W2809026107 @default.
• W4317726608 cites W2897031043 @default.
• W4317726608 cites W2932696668 @default.
• W4317726608 cites W3011934701 @default.
• W4317726608 cites W306621583 @default.
• W4317726608 cites W3088942682 @default.
• W4317726608 cites W3100284926 @default.
• W4317726608 cites W3155951627 @default.
• W4317726608 cites W3183976647 @default.
• W4317726608 cites W4206163256 @default.
• W4317726608 cites W4214719836 @default.
• W4317726608 cites W4223468137 @default.
• W4317726608 cites W4234476530 @default.
• W4317726608 cites W4246146226 @default.
• W4317726608 cites W4367435833 @default.
• W4317726608 cites W602532165 @default.
• W4317726608 doi "https://doi.org/10.1016/j.tecto.2023.229728" @default.
• W4317726608 hasPublicationYear "2023" @default.
• W4317726608 type Work @default.
• W4317726608 citedByCount "3" @default.
• W4317726608 countsByYear W43177266082023 @default.
• W4317726608 crossrefType "journal-article" @default.
• W4317726608 hasAuthorship W4317726608A5053826418 @default.
• W4317726608 hasAuthorship W4317726608A5054072678 @default.
• W4317726608 hasAuthorship W4317726608A5060797133 @default.
• W4317726608 hasAuthorship W4317726608A5074794653 @default.
• W4317726608 hasAuthorship W4317726608A5079151229 @default.
• W4317726608 hasAuthorship W4317726608A5081512089 @default.
• W4317726608 hasBestOaLocation W43177266081 @default.

• next