FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2896986104> ?p ?o ?g. }

• W2896986104 endingPage "250" @default.
• W2896986104 startingPage "225" @default.
• W2896986104 abstract "Abstract. Not all continental rifts mature to form a young ocean. The mechanism and duration of their cessation depend on the crustal structure, modifications in plate kinematics, lithospheric thermal response, or the intensity of subcrustal flow (e.g., plume activity). The cessation is recorded in the structure and stratigraphy of the basins that develop during the rifting process. This architecture is lost due to younger tectonic inversion, severe erosion, or even burial into greater depths that forces their detection by low-resolution geophysical imaging. The current study focuses on a uniquely preserved Oligo-Miocene rift that was subsequently taken over by a crossing transform fault system and, mostly due to that, died out. We integrate all geological, geophysical, and previous study results from across the southern Galilee to unravel the structural development of the Irbid failing rift in northwest Arabia. Despite tectonic, magmatic, and geomorphologic activity postdating the rifting, its subsurface structure northwest of the Dead Sea fault is preserved at depths of up to 1 km. Our results show that a series of basins subsided at the rift front, i.e., rift termination, across the southern Galilee. We constrain the timing and extent of their subsidence into two main stages based on facies analysis and chronology of magmatism. Between 20 and 9 Ma grabens and half-grabens subsided within a larger releasing jog, following a NW direction of a deeper presumed principal displacement zone. The basins continued to subside until a transition from the transtensional Red Sea to the transpressional Dead Sea stress regime occurred. With the transition, the basins ceased to subside as a rift, while the Dead Sea fault split the jog structure. Between 9 and 5 Ma basin subsidence accentuated and an uplift of their margins accompanied their overall elongation to the NNE. Our study provides for the first time a structural as well as tectonic context for the southern Galilee basins. Based on this case study we suggest that the rift did not fail but rather faded and was taken over by a more dominant stress regime. Otherwise, these basins of a failing rift could have simply died out peacefully." @default.
• W2896986104 created "2018-10-26" @default.
• W2896986104 creator A5027445351 @default.
• W2896986104 creator A5040832365 @default.
• W2896986104 creator A5071386500 @default.
• W2896986104 creator A5072750546 @default.
• W2896986104 date "2019-01-31" @default.
• W2896986104 modified "2023-10-16" @default.
• W2896986104 title "Structural expression of a fading rift front: a case study from the Oligo-Miocene Irbid rift of northwest Arabia" @default.
• W2896986104 cites W1482015549 @default.
• W2896986104 cites W1503493870 @default.
• W2896986104 cites W1523108743 @default.
• W2896986104 cites W1570308262 @default.
• W2896986104 cites W1576516474 @default.
• W2896986104 cites W1587390255 @default.
• W2896986104 cites W1587864144 @default.
• W2896986104 cites W1591302912 @default.
• W2896986104 cites W1647500574 @default.
• W2896986104 cites W1660410253 @default.
• W2896986104 cites W181273480 @default.
• W2896986104 cites W1957654099 @default.
• W2896986104 cites W1972724602 @default.
• W2896986104 cites W1979407478 @default.
• W2896986104 cites W1980966991 @default.
• W2896986104 cites W1982621864 @default.
• W2896986104 cites W1982738320 @default.
• W2896986104 cites W1983235437 @default.
• W2896986104 cites W1983393426 @default.
• W2896986104 cites W1983940963 @default.
• W2896986104 cites W1985954666 @default.
• W2896986104 cites W1989877611 @default.
• W2896986104 cites W1993520177 @default.
• W2896986104 cites W1995026670 @default.
• W2896986104 cites W1996835608 @default.
• W2896986104 cites W1996911591 @default.
• W2896986104 cites W1997235146 @default.
• W2896986104 cites W1997252211 @default.
• W2896986104 cites W1997812068 @default.
• W2896986104 cites W1998992890 @default.
• W2896986104 cites W1999278873 @default.
• W2896986104 cites W2001550271 @default.
• W2896986104 cites W2005986282 @default.
• W2896986104 cites W2006004526 @default.
• W2896986104 cites W2006254584 @default.
• W2896986104 cites W2006605170 @default.
• W2896986104 cites W2007074497 @default.
• W2896986104 cites W2009931505 @default.
• W2896986104 cites W2016219895 @default.
• W2896986104 cites W2016496402 @default.
• W2896986104 cites W2018614582 @default.
• W2896986104 cites W2019967542 @default.
• W2896986104 cites W2020093204 @default.
• W2896986104 cites W2022061975 @default.
• W2896986104 cites W2024790553 @default.
• W2896986104 cites W2026932112 @default.
• W2896986104 cites W2027028384 @default.
• W2896986104 cites W2029292238 @default.
• W2896986104 cites W2029769457 @default.
• W2896986104 cites W2032490257 @default.
• W2896986104 cites W2033950135 @default.
• W2896986104 cites W2034896492 @default.
• W2896986104 cites W2036605596 @default.
• W2896986104 cites W2038746064 @default.
• W2896986104 cites W2038827426 @default.
• W2896986104 cites W2039438134 @default.
• W2896986104 cites W2044649453 @default.
• W2896986104 cites W2046149738 @default.
• W2896986104 cites W2046593869 @default.
• W2896986104 cites W2049863680 @default.
• W2896986104 cites W2054461170 @default.
• W2896986104 cites W2056955907 @default.
• W2896986104 cites W2057180761 @default.
• W2896986104 cites W2059889715 @default.
• W2896986104 cites W2060472169 @default.
• W2896986104 cites W2060606614 @default.
• W2896986104 cites W2061448960 @default.
• W2896986104 cites W2062985107 @default.
• W2896986104 cites W2063060675 @default.
• W2896986104 cites W2064317759 @default.
• W2896986104 cites W2064936022 @default.
• W2896986104 cites W2064970633 @default.
• W2896986104 cites W2067117119 @default.
• W2896986104 cites W2069302116 @default.
• W2896986104 cites W2070791820 @default.
• W2896986104 cites W2075747016 @default.
• W2896986104 cites W2076062891 @default.
• W2896986104 cites W2077952475 @default.
• W2896986104 cites W2078007617 @default.
• W2896986104 cites W2081147242 @default.
• W2896986104 cites W2084535484 @default.
• W2896986104 cites W2086618421 @default.
• W2896986104 cites W2087370836 @default.
• W2896986104 cites W2088330959 @default.
• W2896986104 cites W2089808263 @default.
• W2896986104 cites W2103965202 @default.
• W2896986104 cites W2104455234 @default.
• W2896986104 cites W2107858435 @default.
• W2896986104 cites W2108029693 @default.

• next