FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4288045951> ?p ?o ?g. }

• W4288045951 endingPage "229504" @default.
• W4288045951 startingPage "229504" @default.
• W4288045951 abstract "The Aquitaine Basin is closely linked to the evolution of the Pyrenees, providing precious evidence of the early stages of the Pyrenean orogeny in the Late Cretaceous. Although the timing and geometry of the Early Cretaceous rifting stage is well constrained in the Pyrenees and surrounding north Pyrenean basins, the subsequent early inversion stage has resisted characterization. In this study, we used well log correlations and interpretation of seismic reflection profiles to determine the Late Cretaceous evolution of the sedimentary record in the Aquitaine Basin, spanning the transition from the postrift stage to the beginning of convergence. We identified two main deformation stages during the Late Cretaceous with radically different basin geometries in the western and eastern portions of the Aquitaine Basin. The western part appears to remain under a thermal subsidence regime, inherited from the postrift stage initiated in the Turonian, with little to no deformation. In contrast, the eastern part records early inversion, as indicated by the presence of a well-defined Campanian flexural basin. Between them, Coniacian and Santonian strata indicate a sharply increasing distinction between a very slowly subsiding North Aquitaine Domain (condensed sedimentation) and a strongly subsiding South Aquitaine Domain. We interpret this development as a consequence of lithospheric buckling resulting from far-field compressive strain between the Eurasia and Africa plates. During the Campanian, northward convergence of the Iberia plate led to the formation of a flexural basin with a narrower, steeper geometry than the subsequent Eocene basin that formed in nearly the same region during the Pyrenean orogeny. We attribute this difference to the development of the foreland over a lithosphere that was not thermally reequilibrated in Campanian time, roughly 10 Myr after rifting. This thermal inheritance resulted in lithosphere of very low rigidity. Sedimentary basins formed during both the Coniacian-Santonian and Campanian to early Maastrichtian were thus accommodated by short-wavelength flexural deformation of the lithosphere, a distinctive deformation pattern that represents an immediate response to the onset of compressive strain." @default.
• W4288045951 created "2022-07-27" @default.
• W4288045951 creator A5010597798 @default.
• W4288045951 creator A5024380685 @default.
• W4288045951 creator A5040708533 @default.
• W4288045951 creator A5071411964 @default.
• W4288045951 creator A5071541848 @default.
• W4288045951 creator A5087267351 @default.
• W4288045951 date "2022-11-01" @default.
• W4288045951 modified "2023-09-30" @default.
• W4288045951 title "Onset of Iberian-European plate convergence: Late Cretaceous flexural response of a hot lithosphere (Aquitaine Basin, France)" @default.
• W4288045951 cites W1498314499 @default.
• W4288045951 cites W1529788327 @default.
• W4288045951 cites W1728915053 @default.
• W4288045951 cites W1962433520 @default.
• W4288045951 cites W1963646778 @default.
• W4288045951 cites W1963861322 @default.
• W4288045951 cites W1965301027 @default.
• W4288045951 cites W1966396339 @default.
• W4288045951 cites W1970075937 @default.
• W4288045951 cites W1970776112 @default.
• W4288045951 cites W1972749367 @default.
• W4288045951 cites W1974791060 @default.
• W4288045951 cites W1975017135 @default.
• W4288045951 cites W1980642926 @default.
• W4288045951 cites W1984633020 @default.
• W4288045951 cites W1985685882 @default.
• W4288045951 cites W1987085354 @default.
• W4288045951 cites W1988657625 @default.
• W4288045951 cites W1993124638 @default.
• W4288045951 cites W1994368522 @default.
• W4288045951 cites W1994705238 @default.
• W4288045951 cites W1999592091 @default.
• W4288045951 cites W2000176625 @default.
• W4288045951 cites W2001788443 @default.
• W4288045951 cites W2005492924 @default.
• W4288045951 cites W2005637388 @default.
• W4288045951 cites W2006505221 @default.
• W4288045951 cites W2010497203 @default.
• W4288045951 cites W2010553431 @default.
• W4288045951 cites W2020301204 @default.
• W4288045951 cites W2022774377 @default.
• W4288045951 cites W2023504158 @default.
• W4288045951 cites W2027433504 @default.
• W4288045951 cites W2032648806 @default.
• W4288045951 cites W2032964793 @default.
• W4288045951 cites W2034104738 @default.
• W4288045951 cites W2043987660 @default.
• W4288045951 cites W2044249302 @default.
• W4288045951 cites W2044645010 @default.
• W4288045951 cites W2050440902 @default.
• W4288045951 cites W2052346014 @default.
• W4288045951 cites W2058876407 @default.
• W4288045951 cites W2061680126 @default.
• W4288045951 cites W2064065757 @default.
• W4288045951 cites W2064663944 @default.
• W4288045951 cites W2068892745 @default.
• W4288045951 cites W2069420671 @default.
• W4288045951 cites W2069998611 @default.
• W4288045951 cites W2072901235 @default.
• W4288045951 cites W2081617724 @default.
• W4288045951 cites W2092351828 @default.
• W4288045951 cites W2092832226 @default.
• W4288045951 cites W2093980733 @default.
• W4288045951 cites W2098087841 @default.
• W4288045951 cites W2100982634 @default.
• W4288045951 cites W2108610660 @default.
• W4288045951 cites W2113342113 @default.
• W4288045951 cites W2118736400 @default.
• W4288045951 cites W2118755672 @default.
• W4288045951 cites W2133614071 @default.
• W4288045951 cites W2146093540 @default.
• W4288045951 cites W2153985161 @default.
• W4288045951 cites W2157561902 @default.
• W4288045951 cites W2158078060 @default.
• W4288045951 cites W2161761265 @default.
• W4288045951 cites W2163161113 @default.
• W4288045951 cites W2167149240 @default.
• W4288045951 cites W2191470229 @default.
• W4288045951 cites W2208973677 @default.
• W4288045951 cites W2259148476 @default.
• W4288045951 cites W2270060953 @default.
• W4288045951 cites W2297221439 @default.
• W4288045951 cites W2312328317 @default.
• W4288045951 cites W2316455897 @default.
• W4288045951 cites W2316940040 @default.
• W4288045951 cites W2319228517 @default.
• W4288045951 cites W2329647001 @default.
• W4288045951 cites W2331430649 @default.
• W4288045951 cites W2340885470 @default.
• W4288045951 cites W2413867050 @default.
• W4288045951 cites W2494058218 @default.
• W4288045951 cites W2550502871 @default.
• W4288045951 cites W2581782420 @default.
• W4288045951 cites W2593831333 @default.
• W4288045951 cites W2608275755 @default.
• W4288045951 cites W2730260610 @default.
• W4288045951 cites W2735193348 @default.

• next