FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3208378234> ?p ?o ?g. }

• W3208378234 endingPage "488" @default.
• W3208378234 startingPage "457" @default.
• W3208378234 abstract "Abstract The tectono‐stratigraphic evolution of rift systems is at present poorly understood, especially the one preceding the onset of oceanic seafloor spreading. Improving our understanding of the complex, polyphase tectonic evolution of the fossil Alpine Tethys, one of the best calibrated magma‐poor rift systems worldwide, offers great potential for the interpretation of the distal part of global rifted margins, which notoriously lack data. In this paper, we propose a tectono‐stratigraphic model for the former Alpine Tethys, whose remnants are exposed in the Alps of Western Europe. We first review the historical evolution of some concepts grounding present knowledge on the Alpine‐ and global magma‐poor rifted margins. Then we present a spatial and temporal template for the Alpine Tethys rift system using a ‘building block (BB)’ approach. This new approach is powerful in that it can integrate high‐resolution, structural, stratigraphic, thermochronological, and petrological observations from dismembered outcrops into a margin‐scale template compatible with the first‐order seismic architecture defined at present‐day, magma‐poor rifted margins. The detailed analysis of the syn‐rift sequence of the Alpine Tethys margins demonstrates that extension migrated and localised while evolving from the stretching to the necking phase. During hyperextension, rifting was asymmetric and controlled by in‐sequence detachment faulting. Then, the rift system evolved back into a more symmetric, embryonic spreading system. With this contribution, we aim to allow readers without knowledge of the Alps to access this unique ‘archive’ preserving some of the world's best‐exposed rift structures. Recognising these structures is critical to understand the origin of some new concepts used to explain present‐day, deep‐water rifted margins, and to interpret and predict the tectono‐stratigraphic evolution during advanced stages of rifting." @default.
• W3208378234 created "2021-11-08" @default.
• W3208378234 creator A5011630548 @default.
• W3208378234 creator A5019716051 @default.
• W3208378234 creator A5042923352 @default.
• W3208378234 creator A5058228162 @default.
• W3208378234 creator A5072945243 @default.
• W3208378234 date "2021-11-11" @default.
• W3208378234 modified "2023-10-16" @default.
• W3208378234 title "The syn‐rift tectono‐stratigraphic record of rifted margins (Part I): Insights from the Alpine Tethys" @default.
• W3208378234 cites W1095956616 @default.
• W3208378234 cites W1493706511 @default.
• W3208378234 cites W1499351358 @default.
• W3208378234 cites W1505812976 @default.
• W3208378234 cites W1548147260 @default.
• W3208378234 cites W1567244269 @default.
• W3208378234 cites W1586873887 @default.
• W3208378234 cites W1687675348 @default.
• W3208378234 cites W1748545007 @default.
• W3208378234 cites W1769604092 @default.
• W3208378234 cites W1830716544 @default.
• W3208378234 cites W1968534064 @default.
• W3208378234 cites W1972906038 @default.
• W3208378234 cites W1975400835 @default.
• W3208378234 cites W1977875962 @default.
• W3208378234 cites W1980216110 @default.
• W3208378234 cites W1981456162 @default.
• W3208378234 cites W1983186065 @default.
• W3208378234 cites W2002267842 @default.
• W3208378234 cites W2006505221 @default.
• W3208378234 cites W2008877113 @default.
• W3208378234 cites W2015174616 @default.
• W3208378234 cites W2025364748 @default.
• W3208378234 cites W2025371343 @default.
• W3208378234 cites W2027371760 @default.
• W3208378234 cites W2027620484 @default.
• W3208378234 cites W2034753142 @default.
• W3208378234 cites W2042229840 @default.
• W3208378234 cites W2042806383 @default.
• W3208378234 cites W2044732818 @default.
• W3208378234 cites W2061235729 @default.
• W3208378234 cites W2070544161 @default.
• W3208378234 cites W2072877917 @default.
• W3208378234 cites W2076035287 @default.
• W3208378234 cites W2077327086 @default.
• W3208378234 cites W2081501537 @default.
• W3208378234 cites W2082254430 @default.
• W3208378234 cites W2083772074 @default.
• W3208378234 cites W2087564946 @default.
• W3208378234 cites W2110416209 @default.
• W3208378234 cites W2111611821 @default.
• W3208378234 cites W2118755672 @default.
• W3208378234 cites W2122322725 @default.
• W3208378234 cites W2125923958 @default.
• W3208378234 cites W2135032781 @default.
• W3208378234 cites W2138961527 @default.
• W3208378234 cites W2145501948 @default.
• W3208378234 cites W2145511995 @default.
• W3208378234 cites W2146090986 @default.
• W3208378234 cites W2154134823 @default.
• W3208378234 cites W2157861971 @default.
• W3208378234 cites W2159873629 @default.
• W3208378234 cites W2166218667 @default.
• W3208378234 cites W2297778366 @default.
• W3208378234 cites W2320397404 @default.
• W3208378234 cites W2320819202 @default.
• W3208378234 cites W2332718182 @default.
• W3208378234 cites W2469625643 @default.
• W3208378234 cites W2525934248 @default.
• W3208378234 cites W2529247676 @default.
• W3208378234 cites W2560799619 @default.
• W3208378234 cites W2566439189 @default.
• W3208378234 cites W2580947892 @default.
• W3208378234 cites W2764268081 @default.
• W3208378234 cites W2773812625 @default.
• W3208378234 cites W2794214214 @default.
• W3208378234 cites W2804067255 @default.
• W3208378234 cites W2896946579 @default.
• W3208378234 cites W2902825355 @default.
• W3208378234 cites W2907576927 @default.
• W3208378234 cites W2910044667 @default.
• W3208378234 cites W2913178758 @default.
• W3208378234 cites W2916097877 @default.
• W3208378234 cites W2943835756 @default.
• W3208378234 cites W2947176648 @default.
• W3208378234 cites W2947463065 @default.
• W3208378234 cites W2964514590 @default.
• W3208378234 cites W2968975895 @default.
• W3208378234 cites W2971609132 @default.
• W3208378234 cites W2972312462 @default.
• W3208378234 cites W2983318658 @default.
• W3208378234 cites W2986058699 @default.
• W3208378234 cites W3023581952 @default.
• W3208378234 cites W3024631459 @default.
• W3208378234 cites W3034895979 @default.
• W3208378234 cites W3044026987 @default.
• W3208378234 cites W3092367161 @default.
• W3208378234 cites W3092966554 @default.

• next