FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3086570414> ?p ?o ?g. }

• W3086570414 endingPage "103321" @default.
• W3086570414 startingPage "103321" @default.
• W3086570414 abstract "Gravelly tsunami event beds are well known from some contemporary shores, but they are far less known from the pre-Quaternary depositional record. Lacustrine examples are particularly exceptional. Here we present multidisciplinary evidence for a lacustrine cobble to boulder gravel deposited as an onshore paleo-tsunamiite and discuss features that help to identify the depositional setting. The deposit was formed on the rocky shore of a large peninsula within the late Miocene Lake Pannon (Hungary). The lake was several hundred meters deep, and near to the study area it was about 50–80 km wide. The inferred paleo-tsunami deposit includes subangular clasts that are exclusively derived from the underlying Cretaceous sandstone. Imbrication of the bouldery gravel points to landward transport of the clasts, however, a 15-cm-thick lens of cross-bedded sand records an opposing flow direction. The clayey sand matrix contains fossils, i.e. fragmented and articulated mollusc shells, as well as ostracods, that lived on the nearby sandy shoreface and offshore. The facies of the gravel indicates a short-distance transport of clasts typical for an extreme wave event. None of the depositional features e.g. various degree of clast roundness, seaward dipping imbrication, bidirectional transport indicators, clast-supported fabric, large thickness of beds, and lack of grading is either unique to tsunami deposits or excludes storm wave origin. An extreme storm wave origin, however, is discarded in this case, when paleogeography and climate are considered. The combination of matrix-supported fabric, presence of a mixed clayey-sandy matrix in the clast-supported parts, and preservation of articulated mollusc shells, as well as mixture of clasts and fossils from different zones of the shore, identify these beds as paleo-tsunami deposits. As coeval volcanism is not known, a hypothetic tsunami could have been related either to an earthquake along nearby normal faults or to large-scale sliding events on the closely located shelf slope due to rapid deposition or seismic shocks. The recognition of these event beds reinforces structural observations on the syn-depositional character of nearby faults, active after the middle Miocene climax of synrift tectonics in the Pannonian Basin. Thick, boulder-sized onshore paleo-tsunamiites are useful indicators of a paleogeographic situation in which tsunami waves were amplified to produce noticeable beds in the rock record." @default.
• W3086570414 created "2020-09-21" @default.
• W3086570414 creator A5010463648 @default.
• W3086570414 creator A5030879768 @default.
• W3086570414 creator A5058073393 @default.
• W3086570414 creator A5061293396 @default.
• W3086570414 creator A5072376035 @default.
• W3086570414 creator A5086993941 @default.
• W3086570414 date "2020-12-01" @default.
• W3086570414 modified "2023-10-17" @default.
• W3086570414 title "Facies and implications of a coarse-grained lacustrine onshore paleo-tsunamiite: An integrated study of an upper Miocene bouldery cobble gravel" @default.
• W3086570414 cites W1518859909 @default.
• W3086570414 cites W1553120861 @default.
• W3086570414 cites W1875988652 @default.
• W3086570414 cites W1904854050 @default.
• W3086570414 cites W1964577047 @default.
• W3086570414 cites W1966801905 @default.
• W3086570414 cites W1974283590 @default.
• W3086570414 cites W1983903585 @default.
• W3086570414 cites W1984414941 @default.
• W3086570414 cites W1985089912 @default.
• W3086570414 cites W1985975295 @default.
• W3086570414 cites W1988040128 @default.
• W3086570414 cites W2003076378 @default.
• W3086570414 cites W2007765260 @default.
• W3086570414 cites W2012251860 @default.
• W3086570414 cites W2012971520 @default.
• W3086570414 cites W2014861396 @default.
• W3086570414 cites W2016678130 @default.
• W3086570414 cites W2018166685 @default.
• W3086570414 cites W2019916888 @default.
• W3086570414 cites W2023317688 @default.
• W3086570414 cites W2023965570 @default.
• W3086570414 cites W2024095187 @default.
• W3086570414 cites W2027272184 @default.
• W3086570414 cites W2030347900 @default.
• W3086570414 cites W2033452743 @default.
• W3086570414 cites W2034076464 @default.
• W3086570414 cites W2034682255 @default.
• W3086570414 cites W2034774873 @default.
• W3086570414 cites W2034902010 @default.
• W3086570414 cites W2037761763 @default.
• W3086570414 cites W2040733918 @default.
• W3086570414 cites W2041734868 @default.
• W3086570414 cites W2041975830 @default.
• W3086570414 cites W2048798381 @default.
• W3086570414 cites W2051060861 @default.
• W3086570414 cites W2051574583 @default.
• W3086570414 cites W2056403055 @default.
• W3086570414 cites W2058659553 @default.
• W3086570414 cites W2062659097 @default.
• W3086570414 cites W2064254065 @default.
• W3086570414 cites W2064869784 @default.
• W3086570414 cites W2066362794 @default.
• W3086570414 cites W2066711002 @default.
• W3086570414 cites W2068600269 @default.
• W3086570414 cites W2073319947 @default.
• W3086570414 cites W2073688362 @default.
• W3086570414 cites W2074580567 @default.
• W3086570414 cites W2079035254 @default.
• W3086570414 cites W2079321554 @default.
• W3086570414 cites W2080464240 @default.
• W3086570414 cites W2082611744 @default.
• W3086570414 cites W2083076018 @default.
• W3086570414 cites W2089111480 @default.
• W3086570414 cites W2089882631 @default.
• W3086570414 cites W2090061281 @default.
• W3086570414 cites W2093443145 @default.
• W3086570414 cites W2094811045 @default.
• W3086570414 cites W2099458900 @default.
• W3086570414 cites W2102272866 @default.
• W3086570414 cites W2106472685 @default.
• W3086570414 cites W2111233732 @default.
• W3086570414 cites W2112672253 @default.
• W3086570414 cites W2115333736 @default.
• W3086570414 cites W2120162798 @default.
• W3086570414 cites W2122086884 @default.
• W3086570414 cites W2129201475 @default.
• W3086570414 cites W2132528772 @default.
• W3086570414 cites W2138409529 @default.
• W3086570414 cites W2157505241 @default.
• W3086570414 cites W2177906243 @default.
• W3086570414 cites W2268825196 @default.
• W3086570414 cites W2269207215 @default.
• W3086570414 cites W2344977901 @default.
• W3086570414 cites W2433518534 @default.
• W3086570414 cites W2560743889 @default.
• W3086570414 cites W2566959168 @default.
• W3086570414 cites W2570996466 @default.
• W3086570414 cites W2580978574 @default.
• W3086570414 cites W2582227996 @default.
• W3086570414 cites W2603908475 @default.
• W3086570414 cites W2609580193 @default.
• W3086570414 cites W2614496091 @default.
• W3086570414 cites W2621479184 @default.
• W3086570414 cites W2739959283 @default.
• W3086570414 cites W2740337197 @default.
• W3086570414 cites W2754837767 @default.

• next