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| 1 | Gela submarine slide: a major basin-wide e- vent in the Plio-Quaternary foredeep of Sicily 显示文摘 | Trincardi F Argnani A | 1990 | Geo-marine Let- ters1990，10，： | 1 |
| 2 | The PASTA project: investigation of Po and Apennine sediment transport and accumulation 显示文摘 | Nittrouer C A Miserocchi S Trincardi F | 2004 | Oceanography2004，17，： | 1 |
| 3 | Pleistocene ' muddy' forced-regression deposits on the Adriatic shelf: A comparison with prodelta deposits of the late Holocene highstand mud wedge显示文摘 | Ridente D Trincardi F | 2005 | Marine Geology2005，，： | 1 |
| 4 | Pleistocene“muddy”forced-regres-sion deposits on the Adriatic shelf:A comparison with prodeltadeposits of the Late Holocene highstand mud wedge显示文摘 | Ridente D Trincardi F | 2005 | Ma-rine Geology2005，，： | 1 |
| 5 | A high resolution late Holocene palaeo environmental record from the central Adriatic Sea 显示文摘 | Oldfield F Asioli A Accorsi C Langone L tlolph T Trincardi F A Mercuri A M Juggins S Wolff G Gibbs Z Vigliotti L Frignani M van der Post K Branch N | 2003 | Quatern Sci Rev2003，22，24： | 1 |
| 6 | Pleistocene 'muddy' forced-regression deposits on the Adriatic shelf: A comparison with prodelta deposits of the late Holocene highstand mud wedge显示文摘 | Domenico Ridente Fabio Trincardi | 2005 | Marine Geology2005，22，3223： | 1 |
| 7 | Eurostraform special issue of marine geology 显示文摘 | Weaver P P E Canals M Trincardi F | 2006 | Marine Geology2006，234，： | 1 |
| 8 | Evidence of soft sediment deformation,fluid escape,sediment failure and regional weak layers within the late Quaternary mud deposits of the Adriatic Sea显示文摘 | Trincardi F Cattaneo A Correggiari A | 2004 | Marine Geology2004，213，14： | 1 |
| 9 | Triggering mechanisms of slope instability processes and sediment failures on continental margins: a geotechnical approach显示文摘 | N. Sultan P. Cochonat M. Canals A. Cattaneo B. Dennielou H. Haflidason J.S. Laberg D. Long J. Mienert F. Trincardi R. Urgeles T.O. Vorren C. Wilson | 2004 | Marine Geology2004，，1： | 1 |
| 10 | Pleistocene ' muddy' forced-regression de- posits on the Adriatic shelf: A comparison with prodelta deposits of the late Holoeene highstand mud wedge显示文摘 | Ridente D Trincardi F | 2005 | Marine Geology2005，，： | 1 |
| 11 | Evidence of soft sediment deformation, fluid escape, sediment failure and regional weak layers within the late Quaternary mud deposits of the Adiiatic Sea 显示文摘 | Trincardi F Cattaneo A Correggiari A Ridente D | 2004 | Marine Geology2004，213，： | 1 |
| 12 | Contrasting slope channel styles on a prograding mud-prone margin显示文摘 | G. Dalla Valle F. Gamberi F. Trincardi L. Baglioni A. Errera P. Rocchini | 2012 | Marine and Petroleum Geology2012，，： | 1 |
| 13 | The modern Po Delta system: lobe switching and asymmetrical prodelta growth显示文摘 | Correggian A Cattaneo A Trincardi F | 2005 | Marine Geology2005，22，： | 1 |
| 14 | Large-scale single incised valley from a small catchment basin on the western Adriatic margin(central Mediterranean Sea)显示文摘 | Maselli V Trincardi F | 2013 | Global and Planetary Change2013，100，： | 1 |
| 15 | The combined effect of sea level and supply during Milankovitch cyclicity:Evidence from shallow-marine δ18O records and seqence architecture(Adriatic margin)显示文摘 | Ridente D Trincardi F Piva A | 2009 | Geology2009，37，11： | 1 |
| 16 | Evidence of soft sediment deformation,fluid escape,sediment failure and regional weak layers within the late Quaternary mud deposits of the Adriatic Sea显示文摘 | TRINCARDI F CATTANEO A CORREGGIARI A | 2004 | Marine Geology2004，213，： | 1 |
| 17 | Evidence of soft sediment deformation, fluid escape, sediment failure and regional weak layers within the late quaternary mud deposits of the Adriatic Sea显示文摘 | TRINCARDI F CATTANEO A CORREGGIARI A | 2004 | Marine Geology2004，213，14： | 1 |
| 18 | 公元前2.5万年西南亚得里亚海陆缘Gondola滑坡引发海啸的可能性显示文摘亚得里亚海西南陆缘,从陆架外缘到陆坡底部150km范围内,有多处边坡失稳的证据。上陆坡显示有多个陡峭的滑坡后壁,它们出现在向盆内缓倾的更新世海退序列的压实沉积单元中。在海底,Gondola滑坡是最明显的滑坡堆积,断块大,明显的滑痕(10km×2.5km)延伸到了陆架外缘(现今的深度约为180km,但滑塌时的古深度约为50m),约4.5km3的滑体移动的最大距离达到了50km。 | Stefano Tinti Gianluca Pagnoni Alberto Annigliato Fabio Trincardi Filippo Zaniboni Federica Foglini Fabiano Gamberi Daniel Minisini 杨丽娟(译) 闫章存(校对) | 2009 | 海洋地质2009，，1： | 0 |
| 19 | 滑坡形成的海底地形与西南亚得里亚海深水珊瑚生长之间的相互影响显示文摘在西南亚得里亚海大陆边缘150km长的区段内,从陆架外缘到坡底,都存在强烈的边坡失稳现象。已固结的更新世沉积单元的崩塌形成了从块状滑坡到细粒浊积岩的堆积物,侵蚀开阔陆坡以及巴里峡谷陡峭的谷壁。这带陆缘还受到成瀑布般落下陆架、接近海底时流速超过60cm/s的高密度水季节性作用的影响。这些现象的共同作用形成了各种底形,其中部分底形(例如崩塌块的硬化表面)证实是各种底栖的硬海底有机生物最好的安身之处。这种变形的垮塌形成的地貌加上冷的富营养海水的泻落, | Fabio Trincardi Marco Taviani Andre Freiwald Federica Foglini Giuseppe Verdicchio Daniel Minisini 杨丽娟(译) 闫章存(校对) | 2009 | 海洋地质2009，，1： | 0 |
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