Characterization of a deeply buried paleokarst terrain in the Loppa High using core data and multiattribute seismic facies classification J Sayago, M Di Lucia, M Mutti, A Cotti, A Sitta, K Broberg, A Przybylo, ... AAPG bulletin 96 (10), 1843-1866, 2012 | 85 | 2012 |
Facies and seismic analysis of the Late Carboniferous–Early Permian Finnmark carbonate platform (southern Norwegian Barents Sea): An assessment of the carbonate factories and … M Di Lucia, J Sayago, G Frijia, A Cotti, A Sitta, M Mutti Marine and Petroleum Geology 79, 372-393, 2017 | 20 | 2017 |
Late Paleozoic seismic sequence stratigraphy and paleogeography of the paleo-Loppa High in the Norwegian Barents Sea J Sayago, M Di Lucia, M Mutti, A Sitta, A Cotti, G Frijia Marine and Petroleum Geology 97, 192-208, 2018 | 12 | 2018 |
Late Paleozoic basin analysis of the Loppa High and Finnmark Platform in the Norwegian Barents Sea: integration of seismic attributes and seismic sequence stratigraphy J Sayago Universität Potsdam, 2014 | 3 | 2014 |
Marine carbonate factories and stratigraphic response through time and space: Methodology, examples and implications A Letteron, J Sayago, J Michel, C Lanteaume, A Pohl, M Laugié, ... AGU Fall Meeting Abstracts 2020, PP008-0010, 2020 | 2 | 2020 |
3D Seismic Mapping with Attribute Analysis and Core Data to Detect Paleokarst Signatures in the Loppa High, Barents Sea J Sayago, M Di Lucia, M Mutti, A Cotti, A Sitta, K Broberg 73rd EAGE Conference and Exhibition incorporating SPE EUROPEC 2011, cp-238-00182, 2011 | 1 | 2011 |
Sedimentary Evolution of the Bashkirian-Moscovian Siliciclastic-carbonate Deposits of the Loppa High (Barents Sea) M Di Lucia, J Sayago, M Mutti, A Cotti, K Broberg, A Sitta 73rd EAGE Conference and Exhibition incorporating SPE EUROPEC 2011, cp-238-00598, 2011 | | 2011 |
Integrating 3D seismic mapping, volume based multi-attribute seismic facies classification and core analysis to characterize Paleokarst signatures in the Loppa High, Barents Sea J Sayago, M Di Lucia, M Mutti, A Cotti, A Sitta, K Broberg | | |