T. van Weering

614 total citations
18 papers, 479 citations indexed

About

T. van Weering is a scholar working on Environmental Chemistry, Atmospheric Science and Oceanography. According to data from OpenAlex, T. van Weering has authored 18 papers receiving a total of 479 indexed citations (citations by other indexed papers that have themselves been cited), including 8 papers in Environmental Chemistry, 8 papers in Atmospheric Science and 7 papers in Oceanography. Recurrent topics in T. van Weering's work include Geology and Paleoclimatology Research (8 papers), Methane Hydrates and Related Phenomena (8 papers) and Geological formations and processes (5 papers). T. van Weering is often cited by papers focused on Geology and Paleoclimatology Research (8 papers), Methane Hydrates and Related Phenomena (8 papers) and Geological formations and processes (5 papers). T. van Weering collaborates with scholars based in Netherlands, United Kingdom and France. T. van Weering's co-authors include H. de Haas, Norbert Frank, Dominique Blamart, Jean‐Pierre Henriet, Martin White, J H Fred Jansen, D. Eisma, Henko de Stigter, J. Murray Roberts and Veerle A.I. Huvenne and has published in prestigious journals such as Earth and Planetary Science Letters, Marine Geology and Marine and Petroleum Geology.

In The Last Decade

T. van Weering

18 papers receiving 461 citations

Peers — A (Enhanced Table)

Peers by citation overlap · career bar shows stage (early→late) cites · hero ref

Name h Career Trend Papers Cites
T. van Weering Netherlands 9 249 236 168 143 118 18 479
Elsebeth Thomsen Norway 11 137 0.6× 289 1.2× 149 0.9× 139 1.0× 193 1.6× 18 467
Björn Lindberg Norway 7 150 0.6× 189 0.8× 94 0.6× 184 1.3× 103 0.9× 9 402
Naokazu Ahagon Japan 13 280 1.1× 520 2.2× 184 1.1× 81 0.6× 320 2.7× 25 628
A. McDonnell United States 8 182 0.7× 194 0.8× 112 0.7× 208 1.5× 84 0.7× 8 550
Igor M. Venâncio Brazil 15 292 1.2× 462 2.0× 134 0.8× 177 1.2× 122 1.0× 52 597
Peter T. Harris Australia 8 201 0.8× 292 1.2× 107 0.6× 205 1.4× 43 0.4× 9 449
Stephen M Dickson United States 9 116 0.5× 136 0.6× 80 0.5× 193 1.3× 108 0.9× 31 365
Jane A. Reid United States 13 133 0.5× 164 0.7× 113 0.7× 171 1.2× 45 0.4× 25 431
Kathryn M. Scanlon United States 14 193 0.8× 113 0.5× 106 0.6× 67 0.5× 65 0.6× 31 460
Moab Praxedes Gomes Brazil 13 127 0.5× 148 0.6× 128 0.8× 209 1.5× 38 0.3× 39 399

Countries citing papers authored by T. van Weering

Since Specialization
Citations

This map shows the geographic impact of T. van Weering's research. It shows the number of citations coming from papers published by authors working in each country. You can also color the map by specialization and compare the number of citations received by T. van Weering with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites T. van Weering more than expected).

Fields of papers citing papers by T. van Weering

Since Specialization
Physical SciencesHealth SciencesLife SciencesSocial Sciences

This network shows the impact of papers produced by T. van Weering. Nodes represent research fields, and links connect fields that are likely to share authors. Colored nodes show fields that tend to cite the papers produced by T. van Weering. The network helps show where T. van Weering may publish in the future.

Co-authorship network of co-authors of T. van Weering

This figure shows the co-authorship network connecting the top 25 collaborators of T. van Weering. A scholar is included among the top collaborators of T. van Weering based on the total number of citations received by their joint publications. Widths of edges represent the number of papers authors have co-authored together. Node borders signify the number of papers an author published with T. van Weering. T. van Weering is excluded from the visualization to improve readability, since they are connected to all nodes in the network.

All Works

18 of 18 papers shown
1.
Bahr, André, Thomas Pape, Friedrich Abegg, et al.. (2010). Authigenic carbonates from the eastern Black Sea as an archive for shallow gas hydrate dynamics – Results from the combination of CT imaging with mineralogical and stable isotope analyses. Marine and Petroleum Geology. 27(9). 1819–1829. 26 indexed citations
2.
Frank, Norbert, Cees van der Land, Christophe Colin, et al.. (2009). The Holocene occurrence of cold water corals in the NE Atlantic: Implications for coral carbonate mound evolution. Marine Geology. 266(1-4). 129–142. 77 indexed citations
3.
Beranzoli, Laura, Christian Berndt, Paolo Favali, et al.. (2008). ESONET: An European Sea Observatory Initiative. 1–6. 6 indexed citations
4.
White, Martin, J. Murray Roberts, & T. van Weering. (2007). Do bottom-intensified diurnal tidal currents shape the alignment of carbonate mounds in the NE Atlantic?. Geo-Marine Letters. 27(6). 391–397. 48 indexed citations
5.
Beranzoli, Laura, Christian Berndt, Juan José Dañobeitia, et al.. (2007). The European Deep Sea Observatories Network of Excellence ESONET. OCEANS 2007 - Europe. 1–6. 7 indexed citations
6.
Beranzoli, Laura, Christian Berndt, Paolo Favali, et al.. (2007). ESONET: a network to integrate European research on sea. 1–6. 2 indexed citations
7.
Frank, Norbert, Dominique Blamart, Christophe Colin, et al.. (2006). Upper Intermediate Water Reservoir Ages in the Northeastern Atlantic During the Past 11000 Years: New Evidence for Mid Holocene Freshening of the North Atlantic. Flanders Marine Institute (Flanders Marine Institute). 2006(52). 1 indexed citations
8.
Mienis, Furu, T. van Weering, H. de Haas, et al.. (2006). Carbonate mound development at the SW Rockall Trough margin based on high resolution TOBI and seismic recording. Marine Geology. 233(1-4). 1–19. 97 indexed citations
9.
Frank, Norbert, Martine Paterne, Linda K. Ayliffe, et al.. (2004). Eastern North Atlantic deep-sea corals: tracing upper intermediate water Δ14C during the Holocene. Earth and Planetary Science Letters. 219(3-4). 297–309. 94 indexed citations
10.
Thomsen, Laurenz, et al.. (2003). Processes in the benthic boundary layer at continental margins and their implication for carbon mineralization. EAEJA. 13212. 2 indexed citations
11.
Long, David A., Haflidi Haflidason, A.G. Stevenson, et al.. (2003). Mud mound / ?diapiric features in the Faroe - Shetland Channel. EGS - AGU - EUG Joint Assembly. 11201. 4 indexed citations
12.
Blamart, Dominique, Claire Rollion‐Bard, A. Juillet-Leclerc, et al.. (2003). C and O isotopes in deep-sea corals (Lophelia pertusa) measured by ion microprobe. 1 indexed citations
13.
Weering, T. van, et al.. (2002). Hydrographic Conditions At The Carbonate Mound Locations In The NE Atlantic. EGSGA. 6064. 2 indexed citations
14.
Priede, Imants G., P.M. Bagley, Peter Gray, et al.. (2002). Autonomous deep-ocean lander vehicles; modular approaches to design and operation. 3. 1238–1244. 4 indexed citations
15.
Kuijpers, Antoon, Tøve Nielsen, A. Akhmetzhanov, et al.. (2001). Late Quaternary slope instability on the Faeroe margin: mass flow features and timing of events. Geo-Marine Letters. 20(3). 149–159. 37 indexed citations
16.
Mienert, Jürgen, Fatima F Abrantes, G. A. Auffret, et al.. (1998). European North Atlantic Margin (ENAM I): sediment pathways, processes, and fluxes — an introduction. Marine Geology. 152(1-3). 3–6. 8 indexed citations
17.
Weaver, P.P.E., et al.. (1997). Researchers measure carbon cycling at continental shelves. Eos. 78(43). 482–482. 11 indexed citations
18.
Weering, T. van, J H Fred Jansen, & D. Eisma. (1973). Acoustic reflection profiles of the norwegian channel between oslo and bergen. Netherlands Journal of Sea Research. 6(1-2). 241–263. 52 indexed citations

Rankless uses publication and citation data sourced from OpenAlex, an open and comprehensive bibliographic database. While OpenAlex provides broad and valuable coverage of the global research landscape, it—like all bibliographic datasets—has inherent limitations. These include incomplete records, variations in author disambiguation, differences in journal indexing, and delays in data updates. As a result, some metrics and network relationships displayed in Rankless may not fully capture the entirety of a scholar's output or impact.

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