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D-Index & Metrics

Discipline name D-Index World Ranking Current World Ranking National Ranking Current National Ranking Publications Citations
Earth Science 35 7597 7034 161 156 242 4783

Pierre Lanari publications per year

The chart shows the history of publications by Pierre Lanari between 2009 and 2025, highlighting the no. of papers published in each year and offering an overview of the publication velocity of this scholar. Pierre Lanari published across 17 years, from 2009 to 2025, averaging 15.5 papers a year. Output peaked at 36 publications in 2017. 33 of the 264 publications appeared in the last two years.

No. of publications
10 20 30
Bar chart. Horizontal axis: year, 2009 to 2025. Vertical axis: number of publications, 0 to 36. Peak 36 publications in 2017. 2009: 1 publication 2010: 1 publication 2011: 0 publications 2012: 9 publications 2013: 9 publications 2014: 12 publications 2015: 12 publications 2016: 11 publications 2017: 36 publications 2018: 25 publications 2019: 22 publications 2020: 24 publications 2021: 26 publications 2022: 14 publications 2023: 29 publications 2024: 19 publications 2025: 14 publications
2009 2025

264 publications in total across all disciplines

View publications per year as a table
Pierre Lanari: publications per year, 2009 to 2025
Year Publications
2009 1
2010 1
2011 0
2012 9
2013 9
2014 12
2015 12
2016 11
2017 36
2018 25
2019 22
2020 24
2021 26
2022 14
2023 29
2024 19
2025 14
Total 264
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Pierre Lanari publication distribution in Earth Science in 2026

The chart shows the distribution of publications by all Research.com ranked scientists in the field of Earth Science in 2026. The highlighted bar marks where Pierre Lanari sits on this spectrum.

No. of scientists
100 200 300 400 500
Bar chart with 58 bars. Horizontal axis: publications, 38–47 to 603+. Vertical axis: number of scientists, 0 to 557. Most scientists, 557, have 128–137 publications. The last bar groups every scientist with 603 publications or more. The highlighted bar, 238–247 publications, is where this scientist sits. 38–47 publications: 5 scientists 48–57 publications: 33 scientists 58–67 publications: 94 scientists 68–77 publications: 161 scientists 78–87 publications: 278 scientists 88–97 publications: 376 scientists 98–107 publications: 404 scientists 108–117 publications: 484 scientists 118–127 publications: 540 scientists 128–137 publications: 557 scientists 138–147 publications: 491 scientists 148–157 publications: 495 scientists 158–167 publications: 458 scientists 168–177 publications: 490 scientists 178–187 publications: 414 scientists 188–197 publications: 401 scientists 198–207 publications: 333 scientists 208–217 publications: 292 scientists 218–227 publications: 290 scientists 228–237 publications: 262 scientists 238–247 publications: 243 scientists 248–257 publications: 208 scientists 258–267 publications: 185 scientists 268–277 publications: 147 scientists 278–287 publications: 128 scientists 288–297 publications: 119 scientists 298–307 publications: 120 scientists 308–317 publications: 107 scientists 318–327 publications: 93 scientists 328–337 publications: 87 scientists 338–347 publications: 64 scientists 348–357 publications: 87 scientists 358–367 publications: 60 scientists 368–377 publications: 60 scientists 378–387 publications: 34 scientists 388–397 publications: 50 scientists 398–407 publications: 44 scientists 408–417 publications: 31 scientists 418–427 publications: 39 scientists 428–437 publications: 27 scientists 438–447 publications: 36 scientists 448–457 publications: 27 scientists 458–467 publications: 29 scientists 468–477 publications: 30 scientists 478–487 publications: 19 scientists 488–497 publications: 15 scientists 498–507 publications: 18 scientists 508–517 publications: 19 scientists 518–527 publications: 16 scientists 528–537 publications: 10 scientists 538–547 publications: 11 scientists 548–557 publications: 14 scientists 558–567 publications: 11 scientists 568–577 publications: 7 scientists 578–587 publications: 14 scientists 588–597 publications: 5 scientists 598–602 publications: 4 scientists 603+ publications: 100 scientists
38–47 publications 603+

This scientist: 242 publications — 76th percentile

76% of scientists in this discipline score the same or lower.

The last bar groups every scientist with 603 publications or more.

View publications distribution as a table
Number of Earth Science scientists by publication count, Research.com 2026 ranking edition. Based on 9,176 ranked scientists.
Publications Scientists This scientist
38–47 5
48–57 33
58–67 94
68–77 161
78–87 278
88–97 376
98–107 404
108–117 484
118–127 540
128–137 557
138–147 491
148–157 495
158–167 458
168–177 490
178–187 414
188–197 401
198–207 333
208–217 292
218–227 290
228–237 262
238–247 243 242
248–257 208
258–267 185
268–277 147
278–287 128
288–297 119
298–307 120
308–317 107
318–327 93
328–337 87
338–347 64
348–357 87
358–367 60
368–377 60
378–387 34
388–397 50
398–407 44
408–417 31
418–427 39
428–437 27
438–447 36
448–457 27
458–467 29
468–477 30
478–487 19
488–497 15
498–507 18
508–517 19
518–527 16
528–537 10
538–547 11
548–557 14
558–567 11
568–577 7
578–587 14
588–597 5
598–602 4
603+ 100
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Pierre Lanari D-index placement in Earth Science in 2026

The chart shows the D-index (discipline H-index) distribution of Earth Science scientists ranked by Research.com in 2026. The highlighted bar marks where Pierre Lanari sits on this spectrum.

No. of scientists
100 200 300
Bar chart with 77 bars. Horizontal axis: D-Index, 30 to 106+. Vertical axis: number of scientists, 0 to 389. Most scientists, 389, have 36 D-Index. The last bar groups every scientist with 106 D-Index or more. The highlighted bar, 35 D-Index, is where this scientist sits. 30 D-Index: 144 scientists 31 D-Index: 215 scientists 32 D-Index: 278 scientists 33 D-Index: 379 scientists 34 D-Index: 366 scientists 35 D-Index: 372 scientists 36 D-Index: 389 scientists 37 D-Index: 366 scientists 38 D-Index: 344 scientists 39 D-Index: 349 scientists 40 D-Index: 296 scientists 41 D-Index: 289 scientists 42 D-Index: 277 scientists 43 D-Index: 279 scientists 44 D-Index: 248 scientists 45 D-Index: 257 scientists 46 D-Index: 212 scientists 47 D-Index: 202 scientists 48 D-Index: 207 scientists 49 D-Index: 204 scientists 50 D-Index: 183 scientists 51 D-Index: 178 scientists 52 D-Index: 182 scientists 53 D-Index: 178 scientists 54 D-Index: 163 scientists 55 D-Index: 117 scientists 56 D-Index: 163 scientists 57 D-Index: 120 scientists 58 D-Index: 113 scientists 59 D-Index: 136 scientists 60 D-Index: 135 scientists 61 D-Index: 96 scientists 62 D-Index: 103 scientists 63 D-Index: 83 scientists 64 D-Index: 103 scientists 65 D-Index: 83 scientists 66 D-Index: 89 scientists 67 D-Index: 92 scientists 68 D-Index: 89 scientists 69 D-Index: 78 scientists 70 D-Index: 75 scientists 71 D-Index: 53 scientists 72 D-Index: 62 scientists 73 D-Index: 54 scientists 74 D-Index: 35 scientists 75 D-Index: 52 scientists 76 D-Index: 50 scientists 77 D-Index: 32 scientists 78 D-Index: 37 scientists 79 D-Index: 20 scientists 80 D-Index: 33 scientists 81 D-Index: 36 scientists 82 D-Index: 34 scientists 83 D-Index: 34 scientists 84 D-Index: 24 scientists 85 D-Index: 19 scientists 86 D-Index: 18 scientists 87 D-Index: 26 scientists 88 D-Index: 30 scientists 89 D-Index: 17 scientists 90 D-Index: 21 scientists 91 D-Index: 19 scientists 92 D-Index: 15 scientists 93 D-Index: 14 scientists 94 D-Index: 20 scientists 95 D-Index: 9 scientists 96 D-Index: 10 scientists 97 D-Index: 15 scientists 98 D-Index: 13 scientists 99 D-Index: 3 scientists 100 D-Index: 13 scientists 101 D-Index: 3 scientists 102 D-Index: 9 scientists 103 D-Index: 4 scientists 104 D-Index: 6 scientists 105 D-Index: 6 scientists 106+ D-Index: 98 scientists
30 D-Index 106+

This scientist: 35 D-Index — 19th percentile

19% of scientists in this discipline score the same or lower.

The last bar groups every scientist with 106 D-Index or more.

View D-Index distribution as a table
Number of Earth Science scientists by D-index, Research.com 2026 ranking edition. Based on 9,176 ranked scientists.
D-Index Scientists This scientist
30 144
31 215
32 278
33 379
34 366
35 372 35
36 389
37 366
38 344
39 349
40 296
41 289
42 277
43 279
44 248
45 257
46 212
47 202
48 207
49 204
50 183
51 178
52 182
53 178
54 163
55 117
56 163
57 120
58 113
59 136
60 135
61 96
62 103
63 83
64 103
65 83
66 89
67 92
68 89
69 78
70 75
71 53
72 62
73 54
74 35
75 52
76 50
77 32
78 37
79 20
80 33
81 36
82 34
83 34
84 24
85 19
86 18
87 26
88 30
89 17
90 21
91 19
92 15
93 14
94 20
95 9
96 10
97 15
98 13
99 3
100 13
101 3
102 9
103 4
104 6
105 6
106+ 98
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Overview

Pierre Lanari is affiliated with the University of Bern in Switzerland and contributes extensively to the field of Earth and Planetary Sciences. Their work spans multiple subfields, including Geophysics, Artificial Intelligence, Mechanics of Materials, Geochemistry and Petrology, and Atmospheric Science.

Their research covers a broad range of main topics such as Geological and Geochemical Analysis, earthquake and tectonic studies, Geochemistry and Geologic Mapping, High-pressure geophysics and materials, Hydrocarbon exploration and reservoir analysis, Geology and Paleoclimatology Research, and Geochemistry and Elemental Analysis.

Lanari has published numerous papers in respected scientific journals, with notable recent works including:

  • First evidence of eclogites overprinted by ultrahigh temperature metamorphism in Everest East, Himalaya: Implications for collisional tectonics on early Earth (2021, Earth and Planetary Science Letters)
  • Identification of growth mechanisms in metamorphic garnet by high-resolution trace element mapping with LA-ICP-TOFMS (2020, Contributions to Mineralogy and Petrology)
  • The role of the antigorite + brucite to olivine reaction in subducted serpentinites (Zermatt, Switzerland) (2020, Swiss Journal of Geosciences)
  • Magmatic flare-up causes crustal thickening at the transition from subduction to continental collision (2021, Communications Earth & Environment)
  • Titanium isotopic compositions of bulk rocks and mineral separates from the Kos magmatic suite: Insights into fractional crystallization and magma mixing processes (2021, Chemical Geology)

Frequent co-authors collaborating with Lanari include:

  • Jörg Hermann
  • Daniela Rubatto
  • Thomas Pettke
  • Francesca Piccoli
  • Thorsten Markmann

Publication venues where Lanari has contributed multiple works are:

  • Journal of Metamorphic Geology
  • Contributions to Mineralogy and Petrology
  • Chemical Geology
  • Earth and Planetary Science Letters
  • Swiss Journal of Geosciences

Best Publications

  • XMapTools: A MATLAB©-based program for electron microprobe X-ray image processing and geothermobarometry

    Pierre Lanari;Pierre Lanari;Olivier Vidal;Vincent De Andrade;Benoít Dubacq;Benoít Dubacq;Benoít Dubacq

  • Pressure-temperature estimates of the lizardite/antigorite transition in high pressure serpentinites

    Stéphane Schwartz;Stéphane Guillot;Bruno Reynard;Romain Lafay

  • A thermodynamic model for di-trioctahedral chlorite from experimental and natural data in the system MgO–FeO–Al2O3–SiO2–H2O: applications to P–T sections and geothermometry

    Pierre Lanari;Pierre Lanari;Thomas Wagner;Olivier Vidal

  • Local Bulk Composition Effects on Metamorphic Mineral Assemblages

    Pierre Lanari;Martin Engi

  • Quantitative compositional mapping of mineral phases by electron probe micro-analyser

    Pierre Lanari;Alice Vho;Thomas Bovay;Laura Airaghi

  • Modeling Metamorphic Rocks Using Equilibrium Thermodynamics and Internally Consistent Databases: Past Achievements, Problems and Perspectives

    Pierre Lanari;Erik Duesterhoeft

  • Neotethys closure history of Anatolia: insights from 40Ar–39Ar geochronology and P–T estimation in high pressure metasedimentary rocks

    Amaury Pourteau;Masafumi Sudo;Osman Candan;P. Lanari

  • Diachronous evolution of the alpine continental subduction wedge: Evidence from P-T estimates in the Brianconnais Zone houillère (France - Western Alps)

    Pierre Lanari;Stéphane Guillot;Stéphane Schwartz;Olivier Vidal

  • Significant Ages—An Introduction to Petrochronology

    Martin Engi;Pierre Lanari;Matthew J. Kohn

  • Deciphering high-pressure metamorphism in collisional context using microprobe mapping methods: Application to the Stak eclogitic massif (northwest Himalaya)

    Pierre Lanari;Nicolas Riel;Stéphane Guillot;Olivier Vidal

  • Trace element mapping by LA-ICP-MS: assessing geochemical mobility in garnet

    Tom Raimondo;Justin Payne;Benjamin Wade;Pierre Lanari

  • First evidence of eclogites overprinted by ultrahigh temperature metamorphism in Everest East, Himalaya: Implications for collisional tectonics on early Earth

    Jia-Min Wang;Pierre Lanari;Fu-Yuan Wu;Jin-Jiang Zhang

  • Reconstruction of multiple P-T-t stages from retrogressed mafic rocks: Subduction versus collision in the Southern Brasília orogen (SE Brazil)

    Mahyra Tedeschi;Mahyra Tedeschi;Pierre Lanari;Daniela Rubatto;Daniela Rubatto;Antônio Pedrosa-Soares

  • Syn- to post-orogenic exhumation of metamorphic nappes: Structure and thermobarometry of the western Attic-Cycladic metamorphic complex (Lavrion, Greece)

    Christophe Scheffer;Olivier Vanderhaeghe;Olivier Vanderhaeghe;Pierre Lanari;Alexandre Tarantola

  • An Internally-Consistent Database for Oxygen Isotope Fractionation Between Minerals

    Alice Vho;Pierre Lanari;Daniela Rubatto;Daniela Rubatto

  • Deciphering temperature, pressure and oxygen-activity conditions of chlorite formation

    Olivier Vidal;Pierre Lanari;Manuel Munoz;Franck Bourdelle

  • Late Paleozoic evolution of the South Tien Shan: Insights from P–T estimates and allanite geochronology on retrogressed eclogites (Chatkal range, Kyrgyzstan),

    Chloé Loury;Yann Rolland;Bénédicte Cenki-Tok;Pierre Lanari

  • Exhumation of eclogite and blueschist (Cyclades, Greece): Pressure–temperature evolution determined by thermobarometry and garnet equilibrium modelling

    Valentin Laurent;Pierre Lanari;Inès Naïr;Inès Naïr;Romain Augier

  • Permian high-temperature metamorphism in the Western Alps (NW Italy)

    Barbara Eva Kunz;Paola Manzotti;Paola Manzotti;Brigitte von Niederhäusern;Martin Engi

  • Deeply subducted continental fragments – Part 1: Fracturing, dissolution–precipitation, and diffusion processes recorded by garnet textures of the central Sesia Zone (western Italian Alps)

    Francesco Giuntoli;Pierre Lanari;Martin Engi

Frequent Co-Authors

Martin Engi
Martin Engi University of Bern
Stéphane Guillot
Stéphane Guillot Grenoble Alpes University
Yann Rolland
Yann Rolland Université Savoie Mont Blanc
Olivier Vidal
Olivier Vidal Grenoble Alpes University
Thomas Pettke
Thomas Pettke University of Bern
Igor M. Villa
Igor M. Villa University of Milano-Bicocca
Alfons Berger
Alfons Berger University of Bern
Marco Herwegh
Marco Herwegh University of Bern
Stéphane Schwartz
Stéphane Schwartz Grenoble Alpes University
Lukas P. Baumgartner
Lukas P. Baumgartner University of Lausanne

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