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Earth Science
Czechia
2025

D-Index & Metrics

Discipline name D-Index World Ranking Current World Ranking National Ranking Current National Ranking Publications Citations
Earth Science 41 5643 5218 5 5 131 5155

Ondrej Lexa publications per year

The chart shows the history of publications by Ondrej Lexa between 1988 and 2026, highlighting the no. of papers published in each year and offering an overview of the publication velocity of this scholar. Ondrej Lexa published across 39 years, from 1988 to 2026, averaging 3.7 papers a year. Output peaked at 18 publications in 2014. 5 of the 144 publications appeared in the last two years.

No. of publications
5 10 15
Bar chart. Horizontal axis: year, 1988 to 2026. Vertical axis: number of publications, 0 to 18. Peak 18 publications in 2014. 1988: 1 publication 1989: 0 publications 1990: 0 publications 1991: 0 publications 1992: 0 publications 1993: 0 publications 1994: 0 publications 1995: 0 publications 1996: 0 publications 1997: 0 publications 1998: 0 publications 1999: 0 publications 2000: 2 publications 2001: 1 publication 2002: 1 publication 2003: 7 publications 2004: 3 publications 2005: 4 publications 2006: 2 publications 2007: 3 publications 2008: 6 publications 2009: 5 publications 2010: 7 publications 2011: 7 publications 2012: 9 publications 2013: 3 publications 2014: 18 publications 2015: 7 publications 2016: 7 publications 2017: 10 publications 2018: 8 publications 2019: 3 publications 2020: 4 publications 2021: 7 publications 2022: 7 publications 2023: 4 publications 2024: 3 publications 2025: 4 publications 2026: 1 publication
1988 2026

144 publications in total across all disciplines

View publications per year as a table
Ondrej Lexa: publications per year, 1988 to 2026
Year Publications
1988 1
1989 0
1990 0
1991 0
1992 0
1993 0
1994 0
1995 0
1996 0
1997 0
1998 0
1999 0
2000 2
2001 1
2002 1
2003 7
2004 3
2005 4
2006 2
2007 3
2008 6
2009 5
2010 7
2011 7
2012 9
2013 3
2014 18
2015 7
2016 7
2017 10
2018 8
2019 3
2020 4
2021 7
2022 7
2023 4
2024 3
2025 4
2026 1
Total 144
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Ondrej Lexa 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 Ondrej Lexa 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, 128–137 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: 131 publications — 28th percentile

28% 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
128–137 557 131
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
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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Ondrej Lexa 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 Ondrej Lexa 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, 41 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: 41 D-Index — 41st percentile

41% 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
36 389
37 366
38 344
39 349
40 296
41 289 41
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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Research.com Recognitions

  • 2025 - Research.com Earth Science in Czechia Leader Award
  • 2023 - Research.com Earth Science in Czechia Leader Award
  • 2022 - Research.com Earth Science in Czechia Leader Award

Overview

Ondrej Lexa is affiliated with Charles University in the Czech Republic. Their research primarily focuses on Earth and Planetary Sciences, with a strong emphasis on geophysics as demonstrated by 39 publications in this subfield. Additional areas of study include Artificial Intelligence, Mechanics of Materials, Ocean Engineering, and Geochemistry and Petrology.

The main topics of Lexa's work cover a range of geological and geophysical subjects:

  • Geological and Geochemical Analysis
  • High-pressure geophysics and materials
  • Geochemistry and Geologic Mapping
  • Geological Formations and Processes Exploration
  • Earthquake and tectonic studies
  • Rock Mechanics and Modeling
  • Mineralogy and Gemology Studies

Lexa has contributed to a variety of academic journals, with frequent publications appearing in:

  • Gondwana Research
  • Tectonics
  • Journal of Structural Geology
  • Journal of Metamorphic Geology
  • Tectonophysics

Some of their recent papers include:

  • Trans-lithospheric diapirism explains the presence of ultra-high pressure rocks in the European Variscides (2021, Communications Earth & Environment)
  • Structural, metamorphic and geochronological constraints on Palaeozoic multi-stage geodynamic evolution of the Altai accretionary wedge system (Hovd Zone, western Mongolia) (2021, Lithos)
  • Eclogite subduction wedge intruded by arc-type magma: The earliest record of Variscan arc in the Bohemian Massif (2021, Gondwana Research)
  • Structures and geodynamics of the Mongolian tract of the Central Asian Orogenic Belt constrained by potential field analyses (2021, Gondwana Research)
  • Paleozoic Geodynamics and Architecture of the Southern Part of the Mongolian Altai Zone (2022, Tectonics)

Lexa frequently collaborates with several researchers, including:

  • Karel Schulmann (11 coauthored papers)
  • Petr Jeřábek (10 coauthored papers)
  • Pavla Štípská (6 coauthored papers)
  • Vít Peřestý (5 coauthored papers)
  • Jitka Míková (5 coauthored papers)

Best Publications

  • An Andean type Palaeozoic convergence in the Bohemian Massif

    Karel Schulmann;Jiří Konopásek;Vojtĕch Janoušek;Ondrej Lexa

  • Chronological constraints on the pre-orogenic history, burial and exhumation of deep-seated rocks along the eastern margin of the Variscan Orogen, Bohemian Massif, Czech Republic

    Karel Schulmann;Alfred Kröner;Ernst Hegner;Immo Wendt

  • Lithostratigraphic and geochronological constraints on the evolution of the Central Asian Orogenic Belt in SW Mongolia: Early Paleozoic rifting followed by late Paleozoic accretion

    Alfred Kröner;Jérémie Lehmann;Karel Schulmann;Antoine Demoux

  • Structural constraints on the evolution of the Central Asian Orogenic Belt in SW Mongolia

    Jérémie Lehmann;Karel Schulmann;Ondrej Lexa;Michel Corsini

  • Vertical extrusion and horizontal channel flow of orogenic lower crust: key exhumation mechanisms in large hot orogens?

    K. Schulmann;O. Lexa;P. Štípská;M. Racek

  • Anatomy of a diffuse cryptic suture zone: An example from the Bohemian Massif, European Variscides

    Karel Schulmann;Ondrej Lexa;Vojtěch Janoušek;Jean Marc Lardeaux

  • Heat sources and trigger mechanisms of exhumation of HP granulites in Variscan orogenic root.

    O Lexa;Karel Schulmann;V Janoušek;P. Štípská

  • The Moldanubian Zone in the French Massif Central, Vosges/Schwarzwald and Bohemian Massif revisited: differences and similarities

    J. M. Lardeaux;Karel Schulmann;Michel Faure;V Janoušek

  • Late Palaeozoic palaeomagnetic and tectonic constraints for amalgamation of Pangea supercontinent in the European Variscan belt

    Jean Bernard Edel;Karel Schulmann;Ondrej Lexa;Jean Marc Lardeaux

  • Metamorphic record of burial and exhumation of orogenic lower and middle crust: a new tectonothermal model for the Drosendorf window (Bohemian Massif, Austria)

    M. Racek;M. Racek;P. Štípská;P. Pitra;K. Schulmann

  • Anatexis of accretionary wedge, Pacific‐type magmatism, and formation of vertically stratified continental crust in the Altai Orogenic Belt

    Yuchao Jiang;Yuchao Jiang;K. Schulmann;M. Sun;P. Štípská

  • Origin of migmatites by deformation-enhanced melt infiltration of orthogneiss: a new model based on quantitative microstructural analysis

    P. Hasalová;K. Schulmann;O. Lexa;P. Štípská

  • Early Cambrian eclogites in SW Mongolia: evidence that the Palaeo‐Asian Ocean suture extends further east than expected

    P. Štípská;K. Schulmann;J. Lehmann;M. Corsini

  • Late Paleozoic–Mesozoic tectonic evolution of the Trans-Altai and South Gobi Zones in southern Mongolia based on structural and geochronological data

    Alexandra Guy;Alexandra Guy;Karel Schulmann;Norbert Clauer;Pavlina Hasalová

  • Mid-crustal shear zone formation in granitic rocks: Constraints from quantitative textural and crystallographic preferred orientations analyses

    Emilien Oliot;Emilien Oliot;Philippe Goncalves;Karel Schulmann;Didier Marquer

  • Geochemical and geochronological constraints on distinct Early-Neoproterozoic and Cambrian accretionary events along southern margin of the Baydrag Continent in western Mongolia

    David Buriánek;Karel Schulmann;Kristýna Hrdličková;Pavel Hanžl

  • Transforming mylonitic metagranite by open-system interactions during melt flow

    Pavlina Hasalova;Pavla Stipska;Roger Powell;Karel Schulmann

  • Crustal influx, indentation, ductile thinning and gravity redistribution in a continental wedge: Building a Moldanubian mantled gneiss dome with underthrust Saxothuringian material (European Variscan belt)

    F. Chopin;F. Chopin;K. Schulmann;E. Skrzypek;J. Lehmann

  • A geophysical model of the Variscan orogenic root (Bohemian Massif): Implications for modern collisional orogens

    Alexandra Guy;Alexandra Guy;Jean-Bernard Edel;Karel Schulmann;Čestmir Tomek

  • Model of syn‐convergent extrusion of orogenic lower crust in the core of the Variscan belt: implications for exhumation of high‐pressure rocks in large hot orogens

    J. Franěk;K. Schulmann;O. Lexa;Č. Tomek

  • Neoproterozoic-Early Paleozoic Peri-Pacific Accretionary Evolution of the Mongolian Collage System: Insights From Geochemical and U-Pb Zircon Data From the Ordovician Sedimentary Wedge in the Mongolian Altai

    Y. D. Jiang;Y. D. Jiang;K. Schulmann;A. Kröner;M. Sun

  • Cretaceous collision and indentation in the West Carpathians: View based on structural analysis and numerical modeling

    Ondrej Lexa;Karel Schulmann;Josef Ježek

Frequent Co-Authors

Karel Schulmann
Karel Schulmann University of Strasbourg
Pavla Štípská
Pavla Štípská University of Strasbourg
Jean-Bernard Edel
Jean-Bernard Edel University of Strasbourg
Alfred Kröner
Alfred Kröner Johannes Gutenberg University of Mainz
John W. Cosgrove
John W. Cosgrove Imperial College London
Andrew R.C. Kylander-Clark
Andrew R.C. Kylander-Clark University of California, Santa Barbara
Min Sun
Min Sun University of Hong Kong
Bradley R. Hacker
Bradley R. Hacker University of California, Santa Barbara
František Hrouda
František Hrouda Charles University
Chao Yuan
Chao Yuan Chinese Academy of Sciences

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