Hit papers significantly outperform the citation benchmark for their cohort. A paper qualifies
if it has ≥500 total citations, achieves ≥1.5× the top-1% citation threshold for papers in the
same subfield and year (this is the minimum needed to enter the top 1%, not the average
within it), or reaches the top citation threshold in at least one of its specific research
topics.
Shock metamorphism of quartz in nature and experiment: I. Basic observation and theory*
1994508 citationsD. Stöffler, F. Langenhorstprofile →
Peers — A (Enhanced Table)
Peers by citation overlap · career bar shows stage (early→late)
cites ·
hero ref
Countries citing papers authored by F. Langenhorst
Since
Specialization
Citations
This map shows the geographic impact of F. Langenhorst'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 F. Langenhorst with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites F. Langenhorst more than expected).
This network shows the impact of papers produced by F. Langenhorst. 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 F. Langenhorst. The network helps show where F. Langenhorst may publish in the future.
Co-authorship network of co-authors of F. Langenhorst
This figure shows the co-authorship network connecting the top 25 collaborators of F. Langenhorst.
A scholar is included among the top collaborators of F. Langenhorst 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 F. Langenhorst. F. Langenhorst is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Beegle, L. W., R. Bhartia, Lauren DeFlores, et al.. (2014). SHERLOC: Scanning Habitable Environments With Raman & Luminescence for Organics & Chemicals, an Investigation for 2020. 2014 AGU Fall Meeting. 2014.16 indexed citations
3.
Langenhorst, F., et al.. (2014). Martensitic Mechanism of the Zircon-to-Reidite Transformation. 77(1800). 5411.2 indexed citations
4.
Harries, Dennis & F. Langenhorst. (2014). Haxonite from 25143 Itokawa and its Implications for Metamorphic Parent Body Fluids. LPICo. 77(1800). 5136.1 indexed citations
5.
Harries, Dennis & F. Langenhorst. (2011). Nanocrystalline P-Bearing Pentlandite and Chromium Nitrides from CM2 Chondrites Y-791198 and Y-793321. Meteoritics and Planetary Science Supplement. 74. 5165.1 indexed citations
6.
Zolensky, M. E., M. Weisberg, M. A. Velbel, et al.. (2007). Wild-2 Déjà-Vu: Comparison of Wild-2 Particles to Chondrites and IDPs. LPI. 1481.4 indexed citations
7.
Langenhorst, F., et al.. (2006). Shock Metamorphic State of the Chassignite Northwest Africa 2737. Meteoritics and Planetary Science Supplement. 41. 5311.1 indexed citations
8.
Jacobsen, Steven D., H. C. Watson, F. Langenhorst, et al.. (2006). Synthesis and high-pressure synchrotron-infrared studies of OH-bearing silicate perovskite in the laser-heated diamond cell. AGU Fall Meeting Abstracts. 2006.1 indexed citations
9.
Terasaki, Hidenori, D. C. Rubie, Ute Mann, D. J. Frost, & F. Langenhorst. (2005). The Effects of Oxygen, Sulphur and Silicon on the Dihedral Angles Between Fe-rich Liquid Metal and Olivine, Ringwoodite and Silicate Perovskite: Implications for Planetary Core Formation. 36th Annual Lunar and Planetary Science Conference. 1129.1 indexed citations
10.
Langenhorst, F., Frank T. Kyte, & Gregory J. Retallack. (2005). Reexamination of Quartz Grains from the Permian-Triassic Boundary Section at Graphite Peak, Antarctica. 36th Annual Lunar and Planetary Science Conference. 2358.14 indexed citations
11.
Langenhorst, F., et al.. (2004). Experimental Reproduction of Shock Veins in Single-Crystal Minerals. LPI. 1478.1 indexed citations
12.
Terasaki, Hidenori, D. C. Rubie, D. J. Frost, & F. Langenhorst. (2003). Compositional effect on the dihedral angle between olivine and Fe-S liquid up to 20 GPa: Possibility of percolative core formation. AGU Fall Meeting Abstracts. 2003.1 indexed citations
13.
Langenhorst, F., Cliff S. J. Shaw, & K. Metzler. (2000). Mineral Chemistry and Microstructures in ALH84001. Lunar and Planetary Science Conference. 1866.1 indexed citations
14.
Langenhorst, F., A. Deutsch, B. A. Ivanov, & U. Hornemann. (2000). On the Shock Behavior of CaCO3: Dynamic Loading and Fast Unloading Experiments - Modeling - Mineralogical Observations. LPI. 1851.7 indexed citations
15.
Kyte, Frank T., F. Langenhorst, & Frank J. III Tepley. (2000). The Eltanin Meteorite: Large Messenger from the HED or Mesosiderite Parent Body?. Lunar and Planetary Science Conference. 71(4). 1811–30.1 indexed citations
16.
Langenhorst, F., A. Deutsch, & U. Hornemann. (1998). On the Shock Behavior of Calcite: Dynamic 85-GPa Compression, and Multianvil Decompression Experiments. M&PSA. 33.2 indexed citations
17.
Langenhorst, F. & Henning Dypvik. (1996). Microstructural Characteristics of Shocked Quartz from Ejecta of the Submarine Mjolnir Impact Structure, Barents Sea. Lunar and Planetary Science Conference. 27. 727.2 indexed citations
18.
Langenhorst, F. & A. Deutsch. (1996). The Azuara and Rubielos Structures, Spain: Twin Impact Craters or Alpine Thrust Systems? TEM Investigations on Deformed Quartz Disprove Shock Origin. Lunar and Planetary Science Conference. 27. 725.5 indexed citations
19.
Langenhorst, F., et al.. (1995). Meteorites for K-12 Classrooms: NASA Meteorite Educational Materials. Meteoritics and Planetary Science. 30(5). 537.2 indexed citations
20.
Langenhorst, F. & A. Deutsch. (1994). Shock experiments on pre-heated alpha - and beta -quartz: I. Optical and density data. Earth and Planetary Science Letters. 128. 699.6 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.