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.
Microfractures: A review
2014325 citationsMark H. Anders, Christopher H. Scholz et al.profile →
Peers — A (Enhanced Table)
Peers by citation overlap · career bar shows stage (early→late)
cites ·
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Countries citing papers authored by Mark H. Anders
Since
Specialization
Citations
This map shows the geographic impact of Mark H. Anders'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 Mark H. Anders with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Mark H. Anders more than expected).
This network shows the impact of papers produced by Mark H. Anders. 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 Mark H. Anders. The network helps show where Mark H. Anders may publish in the future.
Co-authorship network of co-authors of Mark H. Anders
This figure shows the co-authorship network connecting the top 25 collaborators of Mark H. Anders.
A scholar is included among the top collaborators of Mark H. Anders 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 Mark H. Anders. Mark H. Anders is excluded from
the visualization to improve readability, since they are connected to all nodes in the network.
Malone, David H., et al.. (2014). Age and Provenance of the Eocene Crandall Conglomerate: Implications for the Emplacement of the Heart Mountain Slide. The Mountain Geologist. 51(4). 249–277.3 indexed citations
Goren, Liran, Einat Aharonov, & Mark H. Anders. (2010). The long runout of the Heart Mountain landslide: A chemo-thermo-poro-elastic mechanism. EGUGA. 2009. 10350.3 indexed citations
Anders, Mark H., et al.. (1993). Lower crustal flow: The origin of Late Cenozoic extension north of the eastern Snake River Plain. Geological Society of America, Abstracts with Programs; (United States).1 indexed citations
14.
Bjarnason, Ingi Th., P. A. Cowie, Mark H. Anders, L. Seeber, & Christopher H. Scholz. (1993). The 1912 Iceland earthquake rupture: Growth and development of a nascent transform system. Bulletin of the Seismological Society of America. 83(2). 416–435.72 indexed citations
Anders, Mark H., et al.. (1992). Growth and linkage of normal faults. Geological Society of America, Abstracts with Programs; (United States).2 indexed citations
17.
Dawers, Nancye H. & Mark H. Anders. (1992). Displacement-length scaling for normal faults of the Volcanic Tableland'', eastern California. Geological Society of America, Abstracts with Programs; (United States).2 indexed citations
Asaro, Frank, Walter Álvarez, Helen V. Michel, et al.. (1988). Possible world-wide middle miocene iridium anomaly and its relationship to periodicity of impacts and extinctions. 673. 6.1 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.