Christopher C. Sorlien
About
In The Last Decade
Christopher C. Sorlien
46 papers receiving 1.0k citations
Peers
Comparison fields: 5 of 42
- Geophysics 860
- Atmospheric Science 454
- Earth-Surface Processes 241
- Oceanography 153
- Environmental Chemistry 89
Countries citing papers authored by Christopher C. Sorlien
This map shows the geographic impact of Christopher C. Sorlien'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 Christopher C. Sorlien with the expected number of citations based on a country's size and research output (numbers larger than one mean the country cites Christopher C. Sorlien more than expected).
Fields of papers citing papers by Christopher C. Sorlien
This network shows the impact of papers produced by Christopher C. Sorlien. 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 Christopher C. Sorlien. The network helps show where Christopher C. Sorlien may publish in the future.
Co-authorship network of co-authors of Christopher C. Sorlien
This figure shows the co-authorship network connecting the top 25 collaborators of Christopher C. Sorlien. A scholar is included among the top collaborators of Christopher C. Sorlien 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 Christopher C. Sorlien. Christopher C. Sorlien is excluded from the visualization to improve readability, since they are connected to all nodes in the network.
All Works
| # | Work | Indexed citations |
|---|---|---|
| 1 | 1 | |
| 2 | 30 | |
| 3 | 1 | |
| 4 | 0 | |
| 5 | Marine-to-lacustrine transition, mud volcanism, and slope instability in an active tectonic setting: the MIS 5 to 4 transition in the Sea of Marmara, Turkey | 1 |
| 6 | Anomalous Uplift at Pitas Point: Localized Phenomena or Indicator of Tsunamigenic M8 Earthquakes Along Coastal California? | 1 |
| 7 | The central branch of the North Anatolian Fault In The Southern Marmara Sea: Evidence for a distributed, Holocene-active fault system | 1 |
| 8 | 6 | |
| 9 | The Quaternary North Channel-Pitas Point Fault System in Northwest Santa Barbara Channel, California. | 2 |
| 10 | The SCEC 3D Community Fault Model (CFM-v5): An updated and expanded fault set of oblique crustal deformation and complex fault interaction for southern California | 3 |
| 11 | 8 | |
| 12 | Latest Pleistocene to Holocene Evolution of the Baie de Port au Prince, Haiti | 2 |
| 13 | A Seismo-Tectonic Signal From Offshore Sedimentation: The 2010 Haiti Earthquake and Prior Events | 2 |
| 14 | 62 | |
| 15 | Vertical Deformation of Late Quaternary Features Across Port-au-Prince Bay, Haiti | 1 |
| 16 | 21 | |
| 17 | High Resolution Multichannel Imaging of Basin Growth Along a Continental Transform: The Marmara Sea Along the North Anatolian Fault in NW Turkey | 0 |
| 18 | 3D Fault Geometry and Basin Evolution in the Northern Continental Borderland Offshore Southern California | 6 |
| 19 | Extending the High-Resolution Global Climate Record in Santa Barbara Basin: Developing a More Continuous Composite Section from Overlapping Cores | 1 |
| 20 | The Dume Fault, Northern Santa Monica Bay, California | 1 |
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.