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Record W3095743390 · doi:10.1007/s11214-020-00739-x

Photogeologic Map of the Perseverance Rover Field Site in Jezero Crater Constructed by the Mars 2020 Science Team

2020· article· en· W3095743390 on OpenAlexaff
K. M. Stack, N. R. Williams, F. J. Calef, V. Z. Sun, Kenneth H. Williford, Kenneth A. Farley, Sigurd Eide, David Flannery, C. M. Hughes, Samantha Jacob, Linda C. Kah, Forrest Meyen, A. Molina, Cathy Quantin Nataf, M. S. Rice, Patrick Russell, Eva L. Scheller, Christina H. Seeger, William Abbey, Jacob Adler, H. E. F. Amundsen, R. B. Anderson, S. M. Angel, Gorka Arana, J. Atkins, M. Barrington, Tor Berger, Rose Borden, B. Boring, A. J. Brown, Brandi L. Carrier, P. G. Conrad, Henning Dypvik, S. A. Fagents, Z. E. Gallegos, Brad Garczynski, K. B. Golder, Felipe Gómez, Y. S. Goreva, Sanjeev Gupta, Svein‐Erik Hamran, Taryn Hicks, Eric D. Hinterman, B. Horgan, J. A. Hurowitz, J. R. Johnson, J. Lasue, R. E. Kronyak, Yang Liu, Juan Manuel Madariaga, N. Mangold, John McClean, N. Miklusicak, D. C. Nunes, Corrine Rojas, Kirby Runyon, Nicole Schmitz, N. A. Scudder, E. Shaver, Jason Soohoo, R. Spaulding, L. K. Tamppari, Michael M. Tice, Nathalie Turenne, Peter A. Willis, R. A. Yingst

Bibliographic record

VenueSpace Science Reviews · 2020
Typearticle
Languageen
FieldPhysics and Astronomy
TopicPlanetary Science and Exploration
Canadian institutionsUniversity of Winnipeg
FundersUniversitetet i OsloCentre National d’Etudes SpatialesDeutsches Zentrum für Luft- und RaumfahrtAgencia Estatal de InvestigaciónAgence Nationale de la RechercheNational Aeronautics and Space Administration
KeywordsMars Exploration ProgramAstrobiologyPlanetary scienceExploration of MarsGeologyImpact craterField (mathematics)Physics

Abstract

fetched live from OpenAlex

The Mars 2020 Perseverance rover landing site is located within Jezero crater, a ∼ 50 km diameter impact crater interpreted to be a Noachian-aged lake basin inside the western edge of the Isidis impact structure. Jezero hosts remnants of a fluvial delta, inlet and outlet valleys, and infill deposits containing diverse carbonate, mafic, and hydrated minerals. Prior to the launch of the Mars 2020 mission, members of the Science Team collaborated to produce a photogeologic map of the Perseverance landing site in Jezero crater. Mapping was performed at a 1:5000 digital map scale using a 25 cm/pixel High Resolution Imaging Science Experiment (HiRISE) orthoimage mosaic base map and a 1 m/pixel HiRISE stereo digital terrain model. Mapped bedrock and surficial units were distinguished by differences in relative brightness, tone, topography, surface texture, and apparent roughness. Mapped bedrock units are generally consistent with those identified in previously published mapping efforts, but this study's map includes the distribution of surficial deposits and sub-units of the Jezero delta at a higher level of detail than previous studies. This study considers four possible unit correlations to explain the relative age relationships of major units within the map area. Unit correlations include previously published interpretations as well as those that consider more complex interfingering relationships and alternative relative age relationships. The photogeologic map presented here is the foundation for scientific hypothesis development and strategic planning for Perseverance's exploration of Jezero crater.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: none
GenreCandidate signal: Other · Consensus signal: none
Teacher disagreement score0.088
Threshold uncertainty score0.174

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0060.001

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.013
GPT teacher head0.234
Teacher spread0.222 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designNot applicable
Domainnot available
GenreOther

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations130
Published2020
Admission routes1
Has abstractyes

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