Agata Magdalena Krzesinska

Carrier B., E. Sefton-Nash, H. Graham, C.D.K. Herd, J. Bridges, V. Debaille, A. Fox, K.L. French, T. Haltigin, E.M. Hausrath, A. Krzesińska, D. Paardekooper, E. Rampe, S. Schwenzer, M. Viotti, J. Duprat, M. Ferrari, M. Glamoclija, A.D. Harringon, A. Hutzler, Y. Liu, C. Magnabosco, J. Marlow, C. Maurel, H.M. McLaurin, R. Ogliore, A. Pack, S. Pillai, C. Schroeder, A. Sessions, S. Siljeström, A. Steele, B.L. Teece, V. Tu, and K. Wang, 2025: Mars Sample Return (MSR) Sample Receiving Project (SRP) Measurement Definition Team (MDT) Final Report. Astrobiology 10: 665-670.

Fawdon P., Orgel C., Adeli S., Balme M., Calef F., Davis J.M., Frigeri A., Grindrod P., Hauber E., Le Deit L., Loizeau D., Nass A., Quantin-Nataf C., Sefton-Nash E., Thomas N., Torres I., Vago J.L., Volat M., De Witte S., Altieri F., Apuzzo A., Aramendia J., Arana G., Bahia R., Banham S.G., Barnes R., Barrett A., Benedix W.-S., Bhardwaj A., Boazman S., Bontognali T.R.R., Bridges J., Bultel B., Ciarletti V., De Sanctis M.C., Dickeson Z., Favaro E., Ferrari M., Foucher F., Goetz W., Haldemann A., Harrington E., Kapatza A., Koschny D., Krzesińska A., Le Gall A., Lewis S., Lim T., Madariaga J., Mandon L., Mangold N., McNeil J., Molina A., Moral A.G., Motaghian S., Wright J., Nikiforov S., Oudart N., Pacifici A., Parkes Bowen A., Plettemeier D., Poulakis P., Rizky A., Putri D., Ruesch O., Sam L., Schröder C., Statz C., Thomas R., Tirsch D., Tóth Z., Turner S., Voelker M., Werner S., Westall F., Whiteside B., Williams A., Williams R., Zorzano M.-P., 2024: The high-resolution map of Oxia Planum, Mars; the landing site of the ExoMars Rosalind Franklin rover mission. Journal of Maps 20(1): 2302361.

Baker D.R., Callegaro S., Marzoli A., De Min A., Geraki K., Whitehouse M.J., Krzesińska A.M., Fioretti A.M., 2023. S and Cl in nakhlite clinopyroxenes: Source region concentrations and magmatic evolution. Geochimica et Cosmochimica Acta 359: 1-19.   

Tyminski Z., Hult M., Krzesińska A.M., Lutter G., Tyminska K, Saganowski P, Marissens G., Stroh H., Burakowska A., Ziemek T., Stachowicz M., El-Mallul A., 2023: Underground Radioactivity Measurements of Meteorites: Development of Development of Methods Suitable to Determine Precise Terrestrial Age of Recent Falls. Applied Radiation and Isotopes 195: 110733.

Krzesińska A., 2023: Petrology and chemistry of the Antonin meteorite – classification and reconstruction of thermal-collisional history (in Polish with English summary). Acta Societatits Metheoriticae Polonorum 14: 113-132.

Tymiński Z., Burakowska A., Krzesińska A.M., Tymińska K., Kuć M., Iller E, 2023: Cosmogenic radionuclides in Antonin meteorite (in Polish with English summary). Acta Societatis Metheoriticae Polonorum: 14: 191-198.

Shrbený L, Krzesińska A.M., Borovička J., Spurný P., Tymińnski Z., Kmieciak K., 2022: Analysis of the daylight fireball of July 15, 2021, leading to meteorite fall and find near Antonin, Poland, and description of the recovered chondrite. Meteoritics and Planetary Science 57: 2108-2126.

Loizeau D., Pilorget C., Poulet F., Lantz C., Bibring J.-P., Hamm V., Royer C., Dypvik H., Krzesińska A.M., Rull F., Werner S.C., 2022: Planetary Terrestrial Analogues Library Project: 3. Characterization of Samples With MicrOmega. Astrobiology 22: 263-292.

Krzesińska A.M., Bultel B., Loizeau D., Craw D., April R., Poulet F., Werner S.C., 2021: NIR characterization of Fe-rich vermiculite-bearing terrestrial deposits and constraints for mineralogy of Oxia Planum, ExoMars 2022 landing site. Astrobiology 21(8):997-1015. 

Dypvik H., Hellevang H., Krzesińska A., Sætre C., Viennet J-C., Bultel B., Ray D., Poulet D., Veneranda M., Rull F., Cousin A. Werner S.C., 2021. The Planetary Terrestrial Analogues Library (PTAL) - An Exclusive Lithological Selection of Possible Martian Earth Analogues. Planetary and Space Science 208: 105339. 

Veneranda M., Lopez-Reyes G., Pascual Sanchez E., Krzesińska AM, Lantz C., Manrique-Martinez JA, Sanz-Arranz A., Medina J., Poulet F., Dypvik H., Werner SC, Rull F ., 2021: ExoMars Raman Laser Spectrometer (RLS): a tool to semiquantify the serpentinization degree of olivine-rich rocks on Mars. Astrobiology.

Łuszczek K. and Krzesińska AM ., 2020: Copper in ordinary chondrites: Proxies for resource potential of asteroids and constraints for minimum-invasive and economically efficient exploitation. Planetary and Space Science. DOI: 10.1016 / j.pss.2020.105092

Veneranda M., Manrique JA., Lopez-Reyes G., Medina J., Torre-Fdez I., Castro K., Madariaga JM., Lantz C., Poulet F., Krzesińska AM ., Hellevang H., Werner S ., Rull F, 2019: Spectroscopic study of olivine-bearing rocks and its relevance to the ExoMars rover mission. Spectrochimica Acta A 223: 117360. doi.org/10.1016/j.saa.2019.117360

Krzesińska AM , Wirth R., Kusiak MA, 2019: Petrogenesis of ungrouped enstatite meteorite Zakłodzie: fabric, texture and nanostructure analysis for identification of mechanisms responsible for chondrite-achondrite transition. Meteoritics and Planetary Science 54: 1462-1477. DOI: 10.1111 / maps.13296.

Wilson AP, Genge MJ, Krzesińska AM ., Tomkins AG, 2019: Atmospheric Entry Heating of Micrometeorites at Earth and Mars: Implications for the Survival of Organics. Meteoritics and Planetary Science 54: 1-12. DOI: 10.1111 / maps.13360.

Krzesińska AM . & Almeida NV, 2019: Evidence of shock-induced vaporization of matrix to form porosity in Baszkówka, a porous L5 chondrite. Meteoritics and Planetary Science 54: 54–71. DOI: 10.1111 / maps.13190.

Krzesińska AM , 2018: Impact melt clasts in the Pułtusk breccia (in Polish with English summary). Acta Societatis Metheoriticae Polonorum 9: 74-92.

Krzesińska AM ., 2017: Contribution of early impact events to metal-silicate separation, thermal annealing and volatile redistribution: evidence in the Pułtusk H chondrite. Meteoritics and Planetary Science 52: 2305-2321. DOI: 10.1111 / maps.12933.

Gattacceca J., Krzesińska AM ., Marrocchi Y., Meier MMM, Bourot-Denise M., Lenssen R., 2017: Young asteroid mixing revealed in ordinary chondrites: the case of NWA 5764, a polymict LL breccia with L clasts. Meteoritics and Planetary Science 52: 2289-2304. DOI: 10.1111 / maps.12942.

Krzesińska AM ., 2016: Thermal Metamorphic Evolution of the Pułtusk H Chondrite Breccia - Compositional and Textural Properties not Included in Petrological Classification. Geological Quarterly, 60: 211–224. DOI: 10.7306 / gq.1267.

Krzesińska A. , Gattacceca J., Friedrich JM & Rochette P., 2015: Impact-related non-coaxial deformation in the Pułtusk H chondrite inferred from petrofabric analysis. Meteoritics and Planetary Science 50: 401–417. DOI: 10.1111 / maps.12429.

Krzesińska A. & Fritz J., 2014: Weakly shocked and deformed CM microxenoliths in the Pułtusk H chondrite. Meteoritics and Planetary Science 49: 595–610. DOI: 10.1111 / maps.12276.

Krzesińska A., 2011: High resolution X-ray tomography as a tool for analysis of internal textures in meteorites. Meteorites 1: 3–12. DOI: 10.5277 / met110101.

• Carrier, Brandi L.; Sefton-Nash, Elliot; Graham, Heather V.; Herd, Christopher D.K.; Bridges, John C. & Debaille, Vinciane [Show all 35 contributors for this article] (2025). Mars Sample Return Sample Receiving Project Measurement Definition Team Final Report. Astrobiology. ISSN 1531-1074. 25(10), p. 665–670. doi: 10.1177/15311074251382248. Full text in Research Archive
• Fawdon, Peter; Orgel, Csilla; Adeli, Solmaz; Balme, Matt; Calef, Fred J. & Davis, Joel M. [Show all 80 contributors for this article] (2024). The high-resolution map of Oxia Planum, Mars; the landing site of the ExoMars Rosalind Franklin rover mission. Journal of Maps. 20(1). doi: 10.1080/17445647.2024.2302361. Full text in Research Archive Show summary

  This 1:30,000 scale geological map describes Oxia Planum, Mars, the landing site for the ExoMars Rosalind Franklin rover mission. The map represents our current understanding of bedrock units and their relationships prior to Rosalind Franklin’s exploration of this location. The map details 15 bedrock units organised into 6 groups and 7 textural and surficial units. The bedrock units were identified using visible and near-infrared remote sensing datasets. The objectives of this map are (i) to identify where the most astrobiologically relevant rocks are likely to be found, (ii) to show where hypotheses about their geological context (within Oxia Planum and in the wider geological history of Mars) can be tested, (iii) to inform both the long-term (hundreds of metres to ∼1 km) and the short-term (tens of metres) activity planning for rover exploration, and (iv) to allow the samples analysed by the rover to be interpreted within their regional geological context.

• Krzesinska, Agata Magdalena; Tymiñski, Zbigniew & Maækowska, Roksana (2023). The Antonin Chondrite - the first Polish meteorite with reconstructed pre-atmospheric orbit. Report on registration and classification, including proposals for measures to expand the Polish meteorite collection. Przeglad Geologiczny. ISSN 0033-2151. 71(7), p. 372–385. doi: 10.7306/2023.33. Full text in Research Archive
• Baker, Don R.; Callegaro, Sara; Marzoli, Andrea; Min, Angelo De; Geraki, Kalotina & Whitehouse, Martin, J. [Show all 8 contributors for this article] (2023). Sulfur and chlorine in nakhlite clinopyroxenes: Source region concentrations and magmatic evolution. Geochimica et Cosmochimica Acta. ISSN 0016-7037. 359, p. 1–19. doi: 10.1016/j.gca.2023.08.007. Full text in Research Archive Show summary

  The volatile concentrations of the martian mantle and martian magmas remain important questions due to their role in petrogenesis and planetary habitability. The sulfur and chlorine concentrations, and their spatial distribution, in clinopyroxenes from nakhlites MIL 03346, Nakhla, and NWA 998 were measured to provide insight into these volatiles in the parental melts and source regions of nakhlites, and to constrain the evolution of the nakhlite melts. Sulfur and chlorine in four clinopyroxene crystals from MIL 03346, four from Nakhla, and five from NWA 998 were measured in crystal cores and rims by synchrotron X-ray fluorescence using beamline I18 at the Diamond Light Source. Portions of two crystals from MIL 03346 and one from Nakhla were mapped for S and Cl; a few reconnaissance analyses of Cl and F in MIL 03346 and Nakhla were made by ion microprobe. Clinopyroxene cores in Nakhla and NWA 998 contain ∼ 10 ppm S, ∼ 10 ppm Cl and ∼ 74 ppm F (only Nakhla analyzed), whereas the cores of MIL 03346 contain ∼ 10 ppm S, ∼ 5 ppm Cl and ∼ 53 ppm F. Using the volatile concentrations in the cores combined with previously determined partition coefficients we calculate that these clinopyroxenes crystallized from evolved basaltic melts containing ∼ 500 ppm S, ∼ 500 to 1900 ppm Cl, and 160 to 420 ppm F. These evolved melts can be used to calculate primitive melts in equilibrium with martian peridotite and the concentrations of S, Cl and F in the mantle source region of the nakhlite melts. Depending upon the extent of melting (5 to 30 %) necessary to produce the primary melts associated with nakhlites, our calculations indicate that the nakhlite source region has a S concentration between 20 (5 % melting) to 120 ppm (30 % melting), Cl between 16 to 97 ppm, and F between 14 to 48 ppm. These concentrations in the nakhlite magma source region are similar to previous estimates for the martian mantle; our calculated source region concentrations of F and Cl agree best with previous estimates if the martian mantle undergoes 10 to 20% melting to produce primary magmas that evolve to be parental to nakhlites. However, our maximum estimated sulfur concentration of the source (calculated for 30 % melting) is near previous minimum estimates for the martian mantle, suggesting the possibility that the nakhlite source region is depleted in sulfur relative to much of Mars’ mantle. Mapping the spatial distribution of volatiles in three clinopyroxene crystals demonstrates that S and Cl concentrations of the evolving melts changed significantly from the core to the rim, particularly those in MIL 03346. Increasing S and Cl concentrations between the core and rim of MIL 03346 crystals are attributed to incorporation of additional volatiles through assimilation, but the Nakhla crystal shows no such evidence. However, concentrations of Cl and S at some outer crystal rims of one MIL 03346 crystal decrease, most probably due to volatile degassing during the final stages of clinopyroxene growth.

• Tymiński, Zbigniew; Hult, Mikael; Krzesinska, Agata Magdalena; Tymińska, Katarzyna; Lutter, Guillaume & Saganowski, Paweł [Show all 12 contributors for this article] (2023). Underground radioactivity measurements of meteorites: Development of methods suitable to determine precise terrestrial age of recent falls. Applied Radiation and Isotopes. ISSN 0969-8043. 195. doi: 10.1016/j.apradiso.2023.110733. Full text in Research Archive
• Loizeau, Damien; Pilorget, Cédric; Poulet, François; Lantz, Cateline; Bibring, Jean-Pierre & Hamm, Vincent [Show all 11 contributors for this article] (2022). Planetary Terrestrial Analogues Library Project: 3. Characterization of Samples with MicrOmega. Astrobiology. ISSN 1531-1074. 22(3), p. 263–292. doi: 10.1089/ast.2020.2420. Full text in Research Archive
• Shrbený, Lukáš; Krzesinska, Agata Magdalena; Borovička, Jiří; Spurný, Pavel; Tymiński, Zbigniew & Kmieciak, Kryspin (2022). Analysis of the daylight fireball of July 15, 2021, leading to a meteorite fall and find near Antonin, Poland, and a description of the recovered chondrite. Meteoritics and Planetary Science. ISSN 1086-9379. 57(12), p. 2108–2126. doi: 10.1111/maps.13929. Full text in Research Archive Show summary

  We present the description of an observation of a fireball recorded during the sunrise on July 15, 2021. Atmospheric trajectory, impact area, and heliocentric orbit were determined on the basis of three instrumental video records. The terminal part of the fireball was not instrumentally recorded due to clouds. Based on our computations, one meteorite was found in the predicted impact area by Polish searchers. The specimen was, soon after recovery, analyzed for the presence of short-lived radionuclides and the measurement confirms a very fresh fall, coinciding with the time of the fireball event. The recovered meteorite, Antonin, is an unbrecciated L5 chondrite with shock stage S3, weathering grade W0, and bulk density of 3.42 g cm−3. Unusual for L chondrites, it contains assemblages composed of metal and two sulfides, troilite and mackinawite. We interpret these assemblages to have been formed as products of shock metamorphism and post-shock annealing on the parent body. This suggests that the thermal and collisional history of the Antonin parent body was complex.

• Veneranda, Marco; Lopez-Reyes, Guillermo; Sanchez, Elena Pascual; Krzesinska, Agata Magdalena; Manrique-Martinez, Jose Antonio & Sanz-Arranz, Aurelio [Show all 15 contributors for this article] (2021). ExoMars Raman Laser Spectrometer: A Tool to Semiquantify the Serpentinization Degree of Olivine-Rich Rocks on Mars. Astrobiology. ISSN 1531-1074. 21(3), p. 307–322. doi: 10.1089/ast.2020.2265. Full text in Research Archive
• Dypvik, Henning; Hellevang, Helge; Krzesinska, Agata Magdalena; Sætre, Christian; Viennet, Jean-Christophe & Bultel, Benjamin Gabriel Rene [Show all 13 contributors for this article] (2021). The Planetary Terrestrial Analogues Library (PTAL) – An exclusive lithological selection of possible martian earth analogues. Planetary and Space Science. ISSN 0032-0633. 208. doi: 10.1016/j.pss.2021.105339. Full text in Research Archive Show summary

  The Planetary Terrestrial Analogues Library (PTAL) is a dedicated lithological collection that currently consists of 102 terrestrial rock samples selected to be possible Mars analogues. The ultimate goal is improving future remote mineralogical and petrological analysis on Mars and other planetary bodies based on selected analysis such as Near- Infrared Reflectance Spectroscopy (NIR), Raman spectroscopy, Laser Induced Breakdown Spectroscopy (LIBS) and X-ray diffraction (XRD). Most international standards applied in the remote martian mineralogical and petrological analysis have so far been based on single, pure mineral analysis, with minimal interferences from other naturally occurring minerals. Here we present detailed lithological sample evaluations based on field appearance along with optical and XRD analysis of key terrestrial rock types. The detailed mineralogical and petrological descriptions give good basis for more complete lithological understanding. In combination with NIR, LIBS and Raman analysis of the very same samples PTAL aims at improving mineralogical and petrographical information from future rovers on Mars e.g. NASA's Mars2020-Perseverance and ESA and Roscosmos's ExoMars - Rosalind Franklin. The PTAL sample collection covers exclusively collected volcanic, magmatic and various sedimentary rocks and regoliths from well-known locations all over the world. These samples have a general composition comparable to what is currently known from Mars. The strength of this sample collection is its origin as common whole rock samples, in which minerals occur in their natural settings. It thereby allows studying possible detection interferences and a comparison of the sensitivity of the different techniques. The collection, in addition, forms the base for various alteration studies to better understand and explain alteration and weathering conditions on Mars. The complete results and sample preparations will be available to all scientists interested.

• Krzesinska, Agata Magdalena; Bultel, Benjamin Gabriel Rene; Loizeau, Damien; Craw, David; April, Richard & Poulet, Francois [Show all 7 contributors for this article] (2021). Mineralogical and spectral (NIR) characterization of Fe-rich vermiculite-bearing terrestrial deposits and constraints for mineralogy of Oxia Planum, ExoMars 2022 landing site. Astrobiology. ISSN 1531-1074. 21(8), p. 997–1016. doi: 10.1089/ast.2020.2410. Full text in Research Archive Show summary

  Oxia Planum is a Noachian plain on Mars. It was chosen as the final landing site for in situ studies by ExoMars 2022 rover. The main scientific objectives of the mission are to understand the mineralogy and aqueous evolution of ancient Mars with relevance to habitability. Oxia is covered by vast deposits of Fe,Mg-phyllosilicates, but the exact nature of these deposits is not yet fully understood. We performed a survey of potential terrestrial analog rocks, and here we show combined mineralogical characterization of these rocks with their near-infrared spectral analysis. Samples from two terrestrial sites were studied: (1) vermiculitized chlorite-schists from Otago, New Zealand, which underwent an alteration process without significant oxidation; and (2) basaltic tuffs from Granby, Massachusetts, USA, with Fe-rich clays filling amygdales of supposedly hydrothermal origin. Both analogues are incorporated into the newly built Planetary Terrestrial Analogue Library (PTAL) collection. Oxia bedrock clay-rich deposits are spectrally matched best by a well-crystallized trioctahedral vermiculite/saponite mixture from the basaltic tuff, although the contribution of saponite must be minor. Otago vermiculite is a good analogue to Oxia vermiculite in terms of overall mineralogy and Fe content. However, spectral inconsistencies related to the Al content in the Otago clays indicate that illitization of vermiculite, which results from postalteration oxidation, did not occur at Oxia. This implies limited water/rock interactions and reducing conditions during deposition of sediments now constituting the bedrock at Oxia. Whereas the spectral match does not conclusively imply the mineralogy, trioctahedral vermiculite should be considered a likely mineral component of the bedrock unit at Oxia Planum. Vermiculite has great potential to store organic matter, and the postdeposition geological context of Oxia Planum derived from understanding of environmental conditions in analog sites is promising for organic matter preservation.

• Luszczek, Katarzyna & Krzesinska, Agata Magdalena (2020). Copper in ordinary chondrites: Proxies for resource potential of asteroids and constraints for minimum-invasive and economically efficient exploitation. Planetary and Space Science. ISSN 0032-0633. 194. doi: 10.1016/j.pss.2020.105092. Full text in Research Archive Show summary

  Ordinary chondrites originate from S-type asteroids. These meteorites can be used for laboratory studies that further our understanding of the geological conditions on asteroids, including assessment of their resource potential. Asteroids have since long been considered to host significant resources of siderophilic elements such as Fe, Ni, Co, Cu, that could be exploited in situ. However bulk rock mining would be largely impractical. In this paper, we report on abundance and mineral occurrences of copper in H chondrites, identify Cu carrier minerals and interpret their distribution in the context of processes that must have affected parent bodies. This leads us to suggestion that some parts of S-type asteroids contain Cu in a form and amount that would satisfy requirements of potentially economically and environmentally more efficient exploitation. Parent bodies of chondrites contain 70–100 ​ppm of Cu in bulk and this is mainly contained in Fe,Ni-alloy. However, parts of asteroids that were affected by shock processes and post-shock thermal annealing may host Cu that exsolved from primary alloy and forms native, pure-Cu grains. Up to 50 ​ppm of Cu may be present in such phase in these parts of asteroids. Grains of native copper can be extracted from the host rock via mechanical mineral processing methods, releasing need of extensive chemical leaching. This makes potential exploitation more targeted and less destructive for the local environment. A characteristic feature associated with enrichment in native Cu in chondrites is presence of shock-darkened zones. Therefore, we suggest that shock-darkened asteroids are potentially best sites for Cu exploitation.

• Krzesinska, Agata Magdalena; Wirth, Richard & Kusiak, Monika A (2019). Petrogenesis of ungrouped enstatite meteorite Zaklodzie: Fabric, texture, and nanostructure analysis for identification of mechanisms responsible for chondrite?achondrite transition. Meteoritics and Planetary Science. ISSN 1086-9379. 54(7), p. 1462–1477. doi: 10.1111/maps.13296. Full text in Research Archive
• Wilson, Aaron; Genge, Matthew J; Krzesinska, Agata Magdalena & Tomkins, Andrew (2019). Atmospheric entry heating of micrometeorites at Earth and Mars: Implications for the survival of organics. Meteoritics and Planetary Science. ISSN 1086-9379. 54(9), p. 1–19. doi: 10.1111/maps.13360. Full text in Research Archive
• Veneranda, Marco; Manrique-Martinez, Jose Antonio; Lopez-Reyes, Guillermo; Medina, Jesus E.; Torre-Fdez, Imanol & Castro, Kepa [Show all 13 contributors for this article] (2019). Spectroscopic study of olivine-bearing rocks and its relevance to the ExoMars rover mission. Spectrochimica Acta Part A - Molecular and Biomolecular Spectroscopy. ISSN 1386-1425. 223. doi: 10.1016/j.saa.2019.117360. Full text in Research Archive

View all works in NVA

• Krzesinska, Agata Magdalena; Wirth, Richard & Schreiber, Anja (2026). Deciphering Metasomatic Alteration Conditions in H3.8 Chondrite Oslo from Silica-Ferroan Olivine Assemblages. Meteoritics and Planetary Science. ISSN 1086-9379. Full text in Research Archive
• Schroeder, Christian; Grindrod, Peter; Siljestrom, Sandra; Krzesinska, Agata Magdalena; Paar, Gerhard & Rudin, Mia [Show all 9 contributors for this article] (2025). Looking for Meteorites at Oxia Planum on Mars. Meteoritics and Planetary Science. ISSN 1086-9379. Full text in Research Archive
• Bultel, Benjamin Gabriel Rene; Krzesinska, Agata Magdalena; Loizeau, Damien; Veneranda, Marco & Werner, Stephanie C. (2025). Deciphering the alteration processes by micro-scale characterization of vermiculite-rich sample from Granby Tuff, an analogue to Noachian clay deposits at Oxia Planum. doi: 10.5194/epsc-dps2025-1550. Full text in Research Archive
• Thorpe, M. T.; Velbel, M. A.; Hauber, E.; Tait, K. T.; Thiessen, F. & Sefton-Nash, E. [Show all 12 contributors for this article] (2025). The Mars Sample Return Analogue Sample Library. doi: https:/www.hou.usra.edu/meetings/lpsc2025/pdf/2109.pdf. Full text in Research Archive
• Krzesinska, Agata Magdalena (2024). Prøver (som skal) returneres fra Mars og viktigheten av ‘esrtatningssteiner'. geoforskning.no. Full text in Research Archive
• Krzesinska, Agata Magdalena (2024). Krzesinska A.: Fluid-Assisted Alteration Record in Oslo H3.8-6 Chondrite. Meteoritics and Planetary Science. ISSN 1086-9379. Full text in Research Archive
• Krzesinska, Agata Magdalena (2024). Thiessen F., Krzesinska A., Orgel C., Sefton-Nash E., Hutzler A., Werner S., Griffiths L., Muller A.B., Kminek G., 2024: Mars Sample Return Analogue Sample Library. Full text in Research Archive
• Krzesinska, Agata Magdalena (2024). Bringing rocks from Mars to Earth; why, how and are we ready for it? Full text in Research Archive
• Krzesinska, Agata Magdalena (2024). Meteorites – the only rocky archive to decipher earliest evolution of the Earth. Full text in Research Archive
• Krzesinska, Agata Magdalena (2024). Bridges J. C., Debaille V., Harrington A. D., Herd C.D.K., Hutzler A., Krzesinska A. M., Liu Y., Maurel C., Wang K., 2024: Report of the Sample Receiving Project Measurement Definition Team: Igneous Samples Working Group. Full text in Research Archive
• Krzesinska, Agata Magdalena (2024). Krzesińska A.M., Tymiński Z., Allen N.M., Busemann H., Maden C., Stachowicz M., Kusiak M.A., Lee S., Yi K, 2024: Collisional history of L chondrite Antonin inferred from K-Ar, U,Th-He and phosphate U-Pb dating. Meteoritics and Planetary Science. ISSN 1086-9379. Full text in Research Archive
• Krzesinska, Agata Magdalena (2024). Krzesińska A.M., Tymiński Z., Allen N.M., Busemann H., Maden C., Stachowicz M., Kusiak M.A., Lee S., Yi K.: Collisional history of L chondrite Antonin inferred from K-Ar, U,Th-He and phosphate U-Pb dating. Full text in Research Archive
• Krzesinska, Agata Magdalena (2024). Fluid-Assisted Alteration Record in Oslo H3.8-6 Chondrite. Full text in Research Archive
• Krzesinska, Agata Magdalena (2024). Debaille V., Herd C. D. K., Duprat J., Krzesinska A. M., Maurel C., McLaurin H. M., Liu Y., Tu V. M., Wang K., 2024: Report of the Sample Receiving Project Measurement Definition Team: Chronology, Cratering, and Dynamics Working Group. Full text in Research Archive
• Krzesinska, Agata Magdalena (2024). Thiessen F., Krzesinska A., Orgel C., Sefton-Nash E., Hutzler A., Werner S., Griffiths L., Muller A.B., Kminek G., 2024: Mars Sample Return Analogue Sample Library. Meteoritics and Planetary Science. ISSN 1086-9379. Full text in Research Archive
• Krzesinska, Agata Magdalena (2024). Carrier B. L., Graham H. V., Herd C. D. K., Sefton-Nash E., Haltigin T., Paardekooper D. M., Viotti M. A., Krzesinska A. M., French K.L., Fox A. C., and the MDT-1 Team, 2024: Report of the Sample Receiving Project Measurement Definition Team: Deriving a Proposed Instrument Suite for the Sample Receiving Facility. Full text in Research Archive
• Harrington, Elise Michelle; Bultel, Benjamin; Krzesinska, Agata Magdalena & Werner, Stephanie C. (2020). Paleolakes and evaporite deposits across Mars. Full text in Research Archive

View all works in NVA