Skip to main content

Thank you for visiting nature.com. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in Internet Explorer). In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript.

  • Article
  • Published:

Chandrayaan-3 APXS elemental abundance measurements at lunar high latitude

Abstract

The elemental composition of the lunar surface provides insights into mechanisms of the formation and evolution of the Moon1,2. The chemical composition of lunar regolith have so far been precisely measured using the samples collected by the Apollo, Luna and Chang’e 5 missions, which are from equatorial to mid-latitude regions3,4; lunar meteorites, whose location of origin on the Moon is unknown5,6; and the in situ measurement from the Chang’e 3 and Chang’e 4 missions7,8,9, which are from the mid-latitude regions of the Moon. Here we report the first in situ measurements of the elemental abundances in the lunar southern high-latitude regions by the Alpha Particle X-ray Spectrometer (APXS) experiment10 aboard the Pragyan rover of India’s Chandrayaan-3 mission. The 23 measurements in the vicinity of the Chandrayaan-3 landing site show that the local lunar terrain in this region is fairly uniform and primarily composed of ferroan anorthosite (FAN), a product of the lunar magma ocean (LMO) crystallization. However, observation of relatively higher magnesium abundance with respect to calcium in APXS measurements suggests the mixing of further mafic material. The compositional uniformity over a few tens of metres around the Chandrayaan-3 landing site provides an excellent ground truth for remote-sensing observations.

This is a preview of subscription content, access via your institution

Access options

Buy this article

USD 39.95

Prices may be subject to local taxes which are calculated during checkout

Fig. 1: Chandrayaan-3 landing site and APXS observation locations.
Fig. 2: APXS spectra and measured lunar elemental abundances.
Fig. 3: Compositional classification from APXS measurements.

Similar content being viewed by others

Data availability

APXS raw data and calibrated spectral files, along with the necessary calibration data for abundance estimation, will be available publicly at the Chandrayaan-3 portal of the ISRO Science Data Archive at https://pradan.issdc.gov.in/ch3/ from 23 August 2024. Chandrayaan-2 Orbiter High Resolution Camera (OHRC) data are available at https://pradan.issdc.gov.in/ch2/ (file id ch2_ohr_ncp_20211023T002746282). Data from the LRO WAC, Chandrayaan-1 M3, Kaguya TC and Clementine UVVIS instruments used in this publication are publicly available in the Planetary Data System (PDS) archives. Source data for Fig. 2 and Fig. 3 are provided with this paper.

Code availability

Spectral analysis carried out in this work uses the Xspec spectral fitting package (https://heasarc.gsfc.nasa.gov/xanadu/xspec/). Further analysis and plotting made use of the open-source Python packages numpy, scipy, matplotlib and pyrolite.

References

  1. Shearer, C. K. Thermal and magmatic evolution of the Moon. Rev. Mineral. Geochem. 60, 365–518 (2006).

    Article  CAS  Google Scholar 

  2. Lucey, P. Understanding the lunar surface and space-Moon interactions. Rev. Mineral. Geochem. 60, 83–219 (2006).

    Article  CAS  Google Scholar 

  3. Vaniman, D., Dietrich, J., Taylor, G. J. & Heiken, G. in Lunar Sourcebook, A User’s Guide to the Moon (eds Heiken, G. H., Vaniman, D. T. & French, B. M.) 5–26 (Cambridge Univ. Press, 1991).

  4. Qian, Y. et al. The regolith properties of the Chang’e-5 landing region and the ground drilling experiments using lunar regolith simulants. Icarus 337, 113508 (2020).

    Article  CAS  Google Scholar 

  5. Korotev, R. Lunar geochemistry as told by lunar meteorites. Geochemistry 65, 297–346 (2005).

    Article  CAS  Google Scholar 

  6. Joy, K. H. et al. Lunar meteorites. Rev. Mineral. Geochem. 89, 509–562 (2023).

    Article  Google Scholar 

  7. Ip, W.-H., Yan, J., Li, C.-L. & Ouyang, Z.-Y. Preface: The Chang’e-3 lander and rover mission to the Moon. Res. Astron. Astrophys. 14, 1511–1513 (2014).

    Article  ADS  Google Scholar 

  8. Wu, W. et al. Lunar farside to be explored by Chang’e-4. Nat. Geosci. 12, 222–223 (2019).

    Article  ADS  CAS  Google Scholar 

  9. Li, C. et al. Chang’E-4 initial spectroscopic identification of lunar far-side mantle-derived materials. Nature 569, 378–382 (2019).

    Article  ADS  CAS  PubMed  Google Scholar 

  10. Shanmugam, M. et al. Alpha particle X-ray spectrometer onboard Chandrayaan-2 rover. Curr. Sci. 118, 53 (2020).

    Article  ADS  Google Scholar 

  11. Meyer, H., Denevi, B., Robinson, M. & Boyd, A. The global distribution of lunar light plains from the lunar reconnaissance orbiter camera. J. Geophys. Res. Planets 125, e2019JE006073 (2020).

    Article  ADS  Google Scholar 

  12. Spudis, P. D., Reisse, R. A. & Gillis, J. J. Ancient multiring basins on the Moon revealed by Clementine laser altimetry. Science 266, 1848–1851 (1994).

    Article  ADS  CAS  PubMed  Google Scholar 

  13. Speyerer, E. J., Robinson, M. S., Boyd, A., Wagner, R. V. & Henriksen, M. R. Exploration of the lunar south pole with LROC data products. Lunar Surface Science Workshop, LPI Contribution No. 2241, id.5132 (2020).

  14. Sinha, R. K., Rani, A., Ruj, T. & Bhardwaj, A. Geologic investigation of lobate scarps in the vicinity of Chandrayaan-3 landing site in the southern high latitudes of the moon. Icarus 402, 115636 (2023).

    Article  CAS  Google Scholar 

  15. Durga Prasad, K. et al. Contextual characterization study of Chandrayaan-3 primary landing site. Mon. Not. R. Astron. Soc. 526, L116–L123 (2023).

    ADS  Google Scholar 

  16. Mithun, N. P. S. et al. Ground calibration of Alpha Particle X-ray Spectrometer (APXS) on-board Chandrayaan-2 Pragyaan rover: an empirical approach. Planet. Space Sci. 187, 104923 (2020).

    Article  CAS  Google Scholar 

  17. Korotev, R. L. Some things we can infer about the Moon from the composition of the Apollo 16 regolith. Meteorit. Planet. Sci. 32, 447–478 (1997).

    Article  ADS  CAS  Google Scholar 

  18. Laul, J. C. & Schmitt, E. A. Chemical composition of Luna 20 rocks and soil and Apollo 16 soils. Geochim. Cosmochim. Acta 37, 927–942 (1973).

    Article  ADS  CAS  Google Scholar 

  19. Radhakrishna, V. et al. Chandrayaan-2 large area soft X-ray spectrometer. Curr. Sci. 118, 219–225 (2020).

    Article  Google Scholar 

  20. Pieters, C. et al. The Moon Mineralogy Mapper (M3) on Chandrayaan-1. Curr. Sci. 96, 500–505 (2009).

    CAS  Google Scholar 

  21. Bansal, B. M. et al. The chemical composition of soil from the Apollo 16 and Luna 20 sites. Earth Planet. Sci. Lett. 17, 29–35 (1972).

    Article  ADS  CAS  Google Scholar 

  22. Wood, J. A., Dickey, J. S. Jr, Marvin, U. B. & Powell, B. N. Lunar anorthosites and a geophysical model of the moon. Geochim. Cosmochim. Acta Suppl. 1, 965 (1970).

    ADS  CAS  Google Scholar 

  23. Warren, P. H. The magma ocean concept and lunar evolution. Annu. Rev. Earth Planet. Sci. 13, 201–240 (1985).

    Article  ADS  CAS  Google Scholar 

  24. Wood, J. A. in Origin of the Moon (eds Hartmann, W. K., Phillips, R. J. & Taylor, G. J.) 17–55 (Lunar and Planetary Institute, 1986).

  25. Srivastava, Y., Basu Sarbadhikari, A., Day, J. M., Yamaguchi, A. & Takenouchi, A. A changing thermal regime revealed from shallow to deep basalt source melting in the Moon. Nat. Commun. 13, 7594 (2022).

    Article  ADS  CAS  PubMed  PubMed Central  Google Scholar 

  26. Ohtake, M. et al. The global distribution of pure anorthosite on the Moon. Nature 461, 236–240 (2009).

    Article  ADS  CAS  PubMed  Google Scholar 

  27. Donaldson Hanna, K. L. et al. Global assessment of pure crystalline plagioclase across the Moon and implications for the evolution of the primary crust. J. Geophys. Res. Planets 119, 1516–1545 (2014).

    Article  ADS  CAS  Google Scholar 

  28. Warren, P. H. Lunar anorthosites and the magma-ocean plagioclase-flotation hypotheses: importance of FeO enrichment in the parent magma. Am. Mineral. 75, 46–58 (1990).

    ADS  CAS  Google Scholar 

  29. Warren, P. H. A concise compilation of petrologic information on possibly pristine nonmare Moon rocks. Am. Mineral. 78, 360–376 (1993).

    ADS  CAS  Google Scholar 

  30. McCallum, I. S. A new view of the Moon in light of data from Clementine and Prospector missions. Earth Moon Planets 85, 253–269 (2001).

    ADS  Google Scholar 

  31. Cross, W., Iddings, J. P., Pirsson, L. V. & Washington, H. S. A quantitative chemico-mineralogical classification and nomenclature of igneous rocks. J. Geol. 10, 555–690 (1902).

    Article  ADS  CAS  Google Scholar 

  32. Verma, S. P., Torres-Alvarado, I. S. & Velasco-Tapia, F. A revised CIPW norm. Swiss Bull. Mineral. Petrol. 83, 197–216 (2003).

    CAS  Google Scholar 

  33. Warren, P. H. & Korotev, R. L. Ground truth constraints and remote sensing of lunar highland crust composition. Meteorit. Planet. Sci. 57, 527–557 (2022).

    Article  ADS  CAS  Google Scholar 

  34. Meyer, C. The lunar sample compendium. NASA https://curator.jsc.nasa.gov/Lunar/lsc/index.cfm (2012).

  35. Lemelin, M., Lucey, P. G. & Camon, A. Compositional maps of the lunar polar regions derived from the Kaguya Spectral Profiler and the Lunar Orbiter Laser Altimeter data. Planet. Sci. J. 3, 63 (2022).

    Article  Google Scholar 

  36. Wieczorek, M. A. & Zuber, M. T. The composition and origin of the lunar crust: constraints from central peaks and crustal thickness modeling. Geophys. Res. Lett. 28, 4023–4026 (2001).

    Article  ADS  Google Scholar 

  37. Wieczorek, M. A. The constitution and structure of the lunar interior. Rev. Mineral. Geochem. 60, 221–364 (2006).

    Article  CAS  Google Scholar 

  38. Dygert, N., Lin, J.-F., Marshall, E. W., Kono, Y. & Gardner, J. E. A low viscosity lunar magma ocean forms a stratified anorthitic flotation crust with mafic poor and rich units. Geophys. Res. Lett. 44, 11,282–11,291 (2017).

    Article  Google Scholar 

  39. Tompkins, S. & Pieters, C. M. Mineralogy of the lunar crust: results from Clementine. Meteorit. Planet. Sci. 34, 25–41 (1999).

    Article  ADS  CAS  Google Scholar 

  40. Stuart-Alexander, D. E. Geologic map of the central far side of the Moon. U.S. Geological Survey, IMAP 1047 (1978).

  41. Yamamoto, S. et al. Possible mantle origin of olivine around lunar impact basins detected by SELENE. Nat. Geosci. 3, 533–536 (2010).

    Article  ADS  CAS  Google Scholar 

  42. McGetchin, T. R., Settle, M. & Head, J. W. Radial thickness variation in impact crater ejecta: implications for lunar basin deposits. Earth Planet. Sci. Lett. 20, 226–236 (1973).

    Article  ADS  Google Scholar 

  43. Fassett, C. I., Head, J. W., Smith, D. E., Zuber, M. T. & Neumann, G. A. Thickness of proximal ejecta from the Orientale Basin from Lunar Orbiter Laser Altimeter (LOLA) data: implications for multi-ring basin formation. Geophys. Res. Lett. 38, L17201 (2011).

    Article  ADS  Google Scholar 

  44. Klima, R. L. et al. New insights into lunar petrology: distribution and composition of prominent low-Ca pyroxene exposures as observed by the Moon Mineralogy Mapper (M3). J. Geophys. Res. Planets 116, E00G06 (2011).

    Article  Google Scholar 

  45. Sinha, R. K. et al. Geological characterization of Chandrayaan-2 landing site in the southern high latitudes of the Moon. Icarus 337, 113449 (2020).

    Article  CAS  Google Scholar 

  46. Pike, R. J. Depth/diameter relations of fresh lunar craters: revision from spacecraft data. Geophys. Res. Lett. 1, 291–294 (1974).

    Article  ADS  Google Scholar 

  47. Ivanov, B. A. Size-frequency distribution of small lunar craters: widening with degradation and crater lifetime. Sol. Syst. Res. 52, 1–25 (2018).

    Article  ADS  Google Scholar 

  48. Borg, L. E., Connelly, J. N., Boyet, M. & Carlson, R. W. Chronological evidence that the Moon is either young or did not have a global magma ocean. Nature 477, 70–72 (2011).

    Article  ADS  CAS  PubMed  Google Scholar 

  49. Pernet-Fisher, J. F., Deloule, E. & Joy, K. H. Evidence of chemical heterogeneity within lunar anorthosite parental magmas. Geochim. Cosmochim. Acta 266, 109–130 (2019).

    Article  ADS  CAS  Google Scholar 

  50. Gross, J., Treiman, A. H. & Mercer, C. N. M. in Proc. 43rd Lunar and Planetary Science Conference 2306 (Lunar and Planetary Institute, 2012).

  51. Shirley, D. N. A partially molten magma ocean model. J. Geophys. Res. Solid Earth 88, A519–A527 (1983).

    Article  ADS  CAS  Google Scholar 

  52. Elardo, S. M., Laneuville, M., McCubbin, F. M. & Shearer, C. K. Early crust building enhanced on the Moon’s nearside by mantle melting-point depression. Nat. Geosci. 13, 339–343 (2020).

    Article  ADS  CAS  Google Scholar 

  53. Gross, J., Treiman, A. H. & Mercer, C. N. Lunar feldspathic meteorites: constraints on the geology of the lunar highlands, and the origin of the lunar crust. Earth Planet. Sci. Lett. 388, 318–328 (2014).

    Article  ADS  CAS  Google Scholar 

  54. Song, E., Bandfield, J. L., Lucey, P. G., Greenhagen, B. T. & Paige, D. A. Bulk mineralogy of lunar crater central peaks via thermal infrared spectra from the Diviner Lunar Radiometer: a study of the Moon’s crustal composition at depth. J. Geophys. Res. Planets 118, 689–707 (2013).

    Article  ADS  CAS  Google Scholar 

  55. Elkins-Tanton, L. T. Magma oceans in the inner solar system. Annu. Rev. Earth Planet. Sci. 40, 113–139 (2012).

    Article  ADS  CAS  Google Scholar 

  56. Chowdhury, A. R. et al. Orbiter high resolution camera onboard Chandrayaan-2 orbiter. Curr. Sci. 118, 560–565 (2020).

    Article  Google Scholar 

  57. Shearer, C. K., Elardo, S. M., Petro, N. E., Borg, L. E. & McCubbin, F. M. Origin of the lunar highlands Mg-suite: an integrated petrology, geochemistry, chronology, and remote sensing perspective. Am. Mineral. 100, 294–325 (2015).

    Article  ADS  Google Scholar 

  58. Arnaud, K. A., George, I. M. & Tennant, A. F. The OGIP spectral file format. https://heasarc.gsfc.nasa.gov/docs/heasarc/ofwg/docs/spectra/ogip_92_007.pdf (2021).

  59. Arnaud, K. A. in Astronomical Data Analysis Software and Systems V (eds Jacoby, G. H. & Barnes, J.) 17 (Astronomical Society of the Pacific, 1996).

  60. Arnaud, K., Dorman, B., Gordon, C. & Rutkowski, K. Xspec users’ guide. https://heasarc.gsfc.nasa.gov/xanadu/xspec/manual/manual.html (2024).

  61. Campbell, J. L. et al. Calibration of the Mars Science Laboratory alpha particle X-ray spectrometer. Space Sci. Rev. 170, 319–340 (2012).

    Article  ADS  CAS  Google Scholar 

  62. Narendranath, S. et al. Lunar elemental abundances as derived from Chandrayaan-2. Icarus 410, 115898 (2024).

    Article  CAS  Google Scholar 

  63. Bhatt, M., Wöhler, C., Grumpe, A., Hasebe, N. & Naito, M. Global mapping of lunar refractory elements: multivariate regression vs. machine learning. Astron. Astrophys. 627, A155 (2019).

    Article  ADS  CAS  Google Scholar 

  64. Pillai, N. S. et al. Chandrayaan-2 Large Area Soft X-ray Spectrometer (CLASS): calibration, in-flight performance and first results. Icarus 363, 114436 (2021).

    Article  CAS  Google Scholar 

  65. Taylor, S. R. et al. Composition of the Descartes region, lunar highlands. Geochim. Cosmochim. Acta 37, 2665–2683 (1973).

    Article  ADS  CAS  Google Scholar 

  66. Korotev, R. L. in Proc. 12th Lunar and Planetary Science Conference 577–605 (Pergamon Press, 1982).

  67. Laul, J. C. & Schmitt, R. A. in Proc. 4th Lunar and Planetary Science Conference 460 (Pergamon Press, 1973).

  68. Dowty, E., Keil, K. & Prinz, M. in The Apollo 15 Lunar Samples 62–66 (Lunar Science Institute, 1972).

  69. Haskin, L. A., Helmke, P. A., Blanchard, D. P., Jacobs, J. W. & Telander, K. in Proc. 4th Lunar and Planetary Science Conference 1275–1296 (Pergamon Press, 1973).

  70. Haskin, L. A. et al. in Proc. 5th Lunar and Planetary Science Conference 1213–1225 (Pergamon Press, 1974).

  71. Haskin, L. A. & Korotev, R. L. in Proc. 12th Lunar and Planetary Science Conference 404–405 (Pergamon Press, 1981).

  72. Laul, J. C. & Schmitt, R. A. in Proc. 6th Lunar and Planetary Science Conference 1231–1254 (Pergamon Press, 1975).

  73. Philpotts, J. A. et al. in Proc. 4th Lunar and Planetary Science Conference 1427 (Pergamon Press, 1973).

  74. Rhodes, J. M. & Hubbard, N. J. in Proc. 4th Lunar and Planetary Science Conference 1127 (Pergamon Press, 1973).

  75. Ridley, W. I., Hubbard, N. J., Rhodes, J. M., Weismann, H. & Bansal, B. The petrology of lunar breccia 15445 and petrogenetic implications. J. Geol. 81, 621–631 (1973).

    Article  ADS  CAS  Google Scholar 

  76. Rose, H. J. Jr et al. in Proc. 4th Lunar and Planetary Science Conference 1149 (Pergamon Press, 1973).

  77. Rose, H. J. Jr et al. in Proc. 6th Lunar and Planetary Science Conference 1363–1373 (Pergamon Press, 1975).

  78. Taylor, S. R. Chemical evidence for lunar melting and differentiation. Nature 245, 203–205 (1973).

    Article  ADS  CAS  Google Scholar 

  79. Taylor, S. R. et al. in Proc. 5th Lunar and Planetary Science Conference 789 (Pergamon Press, 1974).

  80. Wänke, H. et al. in Proc. 4th Lunar and Planetary Science Conference 1461 (Pergamon Press, 1973).

  81. Wänke, H. et al. in Proc. 6th Lunar and Planetary Science Conference 1313–1340 (Pergamon Press, 1975).

  82. Wänke, H. et al. in Proc. 7th Lunar and Planetary Science Conference 3479–3499 (Pergamon Press, 1976).

  83. Nava, D. F. in Proc. 5th Lunar and Planetary Science Conference 1087–1096 (Pergamon Press, 1974).

  84. Rhodes, J. M. et al. in Proc. 5th Lunar and Planetary Science Conference 1097–1117 (Pergamon Press, 1974).

  85. Winzer, S. R. et al. Major, minor and trace element abundances in samples from the Apollo 17 station 7 boulder: implications for the origin of early lunar crustal rocks. Earth Planet. Sci. Lett. 23, 439–444 (1974).

    Article  ADS  CAS  Google Scholar 

  86. Blanchard, D. P. et al. in Proc. 6th Lunar and Planetary Science Conference 2321–2341 (Pergamon Press, 1975).

  87. Dixon, J. R. & Papike, J. J. in Proc. 6th Lunar and Planetary Science Conference 263–291 (Pergamon Press, 1975).

  88. Dymek, R. F., Albee, A. L. & Chodos, A. A. in Proc. 6th Lunar and Planetary Science Conference 301–341 (Pergamon Press, 1975).

  89. Warner, J. L., Simonds, C. H. & Phinney, W. C. in Proc. 7th Lunar and Planetary Science Conference 915 (Pergamon Press, 1976).

  90. Lindstrom, M. M., Nielsen, R. L. & Drake, M. J. in Proc. 8th Lunar and Planetary Science Conference 2869–2888 (Pergamon Press, 1977).

  91. Lindstrom, M. M., Marvin, U. B., Vetter, S. K. & Shervais, J. W. in Proc. 18th Lunar and Planetary Science Conference 169–185 (Cambridge Univ. Press/Lunar and Planetary Institute, 1988).

  92. Murali, A. V., Ma, M. S., Laul, J. C. & Schmitt, R. A. in Proc. 8th Lunar and Planetary Science Conference 700 (Pergamon Press, 1977).

  93. Warren, P. H. & Wasson, J. T. in Proc. 8th Lunar and Planetary Science Conference 2215–2235 (Pergamon Press, 1977).

  94. Warren, P. H. & Wasson, J. T. in Proc. 9th Lunar and Planetary Science Conference 185–217 (Pergamon Press, 1978).

  95. Warren, P. H. & Wasson, J. T. in Proc. 10th Lunar and Planetary Science Conference 2051–2083 (Pergamon Press, 1979).

  96. Stöeffler, D., Knoell, H. D., Marvin, U. B., Simonds, C. H. & Warren, P. H. in Proc. Conf. Lunar Highlands Crust (eds Merrill, R. B. & Papike, J. J.) 51–70 (Pergamon Press, 1980).

  97. James, O. B. & McGee, J. J. in Proc. 10th Lunar and Planetary Science Conference 713–743 (Pergamon Press, 1979).

  98. Marvin, U. B. & Warren, P. H. in Proc. 11th Lunar and Planetary Science Conference 507–521 (Pergamon Press, 1980).

  99. Ryder, G., Norman, M. D. & Score, R. A. in Proc. 11th Lunar and Planetary Science Conference 471–479 (Pergamon Press, 1980).

  100. Taylor, G. J., Warner, R. D., Keil, K., Ma, M. S. & Schmitt, R. A. in Proc. Conf. Lunar Highlands Crust (eds Merrill, R. B. & Papike, J. J.) 339–352 (Pergamon Press, 1980).

  101. Blanchard, D. P. & McKay, G. A. in Proc. 12th Lunar and Planetary Science Conference 83–85 (Pergamon Press, 1981).

  102. Simonds, C. H. & Warner, J. L. in Proc. 12th Lunar and Planetary Science Conference 993–995 (Pergamon Press, 1981).

  103. Warren, P. H., Taylor, G. J., Keil, K., Marshall, C. & Wasson, J. T. in Proc. 12th Lunar and Planetary Science Conference 1154–1156 (Pergamon Press, 1981).

  104. Warren, P. H., Taylor, G. J., Keil, K., Marshall, C. & Wasson, J. T. in Proc. 12th Lunar and Planetary Science Conference 21–40 (Pergamon Press, 1982).

  105. Warren, P. H., Taylor, G. J., Keil, K., Shirley, D. N. & Wasson, J. T. Petrology and chemistry of two “large” granite clasts from the moon. Earth Planet. Sci. Lett. 64, 175–185 (1983).

    Article  ADS  CAS  Google Scholar 

  106. Warren, P. H. et al. Seventh Foray: Whitlockite-rich lithologies, a diopside-bearing troctolitic anorthosite, ferroan anorthosites, and KREEP. J. Geophys. Res. Solid Earth 88, B151–B164 (1983).

    Article  ADS  Google Scholar 

  107. Warren, P. H., Shirley, D. N. & Kallemeyn, G. W. A potpourri of pristine Moon rocks, including a VHK mare basalt and a unique, augite-rich Apollo 17 anorthosite. J. Geophys. Res. Solid Earth 91, 319–330 (1986).

    Article  Google Scholar 

  108. Warren, P. H., Jerde, E. A. & Morris, R. V. in Proc. 18th Lunar and Planetary Science Conference 1060, (Cambridge Univ. Press, 1987).

  109. Warren, P. H., Jerde, E. A. & Kallemeyn, G. W. in Proc. 20th Lunar and Planetary Science Conference 31–59 (Lunar and Planetary Institute, 1990).

  110. Warren, P. H., Jerde, E. A. & Kallemeyn, G. W. in Proc. 21st Lunar and Planetary Science Conference 51–61 (Lunar and Planetary Institute, 1991).

  111. Hunter, R. H. & Taylor, L. A. The magma ocean from the Fra Mauro shoreline: an overview of the Apollo 14 crust. J. Geophys. Res. Solid Earth 88, A591–A602 (1983).

    Article  ADS  CAS  Google Scholar 

  112. James, O. B. & Flohr, M. K. Subdivision of the Mg-suite noritic rocks into Mg-gabbronorites and Mg-norites. J. Geophys. Res. Solid Earth 88, A603–A614 (1983).

    Article  ADS  CAS  Google Scholar 

  113. Marti, K. et al. Pieces of the ancient lunar crust: ages and composition of clasts in consortium breccia 67915. J Geophys. Res. Solid Earth 88, B165–B175 (1983).

    Article  ADS  Google Scholar 

  114. Nord, G. L. Jr & Wandless, M. V. Petrology and comparative thermal and mechanical histories of clasts in breccia 62236. J. Geophys. Res. Solid Earth 88, A645–A657 (1983).

    Article  ADS  CAS  Google Scholar 

  115. Shervais, J. W., Taylor, L. A. & Laul, J. C. Ancient crustal components in the Fra Mauro breccias. J. Geophys. Res. Solid Earth 88, B177–B192 (1983).

    Article  ADS  Google Scholar 

  116. Shervais, J. W., Taylor, L. A., Laul, J. C. & Smith, M. R. Pristine highland clasts in consortium breccia 14305: petrology and geochemistry. J. Geophys. Res. Solid Earth 89, C25–C40 (1984).

    Article  ADS  CAS  Google Scholar 

  117. Ryder, G. in Workshop on the Geology of the Apollo 15 Landing Site (eds Spudis, P. D. & Ryder, G.) 41–45 (Lunar and Planetary Institute, 1985).

  118. Laul, J. C. Chemistry of the Apollo 12 highland component. J. Geophys. Res. Solid Earth 91, 241–261 (1986).

    Article  Google Scholar 

  119. James, O. B., Lindstrom, M. M. & Flohr, M. K. Petrology and geochemistry of alkali gabbronorites from lunar breccia 67975. J. Geophys. Res. Solid Earth 92, E314–E330 (1987).

    Article  ADS  CAS  Google Scholar 

  120. James, O. B., Lindstrom, M. M. & Flohr, M. K. in Proc. 19th Lunar and Planetary Science Conference 219–243 (Cambridge Univ. Press/Lunar and Planetary Institute, 1989).

  121. Marvin, U. B., Lindstrom, M. M., Bernatowicz, T. J., Podosek, F. A. & Sugiura, N. The composition and history of breccia 67015 from North Ray Crater. J. Geophys. Res. Solid Earth 92, E471–E490 (1987).

    Article  ADS  CAS  Google Scholar 

  122. Simon, S. B., Papike, J. J., Laul, J. C., Hughes, S. S. & Schmitt, R. A. Apollo 16 regolith breccias and soils: recorders of exotic component addition to the Descartes region of the moon. Earth Planet. Sci. Lett. 89, 147–162 (1988).

    Article  ADS  CAS  Google Scholar 

  123. Ryder, G. & Sherman, S. B. The Apollo 15 coarse fines (4–10 mm). NASA Technical Memorandum 19900005711 (1989).

  124. Lindstrom, M. M., Marvin, U. B. & Mittlefehldt, D. W. in Proc. 19th Lunar and Planetary Science Conference 245–254 (Cambridge Univ. Press/Lunar and Planetary Institute, 1989).

  125. Jolliff, B. L., Korotev, R. L. & Haskin, L. A. in Proc. 21st Lunar and Planetary Science Conference 193–219 (Lunar and Planetary Institute, 1991).

  126. Norman, M. D. & Taylor, S. R. Geochemistry of lunar crustal rocks from breccia 67016 and the composition of the Moon. Geochim. Cosmochim. Acta 56, 1013–1024 (1992).

    Article  ADS  CAS  Google Scholar 

  127. Snyder, G. A., Taylor, L. A., Liu, Y. G. & Schmitt, R. A. in Proc. 22nd Lunar and Planetary Science Conference 399–416 (Lunar and Planetary Institute, 1992).

  128. Shih, C. Y. et al. Ages of pristine noritic clasts from lunar breccias 15445 and 15455. Geochim. Cosmochim. Acta 57, 915–931 (1993).

    Article  ADS  CAS  Google Scholar 

  129. Jolliff, B. L. & Haskin, L. A. Cogenetic rock fragments from a lunar soil: evidence of a ferroan noritic-anorthosite pluton on the Moon. Geochim. Cosmochim. Acta 59, 2345–2374 (1995).

    Article  ADS  CAS  Google Scholar 

  130. Norman, M. D., Keil, K., Griffin, W. L. & Ryan, C. G. Fragments of ancient lunar crust: petrology and geochemistry of ferroan noritic anorthosites from the Descartes region of the Moon. Geochim. Cosmochim. Acta 59, 831–847 (1995).

    Article  ADS  CAS  Google Scholar 

  131. Norman, M. D., Borg, L. E., Nyquist, L. E. & Bogard, D. D. Chronology, geochemistry, and petrology of a ferroan noritic anorthosite clast from Descartes breccia 67215: clues to the age, origin, structure, and impact history of the lunar crust. Meteorit. Planet. Sci. 38, 645–661 (2003).

    Article  ADS  CAS  Google Scholar 

  132. Hansen, E. C., Smith, J. V. & Steele, I. M. in Proc. 11th Lunar and Planetary Science Conference 523–533 (Pergamon Press, 1980).

  133. Hollocher, K. NORM4 Excel spreadsheet programs to calculate petrologic norms from whole-rock chemical analyses. Zenodo https://doi.org/10.5281/zenodo.5818037 (2022).

  134. Lucey, P. G., Blewett, D. T., Taylor, G. J. & Hawke, B. R. Imaging of lunar surface maturity. J. Geophys. Res. Planets 105, 20377–20386 (2000).

    Article  ADS  CAS  Google Scholar 

  135. McEwen, A. S. in Proc. 27th Lunar and Planetary Science Conference 841 (Lunar and Planetary Institute, 1996).

  136. Pieters, C. M. in Proc. Workshop on New Views of the Moon II: Understanding the Moon Through the Integration of Diverse Datasets 8025 (Lunar and Planetary Institute, 1999).

Download references

Acknowledgements

The APXS experiment is designed and developed by the Physical Research Laboratory (PRL), Ahmedabad, supported by the Department of Space, Government of India. The Space Applications Centre (SAC), Ahmedabad, supported the fabrication and space qualification of the APXS flight model. We acknowledge the extensive support from the entire Chandrayaan-3 team, consisting of large groups from U R Rao Satellite Centre (URSC), Bangalore; Vikram Sarabhai Space Center (VSSC), Thiruvananthapuram; ISRO Telemetry, Tracking and Command Network (ISTRAC), Bangalore; Satish Dhawan Space Centre (SDSC), Sriharikota, as well as other ISRO centres. We specifically acknowledge the efforts of various teams involved in the operations of the Chandrayaan-3 Pragyan rover. We acknowledge the use of images from Chandrayaan-3 rover NavCam developed by the Laboratory for Electro-Optics Systems (LEOS) and processed by the SAC and the use of the image from the Orbiter High Resolution Camera (OHRC) aboard the Chandrayaan-2 orbiter provided by the SAC data processing team and archived at the Indian Space Science Data Center (ISSDC). We also acknowledge the use of data from the Chandrayaan-1 M3, LRO WAC, Kaguya TC and Clementine UVVIS instruments. A.B. was J.C. Bose Fellow during this work.

Author information

Authors and Affiliations

Authors

Contributions

S.V.V., M.S., Y.B.A. and S.V.S.M. designed the experiment. M.S., A.R.P., H.L.A., T.L., S.K.G. and N.K.T. developed the APXS instrument. N.P.S.M., N.Si., S.K. and D.K.P. conducted the calibration experiments. A.K.H., A.P., A.K., N.Sa., V.R.S., S.G.N., R.G.V. and L.A. contributed to the mechanical, thermal and mechanism design and integration with the rover. K.S. and Am. provided the rover NavCam and Orbiter High Resolution Camera (OHRC) images. N.P.S.M., C.S.V. and B.S.B.S. carried out data processing. S.V.V. and N.P.S.M. performed the APXS data analysis. A.B.S. and Y.S. carried out the lithological and geochemical analysis. R.K.S., M.B., S.V. and N.Sr. carried out the remote-sensing analysis. A.D.S., A.B.S., Y.S. and V.M.N. carried out laboratory XRF measurements. S.N. and N.S.P. provided remote-sensing XRF data. S.V.V., N.P.S.M., A.B.S., R.K.S., M.B., S.V., N.Sr. and A.B. contributed to the interpretation and preparation of the manuscript.

Corresponding author

Correspondence to Santosh V. Vadawale.

Ethics declarations

Competing interests

The authors declare no competing interests.

Peer review

Peer review information

Nature thanks Paul Warren and the other, anonymous, reviewer(s) for their contribution to the peer review of this work. Peer reviewer reports are available.

Additional information

Publisher’s note Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Extended data figures and tables

Extended Data Fig. 1 Maps of elemental abundances derived from M3.

Elemental abundance maps derived from M3 observations around the landing site (1° × 1°) are shown for Mg (a), Fe (b) and Ca (c). The blue square represents the landing site. Typical uncertainties in abundances are 1 wt% and the colour scale spans about 2σ around the value at the landing site. This shows that there is no variation in abundance over this spatial scale.

Extended Data Fig. 2 Reflectance spectrum of the landing site region.

a, M3 albedo map at 1,578 nm around the Chandrayaan-3 landing site. This 1° × 1° subset was extracted from M3 product ID M3G20090606T010302. The spatial resolution of the M3 strip used here is 280 m pixel−1. The blue dot in the centre shows the landing site. b, Extracted M3 spectrum from the pixel containing the Chandrayaan-3 landing site (marked by the blue dot in panel a). This reflectance spectrum represents a highland-type soil spectrum with no notable absorption feature at 1 and 2 μm.

Extended Data Fig. 3 Source of the material at the landing site.

a, Kaguya TC orthoimage showing the region around the landing site (marked by the solid yellow circle). The chains and clusters of secondaries (classes 1 and 2) are marked in the figure. Solid white lines represent the boundary of the ‘Ntp’ geological unit (intercrater plains region). b, False-colour composite image of band ratios from Clementine UVVIS134. The colours correspond to band ratios of 750 nm/415 nm (red), 750 nm/950 nm (green) and 415 nm/750 nm (blue). In the figure, mature lunar highlands appear in shades of red and the bright blue shades represent rays of a young crater135,136. Arrows mark the ejecta rays from the Schomberger crater extending towards the landing site.

Extended Data Fig. 4 APXS spectrum fitted with the model showing different components.

APXS spectrum (blue data points) from observation ID 18 fitted with the model consisting of continuum component (dashed black line) and lines of different elements. Dashed lines of different colours denote the line components corresponding to the elements marked with the same colour.

Extended Data Fig. 5 Distance dependence of line intensity and distance estimation from continuum rate.

a, Slope of the line intensity–abundance correlation, which is wt% per unit photons per second, of different elements as a function of the sample distance. Data points are the slope values; the solid lines show the power laws that fit them. b, Continuum rates (sum of count rates in 22.4–24.2-keV energy range) obtained for different geochemical reference materials are shown as a function of distance with the red data points and the black line shows the best-fit model. The continuum rate from lunar observation for observation ID 18, along with its error, is plotted on the curve to estimate the respective distance. The blue-shaded regions show uncertainties in the continuum rate and corresponding uncertainty in distance estimates. Uncertainties in the estimated distance are then propagated to abundance measurements through correlation parameters.

Extended Data Fig. 6 Abundance measurement from correlations.

An example of abundance measurement of the lunar sample (observation ID 15) from correlations obtained from ground calibration is shown. Dashed lines and faint points are correlations from USGS samples shown in Supplementary Figs. 2 and 3. Vertical grey shades show the measured line intensity with error from the lunar observation. Three solid lines show the correlation for the measured distance (orange) and at one standard deviation of the distance (blue and green). Matrix-corrected flux values are plotted on these correlations to obtain the abundances (error bars with respective colours). Measured abundance is shown with the red star symbols and associated uncertainties, including the distance uncertainties, are also shown.

Extended Data Fig. 7 Coadded spectrum from all observations.

APXS spectrum obtained by adding data from all 23 scientific observations amounting to a total exposure of 31.34 h. An extra line of zinc (Kα) is detected in the coadded spectrum.

Extended Data Table 1 Elemental abundances from individual APXS observations
Extended Data Table 2 Comparison of APXS abundances with other measurements
Extended Data Table 3 Normative mineralogy based on APXS-measured abundances for each observation

Supplementary information

Supplementary Information (download PDF )

The Supplementary Information file includes a supplementary section on calibration, Supplementary Figs. 1–4 and Supplementary Tables 1–5.

Peer Review File (download PDF )

Source data

Rights and permissions

Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Vadawale, S.V., Mithun, N.P.S., Shanmugam, M. et al. Chandrayaan-3 APXS elemental abundance measurements at lunar high latitude. Nature 633, 327–331 (2024). https://doi.org/10.1038/s41586-024-07870-7

Download citation

  • Received:

  • Accepted:

  • Published:

  • Version of record:

  • Issue date:

  • DOI: https://doi.org/10.1038/s41586-024-07870-7

This article is cited by

Comments

Commenting on this article is now closed.

  1. slot kubet dengan jam pola gacor pasti wd

Search

Quick links

Nature Briefing

Sign up for the Nature Briefing newsletter — what matters in science, free to your inbox daily.

Get the most important science stories of the day, free in your inbox. Sign up for Nature Briefing