Skip to main content

Combination Ejecta

  • Reference work entry
  • First Online:
  • 9 Accesses

Definition

Impact crater ejecta pattern which displays a layered ejecta morphology close to the crater rim and secondary crater chains beyond the edge of the layered ejecta deposit.

Category

A type of ejecta, containing both layered ejecta and radial ejecta.

Synonyms

Diverse ejecta; MLERSRd; Radial-lobate ejecta; SLERSRd; Transitional ejecta

Description

The combination ejecta pattern displays components of both layered (fluidized) and radial (dry) ejecta patterns. There is a layered ejected blanket close to the crater rim, beyond which chains of secondary craters can be seen. The secondary craters appear to extend from beneath the outer edge of the layered ejecta deposit and thus appear to be formed prior to the emplacement of the layered ejecta deposit (Barlow et al. 2000). The layered ejecta part of the combination ejecta pattern is typically either a single layer ejecta or multiple layer ejecta morphology. Secondary craters extending beyond the outer layer of the double layer ejecta...

This is a preview of subscription content, log in via an institution.

Buying options

Chapter
USD   29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD   1,299.99
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Hardcover Book
USD   549.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Learn about institutional subscriptions

References

  • Abramov O, Kring DA (2005) Impact-induced hydrothermal activity on early Mars. J Geophys Res 110. doi:10.1029/2005JE002453

    Google Scholar 

  • Barlow NG (2005) A review of Martian impact crater ejecta structures and their implications for target properties. In: Kenkmann T, Hörz F, Deutsch A (eds) Large meteorite impacts III. Geological Society of America special paper 384. Geological Society of America, Boulder, pp 433–442

    Chapter  Google Scholar 

  • Barlow NG (2006) Martian impact craters and their implications for target characteristics. In: Proceedings of the first international conference on impact cratering in the solar system, European Space Agency Special Publication, Noordwijk, The Netherlands, SP-612

    Google Scholar 

  • Barlow NG, Bradley TL (1990) Martian impact craters: correlations of ejecta and interior morphologies with diameter, latitude, and terrain. Icarus 87:156–179

    Article  Google Scholar 

  • Barlow NG, Boyce JM, Costard FM, Craddock RA, Garvin JB, Sakimoto SEH, Kuzmin RO, Roddy DJ, Soderblom LA (2000) Standardizing the nomenclature of Martian impact crater ejecta morphologies. J Geophys Res 105:26,733–26,738

    Article  Google Scholar 

  • Beaty D, 26 colleagues of the MEPAG Special Regions–Science Analysis Group (2006) Findings of the Mars special regions science analysis group. Astrobiology 6:677–732

    Article  Google Scholar 

  • Boyce JM, Mouginis-Mark PJ (2006) Martian craters viewed by the thermal emission imaging system instrument: double-layered ejecta craters. J Geophys Res 111. doi:10.1029/2005JE002638

    Google Scholar 

  • Cockell CS, Barlow NG (2002) Impact excavation and the search for subsurface life on Mars. Icarus 155:340–349

    Article  Google Scholar 

  • Hartmann WK, Barlow NG (2006) Nature of the Martian uplands: effect on Martian meteorite age distribution and secondary cratering. Meteorit Planet Sci 41:1453–1467

    Article  Google Scholar 

  • McEwen AS, Preblich BS, Turtle EP, Artemieva NA, Golombek MP, Hurst M, Kirk RL, Burr DM, Christensen PR (2005) The rayed crater Zunil and interpretations of small impact craters on Mars. Icarus 176:351–381

    Article  Google Scholar 

  • Mouginis-Mark P (1979) Martian fluidized crater morphology: variations with crater size, latitude, altitude, and target material. J Geophys Res 84:8011–8022

    Article  Google Scholar 

  • Mouginis-Mark PJ, Boyce JM (2012) Tooting crater: geology and geomorphology of the archetytpe large, fresh, impact crater on Mars. Chemie der Erde 72:1–23

    Article  Google Scholar 

  • Preblich BS, McEwen AS, Studer DM (2007) Mapping rays and secondary craters from the Martian crater Zunil. J Geophys Res 112:E05006. doi:10.1029/2006JE002817

    Google Scholar 

  • Tornabene LL, Moersch JE, McSween HY, McEwen AS, Piatek JL, Milam KA, Christensen PR (2006) Identification of large (2–10 km) rayed craters on Mars in THEMIS thermal infrared images: implications for possible Martian meteorite source regions. J Geophys Res 111:E10006. doi:10.1029/2005JE002600

    Article  Google Scholar 

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Nadine G. Barlow .

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2015 Springer Science+Business Media New York

About this entry

Cite this entry

Barlow, N.G. (2015). Combination Ejecta. In: Hargitai, H., Kereszturi, Á. (eds) Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-3134-3_438

Download citation

Publish with us

Policies and ethics