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Evidence for an 800 km Diameter Impact Structure in Meridiani Planum and Associated Channels and Basins: A Connection with the Origin of the Hematite Deposits?Topographic evidence for the existence of an early 800 km diameter multi-ringed impact structure, and evidence for fluvial and lacustrine environments in Meridiani Planum suggests a connection with the origin of the hematite deposits present in the region.
Document ID
20030111578
Acquisition Source
Headquarters
Document Type
Conference Paper
Authors
Newsom, H. E. (New Mexico Univ. Albuquerque, NM, United States)
Barber, C. A. (New Mexico Univ. Albuquerque, NM, United States)
Schelble, R. T. (University of Southern California Los Angeles, CA, United States)
Hare, T. M. (Geological Survey Flagstaff, AZ, United States)
Feldman, W. C. (Los Alamos National Lab. NM, United States)
Sutherland, V. (New Mexico Univ. Albuquerque, NM, United States)
Gordon, H. (New Mexico Univ. Albuquerque, NM, United States)
Thorsos, I. E. (New Mexico Univ. Albuquerque, NM, United States)
Livingston, A. (Southwestern Indian Polytechnic Inst. Albuquerque, NM, United States)
Lewis, K. (Southwestern Indian Polytechnic Inst. Albuquerque, NM, United States)
Date Acquired
August 21, 2013
Publication Date
January 1, 2003
Publication Information
Publication: Lunar and Planetary Science XXXIV
Subject Category
Lunar And Planetary Science And Exploration
Funding Number(s)
CONTRACT_GRANT: NAG5-8804
CONTRACT_GRANT: NAG5-10143
CONTRACT_GRANT: NAG5-11496
Distribution Limits
Public
Copyright
Public Use Permitted.
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IDRelationTitle20030110578Collected WorksLunar and Planetary Science XXXIV20030110578Collected WorksLunar and Planetary Science XXXIV
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