Paleomagnetic Studies of Returned Samples from MarsThe red planet is a magnetic planet. Mars' iron-rich surface is strongly magnetized, likely dating back to the Noachian epoch when the surface may have been habitable. Paleomagnetic measurements of returned samples could transform our understanding of the Martian dynamo and its connection to climatic and planetary thermal evolution and provide powerful constraints on the preservation state of biosignatures in the samples.
Document ID
20180003302
Acquisition Source
Johnson Space Center
Document Type
Conference Paper
Authors
Weiss, B. P. (Massachusetts Inst. of Technology (MIT) Cambridge, MA, United States)
Date Acquired
June 4, 2018
Publication Date
April 25, 2018
Subject Category
Lunar And Planetary Science And Exploration
Report/Patent Number
JSC-E-DAA-TN53716Report Number: JSC-E-DAA-TN53716
Meeting Information
Meeting: International Mars Sample Return Conference