Excerpt from abstract of:
Paper No. 241-2
Presentation Time: 1:50 PM-2:10 PM
THE MINERALOGY OF THE MER LANDING SITES AS INVESTIGATED BY THE MINI-TES EXPERIMENT
CHRISTENSEN, Philip R., Geological Sciences, Arizona State Univ, Tempe, AZ 85287-6305, phil.christensen@asu.edu.
"...The spherical granules that are widespread on the plains are essentially pure hematite, with no silica, carbonates, sulfates, encased silicates, or other oxides detected."
The part about "encased silicates" etc, reveals that these are not concretions, which form in situ and enclose the grains of the host rock. The fine rock layers do not show deformation as if the spherules formed in situ by "swelling" and disrupting the host rock. Therefore, it seems most likely that they did not form in situ. Their very even spatial distribution, and narrow size distribution argue for a process of precipitation with distinct limits - be that seasonal concentration, current limited, biological or some other process.
Spherules are not concretions, as previously hypothesized
