期刊
METEORITICS & PLANETARY SCIENCE
卷 35, 期 3, 页码 457-465出版社
WILEY-BLACKWELL
DOI: 10.1111/j.1945-5100.2000.tb01428.x
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Spherical carbonate globules of similar composition, size, and radial Ca-, Mg-, and Fe-zonation to those in martian meteorite Allan Hills (ALH) 84001 were precipitated from Mg-rich, supersaturated solutions of Ca-Mg-Fe-CO(2)-H(2)O at 150 OC. The supersaturated solutions (pH congruent to 6-7) were prepared at room temperature and contained in Teflon(TM)-lined stainless steel vessels, which were sealed and heated to 150 degrees C for 24 h. Experiments were also conducted at 25 degrees C and no globules comparable to those of ALH 84001 were precipitated. Instead, amorphous Fe-rich carbonates were formed after 24 h and Mg-Fe calcites formed after 96 h. These experiments suggest a possible low-temperature inorganic origin for the carbonates in martian meteorite ALH 84001.
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