Nature of siderite and phosphate in concretions from the upper Jurassic sediment of the Viatka-Kama basin (northeast of the Russian Plate)

Details Nature of siderite and phosphate in concretions from the upper Jurassic sediment of the Viatka-Kama basin (northeast of the Russian Plate) Nature of siderite and phosphate in concretions from the upper Jurassic sediment of the Viatka-Kama basin (northeast of the Russian Plate)

Jan 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003spie.4939..125v&link_type=abstract

Instruments, Methods, and Missions for Astrobiology VI. Edited by Hoover, Richard B.; Rozanov, Alexei Yu.; Lipps, Jere H. Pr

Biology

Scientific paper

Study of the inner structure, mineral, chemical and isotope composition of siderite and phosphate-siderite concretions from the upper Jurassic deposits of the Viatka-Kama basin has been made. A possible mechanism of their formation is discussed. A number of mineralogical and isotopic features indicate that the siderites and phosphates were formed at the diagenetic stage by the agency of both inorganic and microbial processes.

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