Microbial Activity and Neomorphism Influence the Composition and Microfabric of Ooids From Great Salt Lake, UT

By Tyler A. Lincoln, Samuel M. Webb & 3 more. Well-developed radial aragonite microfabrics and the ubiquitous occurrence of a Mg-silicate phase in Great Salt Lake ooids suggest influence of microbial activity and neomorphism.

Figure 13 from Comparative Sedimentology of Lake Bonneville and the Great Salt Lake

Variation of the parameters c 1 and c 2 and the perimeter S versus the

Microbial and diagenetic steps leading to the mineralisation of Great Salt Lake microbialites

Microbial and diagenetic steps leading to the mineralisation of Great Salt Lake microbialites

PDF) Microbial Activity and Neomorphism Influence the Composition and Microfabric of Ooids From Great Salt Lake, UT

Ooid Cortical Stratigraphy Reveals Common Histories of Individual Co‐occurring Sedimentary Grains

NanoSIMS (secondary ion mass spectrometry ) ion images distinguishing

Index Catalog // CU Scholar

Drought Negatively Impacting Great Salt Lake Microbialites and Ecosystem - Utah Geological Survey

Great Salt Lake microbiology: a historical perspective

Microbial and diagenetic steps leading to the mineralisation of Great Salt Lake microbialites

Theodore PRESENT, Associate Scientific Researcher, Ph.D., California Institute of Technology, CA, CIT, Division of Geological and Planetary Sciences

Ooids composed of coarse calcite spar without relics, interpreted as

Calcitic ooid composed of distinct radial-fibrous crystals showing

Index Catalog // CU Scholar