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by
Pederson, Chelsea L., author.
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Deposition and Diagenesis of Subtropical Microbial Carbonates / Pederson, Chelsea L., author.
by
Al-Fahmi, Mohammed M., author.
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Controls on fracture abundance in gently deformed carbonates / Al-Fahmi, Mohammed M., author.
by
Mitnick, Elizabeth H., author.
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-Synthesized Carbonates / Mitnick, Elizabeth H., author.
by
Root, Jonathan Casey, author. (orcid)0000-0003-0537-4418
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Petrological and Isotopic Evidence for Diagenetic Evolution in the Cherry Valley Carbonates and
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Zhelezinskaia, Iadviga, author. (orcid)0000-0002-7677-0488
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Sulfur Isotope Records in Neoarchean Carbonates: Implications for the Precambrian Sulfur Cycle /
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Winhusen, Eric R., author.
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Precambrian Seawater Temperature Analysis Using Oxygen Isotopes from Hamersley Carbonates, Western
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Hadi, Farqad Ali, author.
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-petrophysical properties of carbonates was conducted from previous studies. Data from offset well have also been used to
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Hill, Ethan D., author.
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heterogeneity commonly occurs within carbonates and has been illustrated within the Mississippian Subsystem of
by
Shen, Ruiqing, author.
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Flame retardant additives, such as phosphorus-based fillers, metal hydroxides, metal carbonates
by
Gordon, Andrew, author.
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sandstones and shallow lake carbonates which are encased in non-reservoir mudstones and shales that act as
by
Friday, Mattie E., author.
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lacustrine carbonates and mixed bulk organic samples, pollen is terrestrial and is not directly influenced by
by
Schuller, Kathryn M., author.
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nodular carbonates are mud- to wackestones, contain lenses of fossil fragments, and often form continuous
by
Turpin, DeeAnn-Rose G., author.
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process on the fate of inorganic carbon (especially carbonates), phosphate, sulfides, and volatile fatty
by
Turner, Sarah, author.
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resulting in the precipitation of authigenic carbonates and iron sulfides. One method to identify paleo
by
Nair, Kajal, author.
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carbonates. The superimposed curve shows an overall transgression in the lower part of the succession
by
Elhamali, Emhemed I. E., author.
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understanding the depositional environment of the carbonates. The formation may be divided into six informal
by
Cornah, Sarah J., author.
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of the carbonates and phyllosilicates. These trends were correlatable with the general stratigraphic
by
Ferroud, Anouck, author.
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differents tels que des socles rocheux granitiques, des milieux carbonates (peu ou tres fractures), des

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