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Application of Chemostratigraphy in Clastic, Carbonate and Unconventional Reservoirs
2018Chemostratigraphy is most commonly applied to clastic sediments, particularly where biostratigraphic control is lacking. An example of such a study is in the Berkine Basin, Algeria, where it was almost impossible to use lithostratigraphy and sedimentology alone to correlate the Triassic TAGI Formation.
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Chemostratigraphy: A New Tool for the Correlation of Ancient Sequences
AAPG Bulletin, 1993Chemostratigraphy involves the application of major and trace-element geochemistry to the characterization and correlation of strata in petroleum basins, particularly where biostratigraphic control is poor. The geochemistry of sediments is highly variable and sensitive to subtle changes in composition and uniform succession may show primary differences
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