Characterization of organic matter from the Cretaceous sedimentary and . . . Mudstone samples, representing marine and non-marine strata from the western (Byers Peninsula) and central south part (Hannah Point) of Livingston Island, West Antarctica, are characterized using petrological and organic geochemical methods
Microscopic and Fractal Characterization of Organic Matter within . . . Lacustrine organic-rich shale samples from the first member of the Cretaceous Qingshankou Formation in the Songliao Basin were analyzed with confocal laser scanning microscopy (CLSM) and fluorescence spectral analysis The results show that the occurrences of different organic components are related to the fabric of samples and vary with depth
Paleoenvironment and Organic Characterization of the Lower Cretaceous . . . The variability in sedimentary environments, sources of organic matter of the source rocks in different sags, and the influence of hydrothermal and volcanic activity on the source rock quality in the Erlian Basin were assessed The results reveal that the source rocks can be divided into four types of organic facies (A, B, BC, and C)
Characterization of organic matter from the Cretaceous sedimentary and . . . Mudstone samples, representing marine and non-marine strata from the western (Byers Peninsula) and central south part (Hannah Point) of Livingston Island, West Antarctica, are characterized using petrological and organic geochemical methods
Characterization of organic matter from the Cretaceous sedimentary and . . . Semantic Scholar extracted view of "Characterization of organic matter from the Cretaceous sedimentary and volcano-sedimentary strata from Livingston Island, Antarctic Peninsula: Insights from organic petrology, molecular proxies and carbon and hydrogen isotopes" by I Kostova et al
Characterization of organic matter from the Cretaceous sedimentary and . . . Organic matter (OM) originates predominantly from terrestrially-derived organic particles Mostly highly fragmented plant remains, and locally vitrinite semifusinite as part of plant compressions imprints or thin vitrain fusain lenses, are present
Geochemical characterization of late Jurassic – early Cretaceous age . . . The paleo-depositional environments such as paleo-redox conditions and paleo-water salinity enforce an important control on the quality and abundance of organic matter in sedimentary rocks, while the maturity of rocks rich in organic material plays a significant role in the mutation of organic matter into moving hydrocarbons (Qiao et al , 2021