Results 291 to 300 of about 204,393 (382)
Petrographic and Molecular Characterization of Organic-Rich Mudstones with Petroleum Generative Potential from The Lower Triassic Montney Formation, Western Canada. [PDF]
Becerra D+5 more
europepmc +1 more source
Abstract In Jezero crater, Mars, the Perseverance rover has explored the western fan and encountered loose pieces of rock separated from outcrops or “float” rocks. Comparing float rocks to in‐place outcrops can provide key insights into the crater's erosional history and the diversity of units in the Jezero watershed that Perseverance cannot visit in ...
B. S. Kathir+21 more
wiley +1 more source
Microfacies Characteristics of Late Pennsylvanian Cyclothems on the Carbonate Platform Margin in Guizhou, South China. [PDF]
Wang J+6 more
europepmc +1 more source
Abstract Core images provide a high‐resolution data set of the textures and fabrics of sedimentary rocks, but their availability is often limited by cost and/or poor core recovery. An alternative solution is to utilize advanced high‐resolution micro‐resistivity images acquired through wireline logging, such as the Formation MicroScanner (FMS).
Saira Baharuddin, Cédric M. John
wiley +1 more source
Heterolytic tide-dominated sedimentary facies and depositional environment: An Example from the Boka Bil formation, Sitapahar anticline, Bangladesh. [PDF]
Ali S+8 more
europepmc +1 more source
Abstract The Aegean region marks the convergent boundary between the African and Eurasian plates, reflecting complex tectonic processes, including the closure of the Pindos ocean. The Pelagonian unit (PU) forms the core of mainland Greece and was part of the Eurasian continental margin, while the Pindos oceanic crust subducted beneath it.
Shijie Shang+4 more
wiley +1 more source
Morphological, Morphometrical and Radiological Features of the Pelvic Limb Skeleton in African Green Monkeys (Chlorocebus sabaeus) from Saint Kitts and Nevis Islands. [PDF]
Martonos CO+5 more
europepmc +1 more source
Abstract The North Pyrenean Zone results from the Late Cretaceous‐Cenozoic inversion of the Mesozoic rift system extending along the Iberia‐Europe plate boundary. The western part of this inverted rift (from the Tardets‐Mauléon basin in the West to the Bigorre basin in the East) is strongly decoupled from the basement along Upper Triassic evaporites ...
Esther Izquierdo‐Llavall+6 more
wiley +1 more source
Proto-Tethyan tectonics in East China: a revisit. [PDF]
Meng QR+6 more
europepmc +1 more source