Identifying variation in dinosaur footprints and classifying problematic specimens via unbiased unsupervised machine learning. [PDF]
Hartmann G +3 more
europepmc +1 more source
Sedimentary Paleoenvironment and Hydrocarbon Generation Potential Evaluation of Middle Jurassic Coal-Measure Source Rocks in the Southern Beishan Area. [PDF]
Wang H +10 more
europepmc +1 more source
Integrating optimization and machine learning for estimating water resistivity and saturation in shaley sand reservoirs. [PDF]
Hameedy MAE, Mabrouk WM, Metwally AM.
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<i>Bicharracosaurus dionidei,</i> gen. et sp. nov., a new macronarian (Dinosauria, Sauropoda) from the Late Jurassic Cañadón Calcáreo Formation of Argentina and the problematic early evolution of macronarians. [PDF]
Reutter A +4 more
europepmc +1 more source
Palaeomagnetic and geochronologic results from lower cretaceous volcanics of the western Qiangtang terrane and implications for the Lhasa-Qiangtang collision. [PDF]
Zhang Y +13 more
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In the Early Jurassic, a large-scale transgression occurred on the South China continental margin (SCCM), affected by the initiation of Paleo-Pacific subduction.
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The Qinling mountains are situated in central China and mark the collisional assembly between the North and South China blocks. To understand the early Mesozoic evolution of the Qinling orogenic belt, we present new paleocurrent data, sandstone petrology
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Evidence for Collagen in a Fossil of the Lower Jurassic
Nature, 1966A WELL preserved specimen of Pholidophorus bechei Agassiz has been described from the Lower Lias of England1. The presence along its body axis of a conspicuous series of epineural intermuscular bones made it seem worth while to examine the microstructure of some endochondral bone of the head using the electron microscopic techniques recently developed ...
A R, Doberenz, R, Lund
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Spontaneous imbibition (SI) is a capillary-force controlled process, which has been identified as one of the most important mechanisms to affect hydrocarbon recovery from unconventional shale reservoirs. In this work, we focus on the mineral composition,
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