Results 151 to 160 of about 117,682 (272)
Obligate faunivorous megatheropod size class patterns across the Jurassic-Cretaceous Periods. [PDF]
Boisvert C +5 more
europepmc +1 more source
Hornblendite in the Lower Crust: A Possible Source for Porphyry Cu Deposits
Abstract Lower crustal sulfide‐bearing Cu‐rich cumulates, mainly occurring as hornblendite, have been proposed as a critical source component for the development of giant porphyry Cu deposits (PCDs); however, their mineralogical and geochemical nature remain elusive.
Guangxu Li +5 more
wiley +1 more source
The osteology, taxonomy, and phylogenetic affinities of the Early Jurassic plesiosaur <i>Lusonectes sauvagei</i>. [PDF]
Sachs S, Madzia D.
europepmc +1 more source
Putative Analogs of Pyrite Suns Forming in Proglacial Alaska Mudflats
Abstract Disc‐shaped pyrite suns of the Pennsylvanian age Anna Shale are thought to have formed where pressure restricted pyrite crystal growth to a flattened disc shape during diagenesis at the Anna Shale and the underlying Herrin coal boundary.
Heather L. Fair +2 more
wiley +1 more source
Phylogenetic analysis of fossil stems in Yiwu Jurassic Forest, Hami, Xinjiang, Northwest China. [PDF]
Gou XD, Jiang Y, Liu MJ.
europepmc +1 more source
Abstract Granitoid magmatism along the western Pacific margin records interactions between subduction dynamics and crust–mantle processes; however, the links between plate reorganization and magma‐source evolution remain debated. Here we integrate U–Pb zircon geochronology with Pb–Sr–Nd–Hf isotope systematics to investigate Cretaceous–Paleogene ...
Nghiem V. Dao +7 more
wiley +1 more source
Effects of diagenetic stage and burial depth on the microstructure and mechanical properties of coal-bearing sandstones. [PDF]
Wang J +7 more
europepmc +1 more source
Abstract The paleomagnetism of Miocene calc‐alkaline volcanics and sediments from Sardinia has firmly showed that the Corsica‐Sardinia microplate rotated 50°–60° counterclockwise (CCW) with respect to Europe between 21 and 15 Ma, during its drift from the Provencal margin. However, Permian to Eocene rocks from central‐south Sardinia revealed higher (up
Gaia Siravo +3 more
wiley +1 more source
Quantitative characterization and optimization of fracability in continental shale reservoirs. [PDF]
Cheng L, Gao H, Li H.
europepmc +1 more source

