Results 141 to 150 of about 44,585 (300)
Maastrichtian-paleogene benthic foraminifera from the Middle East and its distribution in the Tethys, a review [PDF]
Haidar Salim Anan
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Geochemical Disequilibrium at the Brittle‐Ductile Transition
Abstract We investigate the microtextural, microchemical, and isotopic effects of late‐stage ductile deformation in quartzite mylonites and kyanite–muscovite–quartz veins from the Raft River shear zone (Utah). Quartz microstructures record pervasive disequilibrium, expressed by unannealed features including undulatory extinction, deformation lamellae ...
Raphaël Gottardi +3 more
wiley +1 more source
Structural setting, stratigraphic relationships, paleontolgical character and sedimentology of Paleogene deposits cropping out in Cabrera Islands are described. They correspond to sandy to silty limestones building up a transgressive-regressive cicle that correlates with s'Envestida Calcarenites Fm. defined in Mallorca Is.
openaire +1 more source
Abstract Igneous Plumbing Systems in sedimentary basins comprise a complex of interconnected intrusive bodies that lead to volcano formation, though their 3D distribution and dynamics are not fully understood. We characterized the post‐breakup igneous plumbing systems at the Santos and Campos Basins using wells and 3D high‐resolution seismic and ...
A. Garcia, N. Stanton, A. Gordon
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Recovering the true size of an Eocene hyperthermal from the marine sedimentary record [PDF]
Kirtland-Turner, Sandy, Ridgwell, Andy
core +1 more source
Abstract Tectonic CO2 Earth degassing is globally relevant and has probably controlled climate on a geological scale (Brune et al., 2019, https://doi.org/10.1038/s41561‐017‐0003‐6). Endogenous CO2 outgassing from rifting areas remains poorly constrained, with most available data from the East African Rift.
Lisa Ricci +6 more
wiley +1 more source
Terrestrial evidence for the Lilliput effect across the Cretaceous-Paleogene (K-Pg) boundary
Logan A. Wiest +4 more
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Abstract The late Eocene to early Oligocene is an intriguing Paleogene period in which the Earth climate state changed from Warmhouse to Coolhouse. Accurate age models are essential for investigating these climate transitions. The southwestern Pacific International Ocean Discovery Program (IODP) Site U1553, with its almost complete succession of the ...
Yang Zhang +5 more
wiley +1 more source

