Results 181 to 190 of about 97,532 (300)
Abstract The Nanga Parbat–Haramosh Massif located in the northwestern syntaxis of the Himalaya is an antiformal structure considered as a crustal diapir undergoing exhumation at a rate larger than 10 mm/yr since 1 Ma. Using GNSS horizontal surface velocities and a vertical and east–west decomposition of the Sentinel‐1 interferometric line‐of‐sight ...
Pauline Meyer +6 more
wiley +1 more source
Correction: Triton, a new species-level database of Cenozoic planktonic foraminiferal occurrences. [PDF]
Fenton IS +7 more
europepmc +1 more source
Abstract The Southern Rocky Mountain Trench (SRMT) is a conspicuous valley in the eastern Canadian Cordillera. It lies above a sharp change in lithospheric strength and thickness and is occupied by a normal fault thought to have last been active in the Eocene.
T. Finley +5 more
wiley +1 more source
The end-Cretaceous mass extinction restructured functional diversity but failed to configure the modern marine biota. [PDF]
Edie SM, Collins KS, Jablonski D.
europepmc +1 more source
Abstract The Wyoming Craton is often cited as an example of decratonization, implying the removal of its lithospheric keel. However, numerous geophysical imaging studies indicate the presence of thick mantle lithosphere beneath much of the Wyoming Craton.
M. J. Bezada +3 more
wiley +1 more source
The earliest fossil cetacean with <i>Osedax</i> borings: narrowing the spatiotemporal gap between Cretaceous marine reptiles and late Cenozoic whales. [PDF]
Jamison-Todd S, Mannion PD, Upchurch P.
europepmc +1 more source
Mount Etna as a Leaking Pipe of Magmas From the Low Velocity Zone
Abstract Mount Etna, one of the most active volcanoes on Earth, exhibits unusual characteristics in terms of its geological setting, effusion rate, and volatile content. Mount Etna is closely related to the subduction of the Ionian plate below Eurasia, but, chemically, Mount Etna lavas are akin to intraplate magmatism.
Sebastien Pilet +6 more
wiley +1 more source
Tracking bioturbation through time: The evolution of the marine sedimentary mixed and transition layers. [PDF]
Tarhan LG +7 more
europepmc +1 more source
Abstract Joint estimation of discrete (e.g., lithology or geofluid type) and continuous (e.g., porosity, pore geometry, related connectivity) subsurface parameters represents a challenging inverse problem due to strong parameter trade‐offs, effective non‐uniqueness, and multi‐modal posterior structures.
Chunjie Zhang, Hikaru Iwamori
wiley +1 more source
Investigating tectonic links between the deep Volturno plain and Campanian volcanism using vintage seismic and potential field data. [PDF]
Bruno PPG +3 more
europepmc +1 more source

