Results 251 to 260 of about 66,624 (345)
Abstract While the evolution of individual passive marginal and foreland basins is well understood, the subsidence pattern of passive margins near convergence zones—where thrust loading overprints earlier extension and the typical wedge and foredeep are obscured—remains poorly understood.
Penggao Fang +3 more
wiley +1 more source
Plastid phylogenomics illuminates backbone relationships, divergence times and character evolution in Caryophyllaceae. [PDF]
Li H, Song S, Comes HP, Yang Z, Li P.
europepmc +1 more source
Abstract Marine carbonate carbon isotopes (δ13C), over orbital to multi‐million‐year timescales, provide critical insight into the carbon cycle connecting Earth's atmosphere, lithosphere, hydrosphere and biosphere. However, the influence of astronomical forcing on deep time carbon cycle dynamics remains poorly constrained.
Deyan Zhang +4 more
wiley +1 more source
Morphological traits and mitogenome of Thaumapsylla breviceps orientalis endemic to China provide insight into the evolution of the order Siphonaptera. [PDF]
Pu J +5 more
europepmc +1 more source
Abstract The Cretaceous–Eocene island arc of Hispaniola is currently shortened between the Bahamas carbonate platform to the north and the thickened crust of the Caribbean Large Igneous Province (CLIP) to the south. Within this transpressional setting, the 15–22‐km‐thick, ∼100‐km‐wide Beata Ridge (BR), the thickest portion of the CLIP, acts as a ...
J. M. Gorosabel‐Araus +3 more
wiley +1 more source
Integrated multidisciplinary approach for reducing uncertainty in reservoir characterization of the Bahariya Formation, Berenice Field, Egypt. [PDF]
Fawzy MN +3 more
europepmc +1 more source
Organic geochemistry records from two Palaeocene-Eocene Thermal Maximum sections in Denmark
Petra L Schoon +4 more
openalex +1 more source
Long‐Term Deformation in the Alpine‐Provence Foreland Constrained by In Situ Calcite U‐Pb Dating
Abstract The evolution of the Alpine‐Provence foreland is characterized by multiple deformation phases since the Mesozoic, representing successive compressional and extensional episodes. The precise timing and spatial evolution of these deformation phases remain poorly constrained due to the lack of absolute geochronological data. Here, we present U–Pb
Dorian Bienveignant +12 more
wiley +1 more source
A whole rock geochemical dataset for magmatic rocks drilled on the mid-Norwegian margin. [PDF]
Tegner C +26 more
europepmc +1 more source

