Results 201 to 210 of about 8,265,842 (328)
Discussion on structural evolution of Mesozoic Peninsular Malaysia [PDF]
Altermann +22 more
core +1 more source
2D seismic and well data reveal multi‐phase basin filling in the Whatcom Sub‐Basin shaped by syn‐depositional tectonism. An Eocene transition from forearc basin to forearc depression corresponds to decreasing normal‐fault density and throw, both upsection and eastward. Paleogene–Neogene strata are the best CO2 storage targets.
Francyne Bochi do Amarante +4 more
wiley +1 more source
Ben Thuy +8 more
semanticscholar +1 more source
The study of heavy mineral assemblages with statistical analysis resolves provenance signatures and quantifies syn‐emplacement modification of sand injection complexes. Results demonstrate transformative petrological processes, including density‐dependent hydraulic sorting and mechanical grain degradation.
Gustavo Zvirtes +6 more
wiley +1 more source
A global overview of pterosaur ichnology: tracksite distribution in space and time [PDF]
Harris, Jerald D. +2 more
core +1 more source
Paleogene unconformity development from ~64 to 22 Ma for the Magallanes‐Austral retroarc foreland basin (MAB). Schematic shows (A) MAB foreland subsidence and basin infilling, (B) onset of cooling and basin inversion as subducting plate shallows, (C) continued foreland uplift, erosion and cooling as the oblique Farallon‐Phoenix ridge subducts beneath ...
Rebecca A. VanderLeest +4 more
wiley +1 more source
ABSTRACT Urban bushland fragments have important natural and social values. Their management is challenging because they typically have experienced complex historical disturbances, making it difficult to settle on the most appropriate restoration targets. We illustrate these issues by chronicling vegetation and fire regime changes in the Queens Domain,
David M. J. S. Bowman +6 more
wiley +1 more source
A new teleosaurid (Crocodylomorpha, Thalattosuchia) from the Sibumasu Terrane of Southeast Asia and a taxonomic reassessment of <i>Indosinosuchus</i>. [PDF]
Lauprasert K +9 more
europepmc +1 more source
ABSTRACT During the Paleocene‐Eocene Thermal Maximum (PETM), there was an increase in global temperatures and emissions of isotopically depleted carbon, resulting in a negative carbon isotope excursion (CIE). This climatic event caused a widespread ocean deoxygenation, leading to substantial biotic turnover.
Olmo Miguez‐Salas +2 more
wiley +1 more source

