Results 141 to 150 of about 64,005 (257)
Subcidence patterns (rate of evolution) of Moscow basin
Moscow basin had subsided in two “half-waves” velocity regime over the time-span: Cambrian (Vendian) — Devonian and carboniferous. Subsidence pattern of this basin in devonian-carboniferous was similar to that of the Dnepr-Donezk rift basin.
E A Dolginov, G Lafi
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Read the free Plain Language Summary for this article on the Journal blog. Abstract The impact of lightning in tropical forests remains uncertain. Specifically, the factors that influence the spatial distribution of lightning damage within forests remain unknown.
Bianca Zoletto +14 more
wiley +1 more source
ABSTRACT This article relocates Marx's theory of the metabolic rift within a broader geographical genealogy, recovering Massimo Quaini's contribution and showing how his work anticipates; in territorial terms, several theoretical components were later systematized by Foster.
Pasquale Pennacchio
wiley +1 more source
New U–Pb zircon dating shows the Rewan Group was deposited between ~250 and 233 million years ago and that sedimentation shifted across the basin through time, with earlier deposition in the foredeep and later deposition in the back bulge. Testing multiple dating approaches and grain‐selection strategies improves confidence in these age estimates and ...
Matthew Scipione +6 more
wiley +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
Differential Accumulation Dynamics of Organic Matter in the Central and Eastern Bohai Bay Basin (Eastern China): Implications for Tectonic Activity. [PDF]
Li Y +10 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
Rift linkage and inheritance determine collisional mountain belt evolution. [PDF]
Wolf SG, Huismans RS, Muñoz JA, May DA.
europepmc +1 more source
ABSTRACT The Quetico subprovince of the Superior Province is among the largest metasedimentary belts globally and provides evidence of tectonic processes at play during the final stages of Archean cratonization. Although previous studies have shown that deformation and metamorphism of the 2.7‐Ga turbiditic protolith resulted in regional subvertical ...
Adrian G. Rehm +4 more
wiley +1 more source

