Results 201 to 210 of about 97,532 (300)
Abstract This study investigates two burial‐related remagnetizations in the Jaca–Pamplona foreland basin (Southern Pyrenees): one with dual polarity and a positive reversals test, and another with only reverse polarity. These components, labeled C3 and C4 based on their mean unblocking temperatures, were identified from a paleomagnetic analysis of 142 ...
P. Calvín +8 more
wiley +1 more source
Record of Foraminifera test composition throughout the Phanerozoic. [PDF]
Faulkner K +4 more
europepmc +1 more source
Abstract The Ediacaran–Cambrian (∼635–539 Ma) geomagnetic field is characterized by unusually high reversal rates and markedly weakened field strength. Estimates of these reversal frequencies can reveal key aspects of deep Earth dynamics and their potential influence on surface environments and early complex life.
J. W. L. Afonso +12 more
wiley +1 more source
Testing the Accuracy of Paleointensity Estimates Using Experimental Pottery Assemblages
Abstract Paleointensity estimates from archaeological pottery represent a key source of information on Holocene variations in geomagnetic field intensity. Yet, pottery rarely exhibits ideal single‐domain behavior that fully satisfies the theoretical assumptions underlying absolute paleointensity methods.
Lior Bar‐Sovik +5 more
wiley +1 more source
Spatiotemporal decoupling of floristic endemism in response to Qinghai-Tibet Plateau uplift. [PDF]
Yang B, Wang X.
europepmc +1 more source
Abstract The cores of rocky planets, including the Earth, are believed to contain light elements such as silicon, oxygen, sulfur, hydrogen, and carbon. Amongst them, sulfur appears to be rich in the cores of small terrestrial bodies like Mars and Ganymede. To understand the evolution of sulfur‐rich cores in the presence of other light elements, we have
Jeongmin Lee +9 more
wiley +1 more source
A unique Sphenophyllum-mimicking insect in the Permian. [PDF]
Fu Y +7 more
europepmc +1 more source
Channel Evolution During Drawdown of Iron Gate and Copco I Reservoirs, Klamath River, CA
Abstract This study used the world's largest dam removal on the Klamath River to investigate channel evolution in unconsolidated silt and clay sediment during reservoir drawdown. Timelapse imagery revealed retrogressing rotational slides and flowslides as key sources of sediment to the re‐emerging channels.
William Nuckoles, Desirée Tullos
wiley +1 more source
Modeling of the Arabian/Nubian shield's geothermal structure: a multi-parametric analysis using geophysical and geological tools. [PDF]
Haggag M +5 more
europepmc +1 more source

