Results 71 to 80 of about 3,374 (191)
Bending the Sierra Madre Oriental: A Paleocene Orocline
Abstract The Sierra Madre Oriental belt of the Mexican thin‐skinned fold‐and‐thrust belt, which formed during the Late Cretaceous due to the subduction of the Farallon Plate beneath North America, exhibits a pronounced curvature of approximately 100°, concave to the southwest.
Rafael Guerra Roel +5 more
wiley +1 more source
Rotational remagnetization and orientational transitions in submicron YIG films
It is shown that for the quasinormal remagnetization of the submicron YIG films with the normal along the [111] axis, which are in the single-domain state, two types of orientation transitions (OT) due to the influence of easy axes can be distinguished ...
Vladyslav Poimanov +3 more
doaj +1 more source
Abstract The Paleo‐Asian Ocean's (PAO) closure timing and the Alxa Block's (ALB) tectonic affinity remain debated. We present new paleomagnetic and geochronologic data from Permian volcanic and sedimentary rocks in the ALB. Characteristic remanent magnetization (ChRM) directions from Early (∼282 Ma), Middle (∼268 Ma), and Late Permian (∼255 Ma) rocks ...
Wei Xu +10 more
wiley +1 more source
Palaeomagnetism of the Bayan Gol formation, western Mongolia [PDF]
Oriented samples of the Lower Cambrian Bayan Gol Formation from Salaany Gol, Mongolia, were collected at roughly 5 m stratigraphic intervals for palaeomagnetic analysis.
Budney, C. J. +3 more
core +1 more source
Abstract Magnetic minerals can preserve remanent magnetization to provide ancient magnetic field records. Although thermoremanent magnetization (TRM) is well understood, chemical remanent magnetization (CRM) from chemical processes is also prevalent in nature and can complicate TRM records by introducing additional remanence signals.
Shichu Chen, Liao Chang, Wyn Williams
wiley +1 more source
Contrasting Recording Efficiency of Chemical Versus Depositional Remanent Magnetization in Sediments
How and when sedimentary rocks record Earth's magnetic field is complex. Most studies assume a time‐progressive lock‐in mechanism during sediment deposition called depositional remanent magnetization (DRM).
Sophie C. Roud, Stuart A. Gilder
doaj +1 more source
Experimental findings of investigation of magnetoresistive and magnetooptical properties of materials, in which the spin-dependent electron scattering can be implemented in the film magnetic Co- and Fe-based systems as well as nonmagnetic Cu-, Ag-, Au ...
I. Yu. Protsenko, I. V. Cheshko, L. V. Odnodvorets’, D. M. Kondrakhova, O. V. Pylypenko, Yu. M. Shabel’nyk, O. V. Vlasenko
doaj +1 more source
The in-plane magnetic structure of a layered system composed of polycrystalline grains smaller than the ferromagnetic exchange length was studied to elucidate the mechanism controlling the magnetic properties considerably different from the bulk using ...
Ryuji Maruyama +5 more
doaj +1 more source
Quasi-Superradiant Soliton State of Matter in Quantum Metamaterials [PDF]
Strong interaction of a system of quantum emitters (e.g., two-level atoms) with electromagnetic field induces specific correlations in the system accompanied by a drastic insrease of emitted radiation (superradiation or superfluorescence).
Asai, H. +3 more
core +1 more source
Abstract To constrain the temporal and spatial evolution of the Ganzi‐Litang Paleo‐Tethys Ocean, this study presents the first paleomagnetic results from Late Triassic volcanic rocks in the Yidun terrane in the eastern Tibetan Plateau. The mean paleomagnetic direction for 27 sites is Ds = 39.2°, Is = −52.9°, κs = 42.2, α95 = 4.3°, and the paleomagnetic
Yong Cao +7 more
wiley +1 more source

