Results 191 to 200 of about 16,196 (284)
Coupling between crustal uplift and magnetic demagnetization in the Tarim Basin. [PDF]
Xu B, Zhao C, Zhang L, Yu P.
europepmc +1 more source
Abstract In this paper, Singular Spectral Analysis (SSA) is applied to the geomagnetic field to delineate signatures from different sources, such as geomagnetic variability and lithospheric processes. We performed SSA on the Y component of the Swarm satellite magnetic field By during the period from September 2023 to January 2024. Eigen values obtained
Amrita Yadav +4 more
wiley +1 more source
Basal mantle structure regenerated through supercontinents. [PDF]
Peng P +8 more
europepmc +1 more source
Subduction Zone Magnetism: The Influence of Metamorphism and Serpentinization in the Mantle Wedge
Abstract Subduction zone magnetic anomalies have previously been used to infer their thermal structure assuming a uniformly serpentinized mantle carries a homogeneous, isotropic magnetization. However, seismic tomography, geological observations and numerical modeling provide increasing evidence for a non‐uniformly serpentinized mantle wedge that may ...
Y. Li +8 more
wiley +1 more source
Slab tearing and segmented subduction termination driven by transform tectonics. [PDF]
Shuck B +14 more
europepmc +1 more source
Magnetic Reversals During the Deccan Volcanism: Paleomagnetic Insights From the Pachmarhi Dykes
Abstract The three main dyke swarms that are linked to the Deccan Continental Flood Basalts are the Nasik‐Pune, Western Coastal, and Narmada‐Satpura‐Tapi (N‐S‐T) swarms. Encompassing approximately 244 mapped basaltic dykes, mainly trending E‐W and positioned along an ancient tectonic zone, the Pachmarhi dyke swarm is situated in the eastern N‐S‐T ...
Garima Shukla +2 more
wiley +1 more source
Geochemical fingerprinting of plume in Suswa silicic volcanics, Kenya rift. [PDF]
Hong LB +5 more
europepmc +1 more source
Abstract The compositional evolution of the Earth's mantle is the result of mantle differentiation and thermal evolution. Partial melting of mantle materials produces geochemical heterogeneities, allows for degassing and depends on the thermal state of the mantle, itself governed by convection.
Nicolas Récalde +4 more
wiley +1 more source
Lens effect of remnant blocks on deep mantle upwelling causing anomalous subsidence. [PDF]
Liu L +7 more
europepmc +1 more source

