Accretion of "young" Phanerozoic subcontinental lithospheric mantle triggered by back-arc extension-the case of the Ivrea-Verbano Zone. [PDF]
Ogunyele AC +4 more
europepmc +1 more source
Seismic imaging of a basaltic Lesser Antilles slab from ancient tectonics. [PDF]
Yang X +7 more
europepmc +1 more source
Refined chronologies of magnetochron M0r reveal asynchronous terrestrial and marine carbon isotope responses to Oceanic Anoxic Event 1a. [PDF]
Lu GM +9 more
europepmc +1 more source
A cosmogenic 10Be anomaly during the late Miocene as independent time marker for marine archives. [PDF]
Koll D +9 more
europepmc +1 more source
Seafloor spreading of the third arm of the Afar triple junction: A review. [PDF]
Nyangena DN +2 more
europepmc +1 more source
A more reduced mantle beneath the lunar South Pole-Aitken basin. [PDF]
Zhang H +16 more
europepmc +1 more source
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Lithospheric magnetic anomalies in Southeast Asia from CHAMP data
Izvestiya, Physics of the Solid Earth, 2013New possibilities for the interpretation of long-period magnetic anomalies were opened up by the construction of their first satellite-based maps. The anomalies are due to lateral variations in the magnetic properties and thickness of the deep layers of magnetized rocks.
D Yu Abramova, L M Abramova
exaly +2 more sources
Changes of lithospheric magnetic anomalies with altitude (According to the CHAMP satellite)
Geomagnetism and Aeronomy, 2016Maps of the magnitude of the full vector and the vertical component of an anomalous lithospheric magnetic field over the Voronezh anticline (VA) for the three high-altitude observation levels were compiled based on geomagnetic measurements from the CHAMP satellite. The isometric positive anomaly centered at about 50° N and 37° E stands out.
D Yu Abramova +2 more
exaly +2 more sources
The potential contribution to long wavelength magnetic anomalies from the lithospheric mantle
Physics of the Earth and Planetary Interiors, 2019Abstract Long-wavelength magnetic anomalies (LWMA) are broad scale variations of the magnetic field that are usually observed at high altitudes with amplitudes ranging up to about 20 nT. The source of these anomalies has typically been assumed to reside within the crust with negligible contributions from the lithospheric mantle.
Justin Filiberto +2 more
exaly +2 more sources

