Results 151 to 160 of about 9,373 (256)

Intensification of Northern Hemisphere Glaciation Triggered the Red Clay to Loess‐Paleosol Shift on the Chinese Loess Plateau 2.7 Million Years Ago

open access: yesGeophysical Research Letters, Volume 53, Issue 4, 28 February 2026.
Abstract Widespread aeolian loess‐paleosol and red clay sediments on the Chinese Loess Plateau (CLP) provide a globally unique terrestrial archive of Neogene–Quaternary climate. However, the timing and associated mechanisms of red clay to loess‐paleosol shift remain debated.
Xinxia Li   +11 more
wiley   +1 more source

New Cretaceous Paleomagnetic and Geochronologic Data From the Antarctic Peninsula: Constraints on the Pre‐Opening Tectonic Evolution of the Drake Passage

open access: yesGeophysical Research Letters, Volume 53, Issue 4, 28 February 2026.
Abstract Reconstructing oroclinal orogens along the Fuegian Andes‐northern Antarctic Peninsula provides critical constraints on the pre‐opening tectonic evolution of the Drake Passage, although such efforts are limited by a lack of reliable Cretaceous paleomagnetic and geochronological data.
Liang Gao   +6 more
wiley   +1 more source

Unraveling the Enrichment Mechanisms of Rare Earth Elements in Deep‐Sea Sediments: An Environmental Magnetic Perspective

open access: yesGeophysical Research Letters, Volume 53, Issue 4, 28 February 2026.
Abstract Deep‐sea rare earth elements and yttrium (REY)‐rich sediments have attracted considerable attention since their discovery in 2011. However, the environmental factors controlling REY enrichment remain poorly understood, largely because paleoceanographic proxies are absent in pelagic clays.
Xiangfeng He   +8 more
wiley   +1 more source

Chemical Demagnetization of the Natural Remanent Magnetization of Rocks

open access: yesChemical Demagnetization of the Natural Remanent Magnetization of Rocks
In 1963, Kawai1) proposed a technique to clarify mineralogical control of the natural remanent magnetization (nrm) of the thin sections of the rock which contained the ferromagnetic minerals such as titanomagnetite-series and also ilmenite-series. He found that first the pure magnetite easely dissolves in concentrated hydrochloric acid and then follows
openaire  

Extraordinarily long duration of Eocene geomagnetic polarity reversals. [PDF]

open access: yesCommun Earth Environ
Yamamoto Y   +3 more
europepmc   +1 more source

Home - About - Disclaimer - Privacy