Results 71 to 80 of about 4,235 (222)

Late Miocene magnetostratigraphy in the Mediterranean [PDF]

open access: yes, 1984
Reversals of the geomagnetic field In the geological past are recorded globally in the natural remanent magnetization (NRM) of igneous and sedimentary rock sequences.
Langereis, C.G.   +4 more
core  

(Table 5) Magnetostratigraphy at DSDP Site 86-576

open access: yes, 1985
(Table 5) Magnetostratigraphy at DSDP Site 86 ...
David K Rea (6961106)   +5 more
core   +1 more source

Synchronous Advance of the Alpine Glaciation Across the Northern and Southern Tibetan Plateau During the Mid‐Pleistocene Transition

open access: yesGeophysical Research Letters, Volume 53, Issue 14, 28 July 2026.
Abstract Chronological studies of glacial sediments from the Shishapangma and Yarlung Tsangpo River valley indicate that Quaternary glaciation on the southern Tibetan Plateau commenced at ∼0.75–0.83 Ma. However, the oldest glacial deposits in the northern plateau are dated to only ∼0.46 Ma, markedly later than the Middle Pleistocene glacial ...
Chengying Liu   +5 more
wiley   +1 more source

(Table S4) Magnetostratigraphy of ODP Site 208-1263

open access: yes, 2015
(Table S4) Magnetostratigraphy of ODP Site 208 ...
Frederichs, Thomas   +9 more
core   +1 more source

MS and NGR data used in cyclostratigraphy analyses, and the magnetostratigraphy and cyclostratigraphy age data

open access: yes, 2022
The raw data, the linear interpolated data, and detrended data of MS and NGR used for Cyclostratigraphy Analyses, and the magnetostratigraphy and cyclostratigraphy age data.
Ye Xu (29869)   +9 more
core   +1 more source

Tracing the Migration of Fronts in the Pacific Southern Ocean Across the Mid‐Pleistocene Transition

open access: yesPaleoceanography and Paleoclimatology, Volume 41, Issue 7, July 2026.
Abstract The Southern Ocean is a key driver of global climate variability, yet its dynamics during the Mid‐Pleistocene Transition (MPT; ∼1.25–0.7 Ma) remain poorly understood, especially in the South Pacific sector. The Polar Frontal Zone (PFZ) underwent significant latitudinal shifts during this critical period of climate reorganization.
V. M. Sinnen   +6 more
wiley   +1 more source

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
Widespread aeolian loess‐paleosol and red clay sediments on the Chinese Loess Plateau (CLP) provide a globally unique terrestrial archive of Neogene–Quaternary climate.
Xinxia Li   +11 more
doaj   +1 more source

Quickly erupted volcanic sections of the Steens Basalt, Columbia River Basalt Group: Secular variation, tectonic rotation, and the Steens Mountain reversal

open access: yesGeochemistry, Geophysics, Geosystems, 2008
The Steens Basalt, now considered part of the Columbia River Basalt Group (CRBG), contains the earliest eruptions of this magmatic episode. Lava flows of the Steens Basalt cover about 50,000 km2 of the Oregon Plateau in sections up to 1000 m thick.
Nicholas A. Jarboe   +4 more
doaj   +1 more source

(Table 8) Magnetostratigraphy at DSDP Site 86-578

open access: yes, 1985
(Table 8) Magnetostratigraphy at DSDP Site 86 ...
David K Rea (6961106)   +5 more
core   +1 more source

Osmium Isotope and Highly Siderophile Element Constraints on the Cretaceous/Paleogene Boundary in Western Pacific Pelagic Clay

open access: yesGeochemistry, Geophysics, Geosystems, Volume 27, Issue 7, July 2026.
Abstract The Cretaceous/Paleogene (K/Pg) Chicxulub impact produced globally synchronous enrichments of highly siderophile elements (HSEs) and a pronounced decline in marine osmium isotope ratios (187Os/188Os), forming a key geochemical marker of the boundary.
Honami Sato   +6 more
wiley   +1 more source

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