Results 71 to 80 of about 4,235 (222)
Late Miocene magnetostratigraphy in the Mediterranean [PDF]
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
(Table 5) Magnetostratigraphy at DSDP Site 86 ...
David K Rea (6961106) +5 more
core +1 more source
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
(Table S4) Magnetostratigraphy of ODP Site 208 ...
Frederichs, Thomas +9 more
core +1 more source
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
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
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
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
(Table 8) Magnetostratigraphy at DSDP Site 86 ...
David K Rea (6961106) +5 more
core +1 more source
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

