Results 91 to 100 of about 8,049 (227)
Climate and Tectonic Forcing of Depositional Evolution in the Southern North China Basin Since ∼3 Ma
Abstract Marginal basins provide sensitive yet incomplete records of climate and tectonic forcing, and the southern North China Basin provides an ideal setting to decode these interactions since the late Pliocene. A 135.6‐m borehole sequence, the XiaoQian (XQ) core, recovered from the Fuyang region, was dated using AMS 14C, OSL, and ESR, supplemented ...
Ting Wang +8 more
wiley +1 more source
Abstract Characteristic remanent magnetizations isolated from the late Variscan Altenberg–Teplice Caldera exhibit paleomagnetic directions, ranging from those consistent with the expected primary Late Carboniferous geomagnetic field to intermediate directions that significantly diverge from the dipole states.
P. Vitouš +3 more
wiley +1 more source
In order to obtain the missing data on the magnetostratigraphy of transitional layers between Sarmatian and the Maeotian parts in the Eastern Paratethys, the authors studied the Upper Sarmatian ― the Lower Maeotian deposits in the Panagia Cape section ...
Pilipenko O.V. +4 more
doaj +1 more source
Magnetostratigraphy of Equatorial Pacific Site 503 Hydraulic Piston Cores [PDF]
The paleomagnetic measurement procedure at Site 503 was similar to that described for Site 502 (See preceding chapter). Each core section was measured with the longcore spinner magnetometer at 10-cm intervals.
Kent, Dennis V., Spariosu, Dann J.
core +2 more sources
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
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
Aproximación a la magnetoestratigrafía de la última terraza media del Guadalquivir (T12) en "las Jarillas" (La Rinconada, Sevilla) [PDF]
"Preliminary magnetostratigraphy of the Guadalquivir river last middle terrace (T12) in “Las Jarillas” (La Rinconada, Sevilla)" Present a model of alluvial in the last middle terrace (T12) in the Guadalquivir river from La Rinconada (Sevilla).
Baena Escudero, Rafael +1 more
core
Magnetostratigraphy of Oligocene to Pleistocene Sediments, Sites 558 and 563 [PDF]
Integrated magnetostratigraphic and biostratigraphic studies of DSDP Sites 563 and 558 (western North Atlantic) show that, except for a short (~2 Ma) early Miocene hiatus, deposition was continuous from time of seafloor formation (Site 563, between ...
Kent, Dennis V. +2 more
core +2 more sources
Abstract The transport medium, mode, energy, and distance are recorded in the grain‐size and grain‐shape distributions in a sedimentary deposit. While grain‐size analysis has long been used in sedimentology, grain‐shape analysis is increasingly recognized as a valuable tool for reconstructing sedimentary processes and palaeoenvironments.
P. P. Stark +5 more
wiley +1 more source
Abstract International Ocean Discovery Program (IODP) Site U1417, located in the Surveyor Fan (Gulf of Alaska), preserves hemipelagic sediments influenced by glacial and fluvial depositional processes from the Cordilleran Ice Sheet in the Chugach–St. Elias Mountains and Coastal Mountains.
B. K. Khim, S. Kim, H. Asahi
wiley +1 more source

