Results 51 to 60 of about 4,235 (222)
Rates of Geomagnetic Field Change During Excursions and Reversals
Abstract The Earth's magnetic field is characterized by complex changes, reflecting various geodynamo processes. Paleomagnetic studies have provided evidence of geomagnetic polarity reversals and excursions throughout Earth's history. We use data‐based paleomagnetic field models (LSMOD.2, GGFSS70, and GGFMB) and the axial dipole moment reconstruction ...
Sunaina Shinu +2 more
wiley +1 more source
All improved knowledge of the stratigraphy of the Rome area has been achieved trom the interpretation and correlation of a large number of stratigraphic logs from drillings, stored in a data bank by the Istituto Nazionale di Geofisica which allowed the ...
F. Marra, F. Florindo
doaj +1 more source
Worldwide database for magnetostratigraphy available [PDF]
The International Association of Geomagnetism and Aeronomy (IAGA) has sponsored the development of databases in paleomagnetism and rock magnetism. The databases operate under Microsoft Access V2.0 (for Windows 3.1) or Access 97 (for Windows 95) [McElhinny and Lock, 1996].
McElhinny, Michael W. +2 more
openaire +2 more sources
Table S30 - Magnetostratigraphy ODP Site 207-1258
Table S30 - Magnetostratigraphy ODP Site 207 ...
James C Zachos (6958619) +13 more
core +1 more source
Abstract The northern extent of Greater India is a critical, yet highly debated, parameter for reconstructing the India‐Asia collision. Previous paleomagnetic estimates, including the fill‐the‐gap and fixed great circle approaches, yield widely varying results, spanning from ∼200 to ∼3,000 km. These large discrepancies stem principally from two primary
Xianwei Jiao +3 more
wiley +1 more source
Geomagnetic Excursions Recorded in North Atlantic IODP Expedition 395C Sites U1555 and U1563
By studying deep‐sea drilled records from the North Atlantic Ocean, several magnetic instabilities of short duration, such as the Iceland Basin (188 ka), the Björn (1,255 ka) and the Gardar (1,460 ka) excursions, were discovered.
Anita Di Chiara +22 more
doaj +1 more source
Abstract Reconstructing past interactions between the West Antarctic Ice Sheet (WAIS) and changing environmental conditions in the Ross Sea region can help determine long‐term WAIS stability. Existing sedimentary records reveal changes to oceanography, sea ice and ice sheet extent over the glacial‐interglacial cycles of the last ∼800 kyr.
J. W. Marschalek +26 more
wiley +1 more source
(Table S7) Magnetostratigraphy of Site 198-1210
(Table S7) Magnetostratigraphy of Site 198 ...
Simonetta Monechi (6886928) +15 more
core +1 more source
Abstract The drawdown of atmospheric CO2 likely triggered Antarctic glaciation during the Eocene‐Oligocene Transition (34 Ma). Accurately constraining this shift from “greenhouse” to an “icehouse” climate is essential for understanding global carbon cycle dynamics.
Keehwan Lee +5 more
wiley +1 more source
The pattern of geomagnetic polarity changes during the Early Carboniferous (Mississippian) is not known in detail. This information sparsity is addressed by determining a magnetostratigraphy from the late Asbian (late Visean at ∼333 Ma) in Trowbarrow ...
Mark W. Hounslow +5 more
doaj +1 more source

