Long-term variations of the geomagnetic field, observed in the palaeomagnetic record, have
the potential to shed much light on the evolution of Earth's deep interior. With a geomagnetic …

Центр коллективного пользования «Петрофизика, геомеханика и палеомагнетизм»,
созданный на базе активно развивающихся структурных подразделений Института …

Our understanding of the past behavior of the geomagnetic field arises from magnetic
signals stored in geological materials, eg,(volcanic) rocks. Bulk rock samples, however …

The magnetic record, preserved by igneous rocks in the form of thermoremanent
magnetization (TRM) or thermo‐chemical remanent magnetization (TCRM), is essential to …

Recovering the geomagnetic field strength in the past is key to understanding deep Earth
dynamics and detecting potential geodynamo regimes throughout the history of Earth. To …

We conducted an absolute paleointensity survey on 74 lava flows from the Okhotsk–
Chukotka Volcanic Belt (NE Russia), emplaced 90–83 Ma toward the end of the Cretaceous …

The state of the geomagnetic field throughout the Precambrian era is largely unknown.
Approximately 8% of global paleointensity records account for∼ 4 billion years of Earth …

Volcanic rocks, preserving paleorecords of Earth's magnetic field, are essential to constrain
the working of the geodynamo, provided their primary signal was not biased. Using a …

The experiments have been carried out on the acquisition of thermochemical remanent
magnetization (TCRM) in basalt samples containing titanomagnetite (TM) with the Curie …

Precambrian palaeointensity measurements provide fundamental constraints on the
evolution of the deep Earth. Core evolution models predict trends in dipole moment on …