The basic features of the geomagnetic reversal chronology of the last 160 million years are
well established. The relationship between this history and other features of the field …

We present here new paleointensity data from 39 sampling sites collected from the
quenched margins of pillow lavas and dikes exposed within the Troodos Ophiolite (∼ 92 …

Palaeomagnetic field intensity measurements, derived from rocks with ages that span
geological time, provide a crucial constraint on the evolution of Earth's deep interior and its …

The global paleointensity database for 65–200 Ma was analyzed using a modified suite of
paleointensity quality criteria (QPI) such that the likely reliability of measurements is …

Tholeiite of the oldest oceanic crust was drilled during ODP Legs 129 and 185 at Hole 801C
in the western Pacific. Fresh appearing submarine basaltic glass (SBG) was recovered from …

Many geodynamo models predict an inverse relationship between geomagnetic reversal
frequency and field strength. However, most of the absolute paleointensity data, obtained …

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 …

We report palaeomagnetic and 40Ar/39Ar dating results from two sequences of basaltic lava
flows deposited at the same locality in western China, yet separated in time by~ 50 Myr: one …

Unravelling the long-term behaviour of the geomagnetic field is crucial for understanding the
dynamics of the deep Earth. Yet, obtaining an accurate measure of geomagnetic …

We present the first geomagnetic paleointensity measurements on single plagioclase
crystals from lavas formed during the∼ 262–318Ma Permo-Carboniferous Reverse Polarity …