Titanomagnetites in mid‐ocean ridge basalt (MORB) experience variable post crystallization
alterations associated with seafloor tectonic and environmental processes. Compared to low …

Hydrothermal alteration at high‐temperature vents near mid‐ocean ridge is thought to
produce pervasive magnetization lows on basaltic ocean crust, but the detailed alteration …

Magnetic properties (natural remanent magnetization (NRM), susceptibility (χ), Curie point
temperature (Tc), saturation isothermal remanent magnetization (IRMs), and Köenigsberger …

Magnetic minerals in six samples of oceanic basalts of the transition zone and upper
sheeted dikes from Deep Sea Drilling Project/Ocean Drilling Program (DSDP/ODP) Hole …

Previous rock magnetic investigations of oceanic basement samples have been mainly
restricted by single drill holes or dredge collections. In this study, we present new and …

Seafloor hydrothermal systems in the back-arc region of the Okinawa Trough have been
viewed as a modern analogue to the Kuroko-type volcanogenic massive sulfide deposits …

The fact that the natural remanent magnetization (NRM) intensity of mid-oceanic-ridge basalt
(MORB) samples shows systematic variations as a function of age has long been …

High-resolution vector magnetic measurements were performed on an inactive ultramafic-
hosted hydrothermal vent field, called Yokoniwa Hydrothermal Field (YHF), using a deep …

Scanning and transmission electron microscopy (STEM) of ocean-floor pillow basalts with
ages between 0 and 70 Ma reveals progressive alteration of submicrometer titanomagnetite …

We studied the change of magnetic behaviour upon laboratory heating of altered mid-ocean
ridge basalt (MORB) samples in the age range of 16–35 Ma to determine the influence of …