Ophiolites, which represent segments of oceanic lithosphere obducted onto the continental
crust, provide an important window into processes such as continental rifting, mantle …

Podiform chromitites have long supplied us with unrivaled information on various mantle
processes, including the peridotite-magma reaction, deep-seated magmatic evolution, and …

Heavily shocked meteorites contain various types of high‐pressure polymorphs of major
minerals (olivine, pyroxene, feldspar, and quartz) and accessory minerals (chromite and Ca …

Abstract Two-dimensional (2D) magnetic materials have attracted extensive research
attention in recent years due to their promising potential for use in nanoscale spintronic …

Podiform chromitites are commonly found within the Moho transition zone to mantle section
of ophiolites, as well as in non-ophiolitic peridotite massifs. However, they have rarely been …

Phase transitions that occur in materials, driven, for instance, by changes in temperature or
pressure, can dramatically change the materials' properties. Discovering new types of …

The absence of inherent magnetism in the family of 2D materials limits its application in
magnetoelectric and magnetic storage media. Here, a simple scalable route for the …

A microcrystalline polymineral aggregate was identified as an inclusion in a diamond from
the Rio Soriso area, Mato Grosso State, Brazil. It is composed of iron carbides, Fe-rich …

The corrosion behaviour of Alloy 690 under four different zinc addition scenarios was
investigated in circulating water containing 2 ppm Li and 1000 ppm B at 330° C. The …

Podiform chromitites occur in mantle peridotites of the Late Triassic Puerto Nuevo Ophiolite,
Baja California Sur State, Mexico. These are high-Cr chromitites [Cr#(Cr/Cr+ Al atomic ratio …