The interaction between ultramafic rocks and hot seawater at slow-spreading mid-oceanic
ridges triggers hydrothermal redox reactions which are known to produce magnetite and H2 …

If magnetite is a common serpentinization product, centimetric, massive and pure magnetite
veins are rarely observed in serpentinites. Unique example, in the Aït Ahmane ultramafic …

The continental margins of the South China Sea (SCS) have undergone episodic rifting
since the Cenozoic, and there are ongoing debates surrounding the processes of crustal …

Abstract The Lakang'e porphyry Mo (Cu) deposit, intermediate to large in size, is located in
the eastern part of the southern Gangdese metallogenic belt. It is associated with a Miocene …

Detachment faults at slow‐and ultraslow‐spreading mid‐ocean ridges are essential for
lithosphere‐hydrosphere interactions. However, their coupling with subseafloor …

Discriminating magnetic minerals of different origins in natural samples is useful to reveal
their associated geological and environmental processes, which can be achieved by the …

Spinel is a ubiquitous mineral in mafic/ultramafic rocks. Spinel cores chemistry is extensively
used as a petrogenetic proxy while their alteration phases, ferritchromite, and Cr‐magnetite …

The outcrops of ultramafic rock along mid‐ocean ridges experience variable extents of
serpentinization related to tectonic and hydrothermal processes. It involves the water …

To quantify the alteration processes in the mantle from geophysical data, an understanding
of the relationship between alteration and the physical properties of mantle peridotite is …

Abstract The Swiss Atlas of Physical Properties of Rocks (SAPHYR) project aims at
centralize, uniform, and digitize dispersed and often hardly accessible laboratory data on …