The following table is an overview of different iron-nickel alloys.

The iron-nickel group is characterized by several iron-nickel alloy species.

Iron-nickel alloy - an alternative expression for meteoric iron.

They range from 0.01 to 0.5mm in thickness and are made from copper, nickel or iron-nickel alloy depending on the application.

Gibeon meteorites are made of an iron-nickel alloy, but contain also cobalt and phosphorus.

The RAT was designed to drill into ordinary rock, not into iron-nickel alloy.

Some surveyors used an iron-nickel alloy tape for extremely precise measurements because those tapes contracted or expanded less with cold or heat.

While the parent body of the meteorites cools off, the metallic core crystallizes into meteoric iron, an iron-nickel alloy.

Analysis showed that the meteorite contained, apart from iron-nickel alloy, a small quantity of silicates (pyroxenes) not occurring on Earth.

Reed switches use a matched seal between an iron-nickel alloy (NiFe 52) and a matched glass.

The inner core of the Earth is generally assumed to consist essentially of an iron-nickel alloy with ε (or β) structure.

Metallic iron is virtually unknown on the surface of the Earth except as iron-nickel alloys from meteorites and very rare forms of deep mantle xenoliths.

Fessenden replaced Edison's delicate platinum lead-in wires with an iron-nickel alloy, thus greatly reducing the cost and increasing the life of the lamp.

About 5% of meteorites that fall are iron meteorites with intergrowths of iron-nickel alloys, such as kamacite and taenite.

Metallic meteorites are composed primarily of the iron-nickel alloys: taenite (high nickel content) and kamacite (low nickel content).

Instead of threading individual ferrite cores on wires, plated wire memory used a grid of wires coated with a thin layer of iron-nickel alloy (called permalloy).

Iron meteorites are meteorites that consist overwhelmingly of an iron-nickel alloy known as meteoric iron that usually consists of two mineral phases, kamacite and taenite.

Instead of threading individual ferrite cores on wires, thin-film memory consisted of 4 micrometre thick dots of permalloy, an iron-nickel alloy, deposited on small glass plates by vacuum evaporation techniques and a mask.

While it makes up about 5% of the Earth's crust, both the Earth's inner and outer core are believed to consist largely of an iron-nickel alloy constituting 35% of the mass of the Earth as a whole.

A similar heterogeneous alloy wire with an Iron-Nickel alloy core and copper cladding under the trade name, Dumet, (Dual-Metal) is also used for this purpose, but for passing through softer soda-lime and lead-alkali glasses.

A very high specific gravity becomes very pronounced in native metals; kamacite, an iron-nickel alloy common in iron meteorites has a specific gravity of 7.9, and gold has an observed specific gravity between 15 and 19.3.

But in a room across the hall from his office, Dr. Prinz can hold in his hand a small moon rock, retrieved by Apollo 11, a smaller piece of Mars, a weighty meteor decorated, by some spontaneous internal chemistry, with crisscrossed bands of iron-nickel alloy.

NiFe redirects here, for the battery see Nickel-iron battery A iron-nickel alloy, nickel-iron alloy, or abbreviated FeNi and NiFe, is a group of alloys that mostly consist of the elements nickel (Ni) and iron (Fe).