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2. Hematite - Wikipedia

   en.wikipedia.org/wiki/Hematite

   Hematite (/ ˈ h iː m ə ˌ t aɪ t, ˈ h ɛ m ə-/), also spelled as haematite, is a common iron oxide compound with the formula, Fe 2 O 3 and is widely found in rocks and soils. [6] Hematite crystals belong to the rhombohedral lattice system which is designated the alpha polymorph of Fe 2 O 3. It has the same crystal structure as corundum ...

3. Paleomagnetism - Wikipedia

   en.wikipedia.org/wiki/Paleomagnetism

   A common form is held by the mineral hematite, another iron oxide. Hematite forms through chemical oxidation reactions of other minerals in the rock including magnetite. Red beds, clastic sedimentary rocks (such as sandstones) are red because of hematite that formed during sedimentary diagenesis. The CRM signatures in red beds can be quite ...

4. Rock magnetism - Wikipedia

   en.wikipedia.org/wiki/Rock_magnetism

   Rock magnetism is the study of the magnetic properties of rocks, sediments and soils. The field arose out of the need in paleomagnetism to understand how rocks record the Earth's magnetic field. This remanence is carried by minerals, particularly certain strongly magnetic minerals like magnetite (the main source of magnetism in lodestone ).

5. Gunflint chert - Wikipedia

   en.wikipedia.org/wiki/Gunflint_Chert

   The Gunflint Iron Formation is a banded iron formation, composed predominantly of dense chert and slate layers interbedded with ankerite carbonate layers. The chert layers can be subdivided into black layers (containing organic material and pyrite), red layers (containing hematite), and green layers (containing siderite). [5]

6. Magnetite - Wikipedia

   en.wikipedia.org/wiki/Magnetite

   Magnetite has been important in understanding the conditions under which rocks form. Magnetite reacts with oxygen to produce hematite, and the mineral pair forms a buffer that can control how oxidizing its environment is (the oxygen fugacity). This buffer is known as the hematite-magnetite or HM buffer.

7. Nuvvuagittuq Greenstone Belt - Wikipedia

   en.wikipedia.org/wiki/Nuvvuagittuq_Greenstone_Belt

   A controversial paper [10] [11] published in March 2017 reported evidence for early life in these rocks. The paper describes putative fossilized microorganisms. The structures seen are interpreted as hematite tubes, and filaments, similar in morphology and size to those produced today by bacteria living in subsea hydrothermal vents. Several ...

8. Iron-rich sedimentary rocks - Wikipedia

   en.wikipedia.org/wiki/Iron-rich_sedimentary_rocks

   Some examples of minerals in iron-rich rocks containing oxides are limonite, hematite, and magnetite. An example of a mineral in iron-rich rock containing carbonates is siderite and an example of minerals in an iron-rich rock containing silicate is chamosite. [2] They are often interbedded with limestones, shales, and fine-grained sandstones.

9. Lodestone - Wikipedia

   en.wikipedia.org/wiki/Lodestone

   [19] [20] [21] While this has been shown to work, archaeologists have yet to discover an actual spoon made of magnetite in a Han tomb. [ 22 ] Based on his discovery of an Olmec artifact (a shaped and grooved magnetic bar) in North America, astronomer John Carlson suggests that lodestone may have been used by the Olmec more than a thousand years ...