Indicators of aqueous alteration in CM carbonaceous chondrites: Microtextures of a layered mineral containing Fe, S, O and Ni
- 1 October 1985
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 49 (10) , 2149-2163
- https://doi.org/10.1016/0016-7037(85)90073-0
Abstract
No abstract availableThis publication has 21 references indexed in Scilit:
- Proposed structures for poorly characterized phases in C2M carbonaceous chondrite meteoritesNature, 1984
- A new layered mineral from the Mighei carbonaceous chondriteNature, 1983
- Fe-Ni-S-O layer phase in C2M carbonaceous chondrites—a hydrous sulphide?Nature, 1983
- An unusual layered mineral in chondrules and aggregates of the Allende carbonaceous chondriteNature, 1982
- Alteration of mesostasis in chondrules and aggregates from three C2 carbonaceous chondritesEarth and Planetary Science Letters, 1981
- Serpentine Minerals: Intergrowths and New Combination StructuresScience, 1979
- Magnetite in CI Carbonaceous Meteorites: Origin by Aqueous Activity on a Planetesimal SurfaceScience, 1979
- New phyllosilicate types in a carbonaceous chondrite matrixNature, 1979
- Study of microstructure of chrysotile asbestos by high-resolution electron microscopyActa Crystallographica Section A, 1971
- La magnétite de la météorite d'Orgueil vue au microscope électronique à balayageIcarus, 1971