Volatile/mobile trace elements in Karoonda (C4) chondrite
Abstract
Data for ten volatile/mobile trace elements and non-volatile Co in Karoonda (C4) and in heated primitive chondrites are consistent with the suggestion that Karoonda derives from low-temperature, open-system metamorphism of pristine C3-like material.
- Publication:
-
Geochimica et Cosmochimica Acta
- Pub Date:
- September 1977
- DOI:
- 10.1016/0016-7037(77)90084-9
- Bibcode:
- 1977GeCoA..41.1398M
- Keywords:
-
- Carbonaceous Chondrites;
- Meteoritic Composition;
- Trace Elements;
- Volatility;
- Bismuth;
- Indium;
- Metamorphism (Geology);
- Neutron Activation Analysis;
- Thallium