Zircon saturation revisited: temperature and composition effects in a variety of crustal magma types

Earth and Planetary Science Letters

Volumn 64, Issue 2, 1983, Pages 295-304

  Watson, E Bruce ^a   Harrison, T Mark ^b  

^a RENSSELAER POLYTECHNIC INSTITUTE   (United States)

^b STATE UNIVERSITY OF NEW YORK   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0020969002     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/0012-821X(83)90211-X     Document Type: Article

References (21)

1. Rare earth concentrations in zircons and apatites and their host dacites and granites
2. Behavior of trace elements during magmatic process— a summary of theoretical models and their applications
3. Some experimentally determined zircon/liquid partition coefficients for the rare earth elements
4. Cogenetic and inherited zircon U-Pb systems in granites: Palaeozoic granites of Scotland
5. Zircon saturation in felsic liquids: experimental data and applications to trace element geochemistry
6. Zircon saturation in lunar basalts and granites
7. 4) in synthetic granitic melts
8. Crystallization of apatite in natural magmas under high pressure, hydrous conditions, with particular reference to “orogenic” rock series
9. The distribution of trace elements during strong fractionation of basic magmas: a further study of the Skaergaard intrusion, East Greenland
10. On the distribution of zirconium and hafnium in the Skaergaard intrusion, East Greenland
11. Two contrasting granite types
12. The Berridale Batholith: a lead and strontium isotopic study of its age and origin
13. U-Pb evidence for the pre-emplacement history of granitic magmas, Berridale Batholith, southeastern Australia
14. Protolith ages from inherited zircon cores measured by a high mass-resolution ion microprobe
15. A Nd, Sr and U-Pb zircon isotopic study of the granitoid batholiths of Penninsular Malaysia
16. Petrogenetic implications of Ti, Zr, Y and Nd variations in volcanic rocks
17. Evolution of continental crust and mantle heterogeneity: Evidence from Hf isotopes