SHRIMP U–Pb geochronology of authigenic xenotime and its potential for dating sedimentary basins
Author:
Publisher
Informa UK Limited
Subject
General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous)
Link
http://www.tandfonline.com/doi/pdf/10.1046/j.1440-0952.2000.00819.x
Reference34 articles.
1. Aleinikoff, J. N. and Grauch, R. I. (1990) U–Pb geochronologic constraints on the origin of a unique monazite‐xenotime gneiss, New York American Journal of Science, 290, pp. 522 - 546.
2. Berner, R. A.(1980) Early Diagenesis: A Theoretical Approach. Princeton : Princeton University Press.
3. Bouch, J. E. and Hole, M. J. and Trewin, N. H. and Morton, A. C. (1995) Low‐temperature aqueous mobility of the rare‐earth elements during sandstone diagenesis Journal of the Geological Society of London, 152, pp. 895 - 898.
4. Brown, S. J. A. and Fletcher, I. R. (1999) SHRIMP U–Pb dating of preeruptive growth history of zircons from the 340 kaWhakamaru Ignimbrite, New Zealand: evidence for >250 k.y. magma residence times Geology, 27, pp. 1035 - 1038.
5. Bruhn, F. and Möller, A. and Sie, S. H. and Henson, B. J. (1999) U–Th–Pb chemical dating of monazites using the proton microprobe Nuclear Instruments and Methods in Physics Research B, 158, pp. 616 - 620.
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