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Ti in zircon geothermometer (view source)
Revision as of 21:03, 29 November 2014
, 21:03, 29 November 2014no edit summary
This technique is also constrained by several assumptions that, while valid, my prove inconsistent in certain situations. Laboratory studies have used constant pressures when calculating cooling temperatures and have assumed that pressure does not play a major role in Ti incorporation. When estimating cooling temperatures, increased pressure is accounted for by increased temperature estimates and thus increases the uncertainty of the estimates.<ref name="Ferry and Watson 2007 New Thermo models and revised calibrations" />
This technique is also constrained by several assumptions that, while valid, my prove inconsistent in certain situations. Laboratory studies have used constant pressures when calculating cooling temperatures and have assumed that pressure does not play a major role in Ti incorporation. When estimating cooling temperatures, increased pressure is accounted for by increased temperature estimates and thus increases the uncertainty of the estimates.<ref name="Ferry and Watson 2007 New Thermo models and revised calibrations" />
==Practice Reference==
<ref> Watson, E.B.; Wark, D.A.; Thomas, J.B. (3 March 2006). "Crystallization thermometers for zircon and rutile". Contributions to Mineral Petrology 151: 413–433. doi:10.1007/s00410-006-0068-5</ref>
==References==
==References==