Различия
Здесь показаны различия между двумя версиями данной страницы.
|
references:nimis2000 [2017/02/17 10:45] user created |
references:nimis2000 [2018/11/12 15:08] |
||
|---|---|---|---|
| Строка 1: | Строка 1: | ||
| - | ====== Single clinopyroxene thermobarometry for garnet peridotites. Part I. Calibration and testing of a Cr-in-Cpx barometer and an enstatite-in-Cpx thermometer, Nimis, Taylor, 2000 ====== | ||
| - | <fullref:nimis2000> | ||
| - | |||
| - | <code> | ||
| - | @Article{Nimis2000, | ||
| - | author="Nimis, Paolo and Taylor, Wayne R.", | ||
| - | title="Single clinopyroxene thermobarometry for garnet peridotites. Part I. Calibration and testing of a Cr-in-Cpx barometer and an enstatite-in-Cpx thermometer", | ||
| - | journal="Contributions to Mineralogy and Petrology", | ||
| - | year="2000", | ||
| - | volume="139", | ||
| - | number="5", | ||
| - | pages="541--554", | ||
| - | abstract="Experimental clinopyroxenes synthesized at 850--1500{\thinspace}{\textdegree}C and 0--60{\thinspace}kbar in the CMS and CMAS-Cr systems and in more complex lherzolitic systems have been used to calibrate a Cr-in-Cpx barometer and an enstatite-in-Cpx thermometer for Cr-diopsides derived from garnet peridotites. The experiments cover a wide range of possible natural peridotitic compositions, from fertile pyrolite to refractory, high-Cr lherzolite. The barometer is based on the Cr exchange between clinopyroxene and garnet. Pressure is formulated as a function of temperature and clinopyroxene composition:", | ||
| - | issn="1432-0967", | ||
| - | doi="10.1007/s004100000156", | ||
| - | url="http://dx.doi.org/10.1007/s004100000156" | ||
| - | } | ||
| - | </code> | ||