Thermometric and Microtextural Study of P21/c Pigeonite from Ureilite PCA82506 (En 76) and an Fe-rich Terrestrial Pigeonite (En 47)

Details Thermometric and Microtextural Study of P21/c Pigeonite from Ureilite PCA82506 (En 76) and an Fe-rich Terrestrial Pigeonite (En 47) Thermometric and Microtextural Study of P21/c Pigeonite from Ureilite PCA82506 (En 76) and an Fe-rich Terrestrial Pigeonite (En 47)

Mar 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999lpi....30.1140m&link_type=abstract

30th Annual Lunar and Planetary Science Conference, March 15-29, 1999, Houston, TX, abstract no. 1140

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Scientific paper

Calibration of the Fe2+-Mg intracrystalline geothermometer for pigeonite
from ureilite PCA82506 and Parana rhyodacite shows no compositional
dependence. PCA82506 pigeonite shows a closure T of 756 C indicating a
very high cooling rate.

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