The thermal history of equilibrated ordinary chondrites and the relationship between textural maturity and temperature

Details The thermal history of equilibrated ordinary chondrites and the relationship between textural maturity and temperature The thermal history of equilibrated ordinary chondrites and the relationship between textural maturity and temperature

Apr 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007gecoa..71.1855k&link_type=abstract

Geochimica et Cosmochimica Acta, Volume 71, Issue 7, p. 1855-1881.

Other

13

Scientific paper

The compositions and textures of phases in eleven equilibrated ordinary chondrites from the H, L, and LL groups spanning petrographic types 4 6 were studied and used to constrain the thermal histories of their parent bodies. Based on Fe Mg exchange between olivine and spinel, average equilibration temperatures for type 4 6 chondrites encompass a small range, 586 777 °C, relative to what is commonly assumed for peak temperatures (600 950 °C). The maximum temperatures recorded by individual chondrites, which are minima relative to peak metamorphic temperatures, increase subtly but systematically with metamorphic type and are tightly clustered for H4-6 (733 754 °C) and LL4-6 (670 777 °C). For the Ls, Ausson (L5) records a higher maximum olivine spinel temperature (761 °C) than does the L4 chondrite Saratov (673 °C) or the L6 chondrite Glatton (712 °C). Our data combined with olivine spinel equilibration temperatures calculated for other equilibrated ordinary chondrites using mineral compositions from the literature demonstrate that, in general, type 4 chondrites within each chemical group record temperatures lower than or equal to those of types 5 6 chondrites. For H chondrites, the olivine spinel closure temperature is a function of spinel grain size, such that larger grains, abundant in types 5 6 chondrites, record temperatures of ˜740 °C or more while smaller grains, rare in types 5 6 but abundant in type 4 chondrites, record lower temperatures. Olivine spinel temperatures in the type 6 chondrites Guareña and Glatton are consistent with rapid (50 100 °C/Myr) cooling from high temperatures in the ordinary chondrite parent bodies. With one exception (˜500 °C/Myr), olivine spinel data for St.-Séverin (LL6) are consistent with similar cooling rates. Cooling rates of order 100 °C/Myr at ˜750 °C for type 6 chondrites are considerably higher than previously determined cooling rates for lower temperatures (⩽550 °C) based on metallography, fission tracks, and geochronology. For H chondrites, current thermal models of an “onion shell” parent body are inconsistent with a small range of peak temperatures based on olivine spinel and two pyroxene thermometry combined with a wide dispersion of cooling rates at low temperatures. Equilibrated chondrites may have sampled regions near a major transition in physical properties such as near the base of a regolith pile.

Affiliated with

Also associated with

No associations

Rating

The thermal history of equilibrated ordinary chondrites and the relationship between textural maturity and temperature does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with The thermal history of equilibrated ordinary chondrites and the relationship between textural maturity and temperature, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and The thermal history of equilibrated ordinary chondrites and the relationship between textural maturity and temperature will most certainly appreciate the feedback.

Rate now

Comments { 0 }

Profile ID: LFWR-SCP-O-1079852