Fluid flow in chondritic parent bodies: Deciphering the compositions of planetesimals

Fluid flow in chondritic parent bodies: Deciphering the compositions of planetesimals

Alteration of the Allende meteorite caused shifts in oxygen isotope ratios along a single mass fractionation line. If alteration was caused by aqueous fluid, the pattern of oxygen isotope fractionation can be explained only by flow of reactive water down a temperature gradient. Down-temperature flow...

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Xehetasun bibliografikoak
Egile Nagusiak:	Young, E, Ash, R, England, P, Rumble, D
Formatua:	Journal article
Hizkuntza:	English
Argitaratua:	1999

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