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Geochimica et Cosmochimica Acta, 1951
Abstract Natural silicates vary in their O18/O16ratios by as much as 2–4%. This difference is largely due to an exchange reaction between silica and water during the processes of erosion and sedimentation, as a result of which sedimentary rocks are richer in O18 than are the igneous rocks. The temperature coefficient for the silica-water exchange has
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Abstract Natural silicates vary in their O18/O16ratios by as much as 2–4%. This difference is largely due to an exchange reaction between silica and water during the processes of erosion and sedimentation, as a result of which sedimentary rocks are richer in O18 than are the igneous rocks. The temperature coefficient for the silica-water exchange has
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Annual Review of Earth and Planetary Sciences, 1993
Among all the c he mic al e le men ts, ox ygen has a co mbin ation of pro pe rtie s tha t ma kes it u nique ly im por ta nt in cosmoc hem is tr y. I t is a n abu nda nt e leme nt , a nd is t he pr inc ipa l co nst it ue nt o f most m inera ls a nd roc ks.
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Among all the c he mic al e le men ts, ox ygen has a co mbin ation of pro pe rtie s tha t ma kes it u nique ly im por ta nt in cosmoc hem is tr y. I t is a n abu nda nt e leme nt , a nd is t he pr inc ipa l co nst it ue nt o f most m inera ls a nd roc ks.
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Source partitioning using phosphate oxygen isotopes and multiple models in a large catchment
Water Research, 2023Zi-Teng Wang +2 more
exaly
2019
The 'detective' power of stable isotopes for processes that occurred in the past, and for elucidating mechanisms at the molecular level, has impressed researchers over the past 100 years, since the time when isotopes of elements were first discovered.
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The 'detective' power of stable isotopes for processes that occurred in the past, and for elucidating mechanisms at the molecular level, has impressed researchers over the past 100 years, since the time when isotopes of elements were first discovered.
openaire +1 more source