Dissolution Phenomena of Ca0-Si02-H20 Gel at Ca/Si>l Coexisting with Ettringite System
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چکیده
منابع مشابه
Peridotite, kimberlite, and carbonatite explained in the system Ca0-Mg0-Si02-CC>2
The key to the origin of carbonatite and kimberlite lies in the system CaOMg0-Si0 2 -C0 2 . Increase in pressure causes a carbonation reaction in the peridotite assemblage as follows: forsterite + clinopyroxene + C 0 2 ^ orthopyroxene + carbonate (Ca:Mg::70:30). This reaction passes through 15 kb-960°C with slope 45 b/°C and terminates at an invariant point near 25 kb-1200°C, where melting begi...
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ژورنال
عنوان ژورنال: Journal of Nuclear Science and Technology
سال: 2000
ISSN: 0022-3131,1881-1248
DOI: 10.1080/18811248.2000.9714958