داستان آبیدیک

water containing minerals


فارسی

1 زمین‌شناسی و معدن:: کانی های آبدار

permanently transported into the mantle in sub- duction zones as water-containing sediments or within basalts whose original dry minerals are converted into water-containing minerals. Basaltic rocks contain abundant water because interaction with seawater near the mid-ocean ridge forms water-containing minerals (zeolite, chlorite, epidote, amphibole; Ch. 5). Under conditions of subduction metamorphism, the water-containing minerals become unstable and are replaced. Sediments contribute significantly to the de- watering in a subduction zone although following high-pressure metamorphism they continue to in- clude water-containing minerals such as phengite (a type of mica), karpholite, chloritoid and lawsonite. Water may also be released by the collapse of water-containing minerals.

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