A fertile mantle is a peridotite, typically a lherzolite, that still contains the clinopyroxene and aluminous mineral from which basalt is made. A residual mantle is the peridotite left behind once a melt has been extracted from it: poorer in clinopyroxene, aluminium, calcium and the incompatible elements, richer in olivine and with a higher Mg number.
বইগুলো এখনো বাংলা ভাষায় পাওয়া যায় না — ইংরেজি সংস্করণ দেখানো হচ্ছে।
Earth and Space Sciences · পরিভাষা
Fertile and residual mantle কী?
অন্য নাম: fertile mantle · residual mantle