Using newly developed radar techniques i observed that volcano l has several small 200 500 meter subglacial lakes located over and on the boundaries of the modeled underlying intrusive body implying the intrusive body is associated with. The even younger novate granite 755000 120000 and late pegmatitic dikes in the southern steep belt have been affected neither by d 3 nor by d 4 structures. Protect young shotcrete inclined cross passages allowed to redo the tunnels without interrupting.
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